CINXE.COM

<!DOCTYPE html> <html lang="en" xmlns:fb="http://www.facebook.com/2008/fbml" class="wf-loading"> <head prefix="og: https://ogp.me/ns# fb: https://ogp.me/ns/fb# academia: https://ogp.me/ns/fb/academia#"> <meta charset="utf-8"> <meta name=viewport content="width=device-width, initial-scale=1"> <meta rel="search" type="application/opensearchdescription+xml" href="/open_search.xml" title="Academia.edu"> <title>Anders Omstedt | University of Gothenburg - Academia.edu</title>  <link href="//a.academia-assets.com/images/favicons/favicon-production.ico" rel="shortcut icon" type="image/vnd.microsoft.icon"> <link rel="apple-touch-icon" sizes="57x57" href="//a.academia-assets.com/images/favicons/apple-touch-icon-57x57.png"> <link rel="apple-touch-icon" sizes="60x60" href="//a.academia-assets.com/images/favicons/apple-touch-icon-60x60.png"> <link rel="apple-touch-icon" sizes="72x72" href="//a.academia-assets.com/images/favicons/apple-touch-icon-72x72.png"> <link rel="apple-touch-icon" sizes="76x76" href="//a.academia-assets.com/images/favicons/apple-touch-icon-76x76.png"> <link rel="apple-touch-icon" sizes="114x114" href="//a.academia-assets.com/images/favicons/apple-touch-icon-114x114.png"> <link rel="apple-touch-icon" sizes="120x120" href="//a.academia-assets.com/images/favicons/apple-touch-icon-120x120.png"> <link rel="apple-touch-icon" sizes="144x144" href="//a.academia-assets.com/images/favicons/apple-touch-icon-144x144.png"> <link rel="apple-touch-icon" sizes="152x152" href="//a.academia-assets.com/images/favicons/apple-touch-icon-152x152.png"> <link rel="apple-touch-icon" sizes="180x180" href="//a.academia-assets.com/images/favicons/apple-touch-icon-180x180.png"> <link rel="icon" type="image/png" href="//a.academia-assets.com/images/favicons/favicon-32x32.png" sizes="32x32"> <link rel="icon" type="image/png" href="//a.academia-assets.com/images/favicons/favicon-194x194.png" sizes="194x194"> <link rel="icon" type="image/png" href="//a.academia-assets.com/images/favicons/favicon-96x96.png" sizes="96x96"> <link rel="icon" type="image/png" href="//a.academia-assets.com/images/favicons/android-chrome-192x192.png" sizes="192x192"> <link rel="icon" type="image/png" href="//a.academia-assets.com/images/favicons/favicon-16x16.png" sizes="16x16"> <link rel="manifest" href="//a.academia-assets.com/images/favicons/manifest.json"> <meta name="msapplication-TileColor" content="#2b5797"> <meta name="msapplication-TileImage" content="//a.academia-assets.com/images/favicons/mstile-144x144.png"> <meta name="theme-color" content="#ffffff"> <script> window.performance && window.performance.measure && window.performance.measure("Time To First Byte", "requestStart", "responseStart"); </script> <script> (function() { if (!window.URLSearchParams || !window.history || !window.history.replaceState) { return; } var searchParams = new URLSearchParams(window.location.search); var paramsToDelete = [ 'fs', 'sm', 'swp', 'iid', 'nbs', 'rcc', // related content category 'rcpos', // related content carousel position 'rcpg', // related carousel page 'rchid', // related content hit id 'f_ri', // research interest id, for SEO tracking 'f_fri', // featured research interest, for SEO tracking (param key without value) 'f_rid', // from research interest directory for SEO tracking 'f_loswp', // from research interest pills on LOSWP sidebar for SEO tracking 'rhid', // referrring hit id ]; if (paramsToDelete.every((key) => searchParams.get(key) === null)) { return; } paramsToDelete.forEach((key) => { searchParams.delete(key); }); var cleanUrl = new URL(window.location.href); cleanUrl.search = searchParams.toString(); history.replaceState({}, document.title, cleanUrl); })(); </script> <script async src="https://www.googletagmanager.com/gtag/js?id=G-5VKX33P2DS"></script> <script> window.dataLayer = window.dataLayer || []; function gtag(){dataLayer.push(arguments);} gtag('js', new Date()); gtag('config', 'G-5VKX33P2DS', { cookie_domain: 'academia.edu', send_page_view: false, }); gtag('event', 'page_view', { 'controller': "profiles/works", 'action': "summary", 'controller_action': 'profiles/works#summary', 'logged_in': 'false', 'edge': 'unknown', // Send nil if there is no A/B test bucket, in case some records get logged // with missing data - that way we can distinguish between the two cases. // ab_test_bucket should be of the form <ab_test_name>:<bucket> 'ab_test_bucket': null, }) </script> <script type="text/javascript"> window.sendUserTiming = function(timingName) { if (!(window.performance && window.performance.measure)) return; var entries = window.performance.getEntriesByName(timingName, "measure"); if (entries.length !== 1) return; var timingValue = Math.round(entries[0].duration); gtag('event', 'timing_complete', { name: timingName, value: timingValue, event_category: 'User-centric', }); }; window.sendUserTiming("Time To First Byte"); </script> <meta name="csrf-param" content="authenticity_token" /> <meta name="csrf-token" content="K0qwvvnzmHaa4WETZ91g9O0aV0c0VHaMbM5Mdn3IWApT33BMcTWfu1ipGfoOgqAifmKExOR+ZiVWQ8MDzvn8Wg==" /> <link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/wow-77f7b87cb1583fc59aa8f94756ebfe913345937eb932042b4077563bebb5fb4b.css" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/social/home-9e8218e1301001388038e3fc3427ed00d079a4760ff7745d1ec1b2d59103170a.css" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system/heading-b2b823dd904da60a48fd1bfa1defd840610c2ff414d3f39ed3af46277ab8df3b.css" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system/button-3cea6e0ad4715ed965c49bfb15dedfc632787b32ff6d8c3a474182b231146ab7.css" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system/text_button-73590134e40cdb49f9abdc8e796cc00dc362693f3f0f6137d6cf9bb78c318ce7.css" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system/body-8d679e925718b5e8e4b18e9a4fab37f7eaa99e43386459376559080ac8f2856a.css" /><link crossorigin="" href="https://fonts.gstatic.com/" rel="preconnect" /><link href="https://fonts.googleapis.com/css2?family=DM+Sans:ital,opsz,wght@0,9..40,100..1000;1,9..40,100..1000&family=Gupter:wght@400;500;700&family=IBM+Plex+Mono:wght@300;400&family=Material+Symbols+Outlined:opsz,wght,FILL,GRAD@20,400,0,0&display=swap" rel="stylesheet" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system/common-10fa40af19d25203774df2d4a03b9b5771b45109c2304968038e88a81d1215c5.css" /> <meta name="author" content="anders omstedt" /> <meta name="description" content="Professor emeritus, Department of Marine Sciences, University of Gothenburg with main interest in Oceanography, especially lakes and coastal seas including…" /> <meta name="google-site-verification" content="bKJMBZA7E43xhDOopFZkssMMkBRjvYERV-NaN4R6mrs" /> <script> var $controller_name = 'works'; var $action_name = "summary"; var $rails_env = 'production'; var $app_rev = '804f70c34f4012696fd2e8a7fa034fa9190bc0eb'; var $domain = 'academia.edu'; var $app_host = "academia.edu"; var $asset_host = "academia-assets.com"; var $start_time = new Date().getTime(); var $recaptcha_key = "6LdxlRMTAAAAADnu_zyLhLg0YF9uACwz78shpjJB"; var $recaptcha_invisible_key = "6Lf3KHUUAAAAACggoMpmGJdQDtiyrjVlvGJ6BbAj"; var $disableClientRecordHit = false; </script> <script> window.Aedu = { hit_data: null }; window.Aedu.SiteStats = {"premium_universities_count":15262,"monthly_visitors":"121 million","monthly_visitor_count":121005025,"monthly_visitor_count_in_millions":121,"user_count":278720373,"paper_count":55203019,"paper_count_in_millions":55,"page_count":432000000,"page_count_in_millions":432,"pdf_count":16500000,"pdf_count_in_millions":16}; window.Aedu.serverRenderTime = new Date(1734111830000); window.Aedu.timeDifference = new Date().getTime() - 1734111830000; window.Aedu.isUsingCssV1 = false; window.Aedu.enableLocalization = true; window.Aedu.activateFullstory = false; window.Aedu.serviceAvailability = { status: {"attention_db":"on","bibliography_db":"on","contacts_db":"on","email_db":"on","indexability_db":"on","mentions_db":"on","news_db":"on","notifications_db":"on","offsite_mentions_db":"on","redshift":"on","redshift_exports_db":"on","related_works_db":"on","ring_db":"on","user_tests_db":"on"}, serviceEnabled: function(service) { return this.status[service] === "on"; }, readEnabled: function(service) { return this.serviceEnabled(service) || this.status[service] === "read_only"; }, }; window.Aedu.viewApmTrace = function() { // Check if x-apm-trace-id meta tag is set, and open the trace in APM // in a new window if it is. var apmTraceId = document.head.querySelector('meta[name="x-apm-trace-id"]'); if (apmTraceId) { var traceId = apmTraceId.content; // Use trace ID to construct URL, an example URL looks like: // https://app.datadoghq.com/apm/traces?query=trace_id%31298410148923562634 var apmUrl = 'https://app.datadoghq.com/apm/traces?query=trace_id%3A' + traceId; window.open(apmUrl, '_blank'); } }; </script>  <link href="https://fonts.googleapis.com/css?family=Roboto:100,100i,300,300i,400,400i,500,500i,700,700i,900,900i" rel="stylesheet"> <link href="//maxcdn.bootstrapcdn.com/font-awesome/4.3.0/css/font-awesome.min.css" rel="stylesheet"> <link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/libraries-a9675dcb01ec4ef6aa807ba772c7a5a00c1820d3ff661c1038a20f80d06bb4e4.css" /> <link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/academia-0fb6fc03c471832908791ad7ddba619b6165b3ccf7ae0f65cf933f34b0b660a7.css" /> <link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system_legacy-056a9113b9a0f5343d013b29ee1929d5a18be35fdcdceb616600b4db8bd20054.css" /> <script src="//a.academia-assets.com/assets/webpack_bundles/runtime-bundle-005434038af4252ca37c527588411a3d6a0eabb5f727fac83f8bbe7fd88d93bb.js"></script> <script src="//a.academia-assets.com/assets/webpack_bundles/webpack_libraries_and_infrequently_changed.wjs-bundle-8725d44cf7fef59a36f3a49c1fdad537837f54fdcd46824499ece5eb79144604.js"></script> <script src="//a.academia-assets.com/assets/webpack_bundles/core_webpack.wjs-bundle-8bef471101e20eeb6387f1463424c287e25f4c6e19169c3d34a7fc2b3a6cf862.js"></script> <script src="//a.academia-assets.com/assets/webpack_bundles/sentry.wjs-bundle-5fe03fddca915c8ba0f7edbe64c194308e8ce5abaed7bffe1255ff37549c4808.js"></script> <script> jade = window.jade || {}; jade.helpers = window.$h; jade._ = window._; </script>  <script id="tag-manager-head-root">(function(w,d,s,l,i){w[l]=w[l]||[];w[l].push({'gtm.start': new Date().getTime(),event:'gtm.js'});var f=d.getElementsByTagName(s)[0], j=d.createElement(s),dl=l!='dataLayer'?'&l='+l:'';j.async=true;j.src= 'https://www.googletagmanager.com/gtm.js?id='+i+dl;f.parentNode.insertBefore(j,f); })(window,document,'script','dataLayer_old','GTM-5G9JF7Z');</script>  <script> window.gptadslots = []; window.googletag = window.googletag || {}; window.googletag.cmd = window.googletag.cmd || []; </script> <script type="text/javascript"> // TODO(jacob): This should be defined, may be rare load order problem. // Checking if null is just a quick fix, will default to en if unset. // Better fix is to run this immedietely after I18n is set. if (window.I18n != null) { I18n.defaultLocale = "en"; I18n.locale = "en"; I18n.fallbacks = true; } </script> <link rel="canonical" href="https://gu-se.academia.edu/AndersOmstedt" /> </head>   <body class='c-profiles/works a-summary logged_out'>  <div id="fb-root"></div><script>window.fbAsyncInit = function() { FB.init({ appId: "2369844204", version: "v8.0", status: true, cookie: true, xfbml: true }); // Additional initialization code. if (window.InitFacebook) { // facebook.ts already loaded, set it up. window.InitFacebook(); } else { // Set a flag for facebook.ts to find when it loads. window.academiaAuthReadyFacebook = true; } };</script><script>window.fbAsyncLoad = function() { // Protection against double calling of this function if (window.FB) { return; } (function(d, s, id){ var js, fjs = d.getElementsByTagName(s)[0]; if (d.getElementById(id)) {return;} js = d.createElement(s); js.id = id; js.src = "//connect.facebook.net/en_US/sdk.js"; fjs.parentNode.insertBefore(js, fjs); }(document, 'script', 'facebook-jssdk')); } if (!window.defer_facebook) { // Autoload if not deferred window.fbAsyncLoad(); } else { // Defer loading by 5 seconds setTimeout(function() { window.fbAsyncLoad(); }, 5000); }</script> <div id="google-root"></div><script>window.loadGoogle = function() { if (window.InitGoogle) { // google.ts already loaded, set it up. window.InitGoogle("331998490334-rsn3chp12mbkiqhl6e7lu2q0mlbu0f1b"); } else { // Set a flag for google.ts to use when it loads. window.GoogleClientID = "331998490334-rsn3chp12mbkiqhl6e7lu2q0mlbu0f1b"; } };</script><script>window.googleAsyncLoad = function() { // Protection against double calling of this function (function(d) { var js; var id = 'google-jssdk'; var ref = d.getElementsByTagName('script')[0]; if (d.getElementById(id)) { return; } js = d.createElement('script'); js.id = id; js.async = true; js.onload = loadGoogle; js.src = "https://accounts.google.com/gsi/client" ref.parentNode.insertBefore(js, ref); }(document)); } if (!window.defer_google) { // Autoload if not deferred window.googleAsyncLoad(); } else { // Defer loading by 5 seconds setTimeout(function() { window.googleAsyncLoad(); }, 5000); }</script> <div id="tag-manager-body-root">  <noscript><iframe src="https://www.googletagmanager.com/ns.html?id=GTM-5G9JF7Z" height="0" width="0" style="display:none;visibility:hidden"></iframe></noscript>   <script> window.addEventListener('load', function() { if (document.querySelector('input[name="commit"]')) { document.querySelector('input[name="commit"]').addEventListener('click', function() { gtag('event', 'click', { event_category: 'button', event_label: 'Log In' }) }) } }); </script> </div> <script>var _comscore = _comscore || []; _comscore.push({ c1: "2", c2: "26766707" }); (function() { var s = document.createElement("script"), el = document.getElementsByTagName("script")[0]; s.async = true; s.src = (document.location.protocol == "https:" ? "https://sb" : "http://b") + ".scorecardresearch.com/beacon.js"; el.parentNode.insertBefore(s, el); })();</script><img src="https://sb.scorecardresearch.com/p?c1=2&c2=26766707&cv=2.0&cj=1" style="position: absolute; visibility: hidden" /> <div id='react-modal'></div> <div class='DesignSystem'> <a class='u-showOnFocus' href='#site'> Skip to main content </a> </div> <div id="upgrade_ie_banner" style="display: none;"><p>Academia.edu no longer supports Internet Explorer.</p><p>To browse Academia.edu and the wider internet faster and more securely, please take a few seconds to <a href="https://www.academia.edu/upgrade-browser">upgrade your browser</a>.</p></div><script>// Show this banner for all versions of IE if (!!window.MSInputMethodContext || /(MSIE)/.test(navigator.userAgent)) { document.getElementById('upgrade_ie_banner').style.display = 'block'; }</script> <div class="DesignSystem bootstrap ShrinkableNav"><div class="navbar navbar-default main-header"><div class="container-wrapper" id="main-header-container"><div class="container"><div class="navbar-header"><div class="nav-left-wrapper u-mt0x"><div class="nav-logo"><a data-main-header-link-target="logo_home" href="https://www.academia.edu/"><img class="visible-xs-inline-block" style="height: 24px;" alt="Academia.edu" src="//a.academia-assets.com/images/academia-logo-redesign-2015-A.svg" width="24" height="24" /><img width="145.2" height="18" class="hidden-xs" style="height: 24px;" alt="Academia.edu" src="//a.academia-assets.com/images/academia-logo-redesign-2015.svg" /></a></div><div class="nav-search"><div class="SiteSearch-wrapper select2-no-default-pills"><form class="js-SiteSearch-form DesignSystem" action="https://www.academia.edu/search" accept-charset="UTF-8" method="get"><input name="utf8" type="hidden" value="✓" autocomplete="off" /><i class="SiteSearch-icon fa fa-search u-fw700 u-positionAbsolute u-tcGrayDark"></i><input class="js-SiteSearch-form-input SiteSearch-form-input form-control" data-main-header-click-target="search_input" name="q" placeholder="Search" type="text" value="" /></form></div></div></div><div class="nav-right-wrapper pull-right"><ul class="NavLinks js-main-nav list-unstyled"><li class="NavLinks-link"><a class="js-header-login-url Button Button--inverseGray Button--sm u-mb4x" id="nav_log_in" rel="nofollow" href="https://www.academia.edu/login">Log In</a></li><li class="NavLinks-link u-p0x"><a class="Button Button--inverseGray Button--sm u-mb4x" rel="nofollow" href="https://www.academia.edu/signup">Sign Up</a></li></ul><button class="hidden-lg hidden-md hidden-sm u-ml4x navbar-toggle collapsed" data-target=".js-mobile-header-links" data-toggle="collapse" type="button"><span class="icon-bar"></span><span class="icon-bar"></span><span class="icon-bar"></span></button></div></div><div class="collapse navbar-collapse js-mobile-header-links"><ul class="nav navbar-nav"><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/login">Log In</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/signup">Sign Up</a></li><li class="u-borderColorGrayLight u-borderBottom1 js-mobile-nav-expand-trigger"><a href="#">more&nbsp<span class="caret"></span></a></li><li><ul class="js-mobile-nav-expand-section nav navbar-nav u-m0x collapse"><li class="u-borderColorGrayLight u-borderBottom1"><a rel="false" href="https://www.academia.edu/about">About</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/press">Press</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="false" href="https://www.academia.edu/documents">Papers</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/terms">Terms</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/privacy">Privacy</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/copyright">Copyright</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/hiring"><i class="fa fa-briefcase"></i> We're Hiring!</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://support.academia.edu/"><i class="fa fa-question-circle"></i> Help Center</a></li><li class="js-mobile-nav-collapse-trigger u-borderColorGrayLight u-borderBottom1 dropup" style="display:none"><a href="#">less&nbsp<span class="caret"></span></a></li></ul></li></ul></div></div></div><script>(function(){ var $moreLink = $(".js-mobile-nav-expand-trigger"); var $lessLink = $(".js-mobile-nav-collapse-trigger"); var $section = $('.js-mobile-nav-expand-section'); $moreLink.click(function(ev){ ev.preventDefault(); $moreLink.hide(); $lessLink.show(); $section.collapse('show'); }); $lessLink.click(function(ev){ ev.preventDefault(); $moreLink.show(); $lessLink.hide(); $section.collapse('hide'); }); })() if ($a.is_logged_in() || false) { new Aedu.NavigationController({ el: '.js-main-nav', showHighlightedNotification: false }); } else { $(".js-header-login-url").attr("href", $a.loginUrlWithRedirect()); } Aedu.autocompleteSearch = new AutocompleteSearch({el: '.js-SiteSearch-form'});</script></div></div> <div id='site' class='fixed'> <div id="content" class="clearfix"> <script>document.addEventListener('DOMContentLoaded', function(){ var $dismissible = $(".dismissible_banner"); $dismissible.click(function(ev) { $dismissible.hide(); }); });</script> <script src="//a.academia-assets.com/assets/webpack_bundles/profile.wjs-bundle-682da5bfe717a81da1eb3b05151217255d7ca4c2b93c310724f37d503f7e9668.js" defer="defer"></script><script>Aedu.rankings = { showPaperRankingsLink: false } $viewedUser = Aedu.User.set_viewed( {"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt","photo":"https://0.academia-photos.com/11956707/9542001/60445714/s65_anders.omstedt.jpg","has_photo":true,"department":{"id":1586445,"name":"Department of Marine Sciences","url":"https://gu-se.academia.edu/Departments/Department_of_Marine_Sciences/Documents","university":{"id":579,"name":"University of Gothenburg","url":"https://gu-se.academia.edu/"}},"position":"Emeritus","position_id":6,"is_analytics_public":false,"interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":410933,"name":"Baltic Sea","url":"https://www.academia.edu/Documents/in/Baltic_Sea"},{"id":1512,"name":"Climate Change","url":"https://www.academia.edu/Documents/in/Climate_Change"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":1275,"name":"Coastal Management","url":"https://www.academia.edu/Documents/in/Coastal_Management"},{"id":231615,"name":"Climate policy","url":"https://www.academia.edu/Documents/in/Climate_policy"},{"id":789603,"name":"Coastal Research","url":"https://www.academia.edu/Documents/in/Coastal_Research"},{"id":549694,"name":"Storms","url":"https://www.academia.edu/Documents/in/Storms"},{"id":1004426,"name":"North Sea Region","url":"https://www.academia.edu/Documents/in/North_Sea_Region"},{"id":276491,"name":"Baltic Sea region","url":"https://www.academia.edu/Documents/in/Baltic_Sea_region"},{"id":615930,"name":"Regional Climate Models","url":"https://www.academia.edu/Documents/in/Regional_Climate_Models"},{"id":1442177,"name":"Global Models","url":"https://www.academia.edu/Documents/in/Global_Models"},{"id":18845,"name":"Environmental Sustainability","url":"https://www.academia.edu/Documents/in/Environmental_Sustainability"},{"id":45405,"name":"Global Warming","url":"https://www.academia.edu/Documents/in/Global_Warming"},{"id":16441,"name":"Marine Science","url":"https://www.academia.edu/Documents/in/Marine_Science"},{"id":2258,"name":"Paleoclimatology","url":"https://www.academia.edu/Documents/in/Paleoclimatology"}]} ); if ($a.is_logged_in() && $viewedUser.is_current_user()) { $('body').addClass('profile-viewed-by-owner'); } $socialProfiles = []</script><div id="js-react-on-rails-context" style="display:none" data-rails-context="{"inMailer":false,"i18nLocale":"en","i18nDefaultLocale":"en","href":"https://gu-se.academia.edu/AndersOmstedt","location":"/AndersOmstedt","scheme":"https","host":"gu-se.academia.edu","port":null,"pathname":"/AndersOmstedt","search":null,"httpAcceptLanguage":null,"serverSide":false}"></div> <div class="js-react-on-rails-component" style="display:none" data-component-name="ProfileCheckPaperUpdate" data-props="{}" data-trace="false" data-dom-id="ProfileCheckPaperUpdate-react-component-91521c16-0a32-4c5a-848d-1f094d6f44f6"></div> <div id="ProfileCheckPaperUpdate-react-component-91521c16-0a32-4c5a-848d-1f094d6f44f6"></div> <div class="DesignSystem"><div class="onsite-ping" id="onsite-ping"></div></div><div class="profile-user-info DesignSystem"><div class="social-profile-container"><div class="left-panel-container"><div class="user-info-component-wrapper"><div class="user-summary-cta-container"><div class="user-summary-container"><div class="social-profile-avatar-container"><img class="profile-avatar u-positionAbsolute" alt="Anders Omstedt" border="0" onerror="if (this.src != '//a.academia-assets.com/images/s200_no_pic.png') this.src = '//a.academia-assets.com/images/s200_no_pic.png';" width="200" height="200" src="https://0.academia-photos.com/11956707/9542001/60445714/s200_anders.omstedt.jpg" /></div><div class="title-container"><h1 class="ds2-5-heading-sans-serif-sm">Anders Omstedt</h1><div class="affiliations-container fake-truncate js-profile-affiliations"><div><a class="u-tcGrayDarker" href="https://gu-se.academia.edu/">University of Gothenburg</a>, <a class="u-tcGrayDarker" href="https://gu-se.academia.edu/Departments/Department_of_Marine_Sciences/Documents">Department of Marine Sciences</a>, <span class="u-tcGrayDarker">Emeritus</span></div><div><a class="u-tcGrayDarker" href="https://gu-se.academia.edu/">University of Gothenburg</a>, <a class="u-tcGrayDarker" href="https://gu-se.academia.edu/Departments/Earth_Sciences/Documents">Earth Sciences</a>, <span class="u-tcGrayDarker">Faculty Member</span></div></div></div></div><div class="sidebar-cta-container"><button class="ds2-5-button hidden profile-cta-button grow js-profile-follow-button" data-broccoli-component="user-info.follow-button" data-click-track="profile-user-info-follow-button" data-follow-user-fname="Anders" data-follow-user-id="11956707" data-follow-user-source="profile_button" data-has-google="false"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">add</span>Follow</button><button class="ds2-5-button hidden profile-cta-button grow js-profile-unfollow-button" data-broccoli-component="user-info.unfollow-button" data-click-track="profile-user-info-unfollow-button" data-unfollow-user-id="11956707"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">done</span>Following</button></div></div><div class="user-stats-container"><a><div class="stat-container js-profile-followers"><p class="label">Followers</p><p class="data">75</p></div></a><a><div class="stat-container js-profile-followees" data-broccoli-component="user-info.followees-count" data-click-track="profile-expand-user-info-following"><p class="label">Following</p><p class="data">25</p></div></a><a><div class="stat-container js-profile-coauthors" data-broccoli-component="user-info.coauthors-count" data-click-track="profile-expand-user-info-coauthors"><p class="label">Co-authors</p><p class="data">21</p></div></a><a href="/AndersOmstedt/mentions"><div class="stat-container"><p class="label">Mentions</p><p class="data">3,480</p></div></a><span><div class="stat-container"><p class="label"><span class="js-profile-total-view-text">Public Views</span></p><p class="data"><span class="js-profile-view-count"></span></p></div></span></div><div class="user-bio-container"><div class="profile-bio fake-truncate js-profile-about" style="margin: 0px;">Professor emeritus, Department of Marine Sciences, University of Gothenburg with main interest in Oceanography, especially lakes and coastal seas including physical, biochemical modelling and human impacts.<br /><b>Address: </b>Göteborg, Västra Götaland, Sweden<br /><div class="js-profile-less-about u-linkUnstyled u-tcGrayDarker u-textDecorationUnderline u-displayNone">less</div></div></div><div class="ri-section"><div class="ri-section-header"><span>Interests</span><a class="ri-more-link js-profile-ri-list-card" data-click-track="profile-user-info-primary-research-interest" data-has-card-for-ri-list="11956707">View All (17)</a></div><div class="ri-tags-container"><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="11956707" href="https://www.academia.edu/Documents/in/Earth_Sciences"><div id="js-react-on-rails-context" style="display:none" data-rails-context="{"inMailer":false,"i18nLocale":"en","i18nDefaultLocale":"en","href":"https://gu-se.academia.edu/AndersOmstedt","location":"/AndersOmstedt","scheme":"https","host":"gu-se.academia.edu","port":null,"pathname":"/AndersOmstedt","search":null,"httpAcceptLanguage":null,"serverSide":false}"></div> <div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Earth Sciences"]}" data-trace="false" data-dom-id="Pill-react-component-a5018486-e61e-4e15-872c-c918cc12a9e3"></div> <div id="Pill-react-component-a5018486-e61e-4e15-872c-c918cc12a9e3"></div> </a><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="11956707" href="https://www.academia.edu/Documents/in/Baltic_Sea"><div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Baltic Sea"]}" data-trace="false" data-dom-id="Pill-react-component-2c3de0ad-0ff2-4a7a-bf4c-afab8d298b00"></div> <div id="Pill-react-component-2c3de0ad-0ff2-4a7a-bf4c-afab8d298b00"></div> </a><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="11956707" href="https://www.academia.edu/Documents/in/Climate_Change"><div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Climate Change"]}" data-trace="false" data-dom-id="Pill-react-component-bddbb33e-adfd-49f2-97a7-e93b570b8c23"></div> <div id="Pill-react-component-bddbb33e-adfd-49f2-97a7-e93b570b8c23"></div> </a><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="11956707" href="https://www.academia.edu/Documents/in/Geology"><div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Geology"]}" data-trace="false" data-dom-id="Pill-react-component-222065be-db1c-4e77-a355-500ffe2f03bd"></div> <div id="Pill-react-component-222065be-db1c-4e77-a355-500ffe2f03bd"></div> </a><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="11956707" href="https://www.academia.edu/Documents/in/Environmental_Science"><div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Environmental Science"]}" data-trace="false" data-dom-id="Pill-react-component-c666c7d7-2817-4a56-9107-3ca953c59f07"></div> <div id="Pill-react-component-c666c7d7-2817-4a56-9107-3ca953c59f07"></div> </a></div></div><div class="external-links-container"><ul class="profile-links new-profile js-UserInfo-social"><li class="left-most js-UserInfo-social-cv" data-broccoli-component="user-info.cv-button" data-click-track="profile-user-info-cv" data-cv-filename="CV_Anders_Omstedt_2022-01-20.pdf" data-placement="top" data-toggle="tooltip" href="/AndersOmstedt/CurriculumVitae"><button class="ds2-5-text-link ds2-5-text-link--small" style="font-size: 20px; letter-spacing: 0.8px"><span class="ds2-5-text-link__content">CV</span></button></li><li><a class="ds2-5-text-link ds2-5-text-link--small" href="https://andersomstedt.academia.edu/"><span class="ds2-5-text-link__content"><i class="fa fa-laptop"></i></span></a></li><li class="profile-profiles js-social-profiles-container"><i class="fa fa-spin fa-spinner"></i></li></ul></div></div></div><div class="right-panel-container"><div class="user-content-wrapper"><div class="uploads-container" id="social-redesign-work-container"><div class="upload-header"><h2 class="ds2-5-heading-sans-serif-xs">Uploads</h2></div><div class="nav-container backbone-profile-documents-nav hidden-xs"><ul class="nav-tablist" role="tablist"><li class="nav-chip active" role="presentation"><a data-section-name="" data-toggle="tab" href="#all" role="tab">all</a></li><li class="nav-chip" role="presentation"><a class="js-profile-docs-nav-section u-textTruncate" data-click-track="profile-works-tab" data-section-name="Papers" data-toggle="tab" href="#papers" role="tab" title="Papers"><span>305</span> <span class="ds2-5-body-sm-bold">Papers</span></a></li><li class="nav-chip" role="presentation"><a class="js-profile-docs-nav-section u-textTruncate" data-click-track="profile-works-tab" data-section-name="Books" data-toggle="tab" href="#books" role="tab" title="Books"><span>2</span> <span class="ds2-5-body-sm-bold">Books</span></a></li></ul></div><div class="divider ds-divider-16" style="margin: 0px;"></div><div class="documents-container backbone-social-profile-documents" style="width: 100%;"><div class="u-taCenter"></div><div class="profile--tab_content_container js-tab-pane tab-pane active" id="all"><div class="profile--tab_heading_container js-section-heading" data-section="Papers" id="Papers"><h3 class="profile--tab_heading_container">Papers by Anders Omstedt</h3></div><div class="js-work-strip profile--work_container" data-work-id="124218655"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/124218655/The_ocean_Excursion_and_return_The_ocean_Excursion_and_return"><img alt="Research paper thumbnail of The ocean: Excursion and return The ocean: Excursion and return" class="work-thumbnail" src="https://attachments.academia-assets.com/118486198/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/124218655/The_ocean_Excursion_and_return_The_ocean_Excursion_and_return">The ocean: Excursion and return The ocean: Excursion and return</a></div><div class="wp-workCard_item"><span>Filosofia,</span><span>, 2022</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The ocean with its coastal seas is under increasing anthropogenic pressure, severely threatening ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The ocean with its coastal seas is under increasing anthropogenic pressure, severely threatening ocean health and marine life. Human dependency on and management of the ocean are disconnected, which is in part why the United Nations (UN) is launching the Decade of Ocean Science for Sustainable Development, 2021-2030 ("Ocean Decade"). Here we investigate how philosophy and literature can inspire us to change the relationship between humans and the ocean. The starting point is natural science and human exploration of the sea. Then we consider philosophy, starting from Aristotle's forms of knowledge-episteme, techne, and phronesis-focusing particularly on phronesis, or practical wisdom. Referring to Homer's Odyssey, we investigate the threats that the ocean may face during the UN's Ocean Decade. From this, we identify several things that will make for a successful Ocean Decade: practical wise leadership, clear vision, societal involvement, information sharing, admitting the vulnerability of both the ocean and humans, and storytelling.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ac732a596bc430bdd4d58da23b308f46" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":118486198,"asset_id":124218655,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/118486198/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="124218655"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="124218655"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124218655; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124218655]").text(description); $(".js-view-count[data-work-id=124218655]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124218655; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124218655']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124218655, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "ac732a596bc430bdd4d58da23b308f46" } } $('.js-work-strip[data-work-id=124218655]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124218655,"title":"The ocean: Excursion and return The ocean: Excursion and return","translated_title":"","metadata":{"doi":"10.13135/2704-8195/7241","abstract":"The ocean with its coastal seas is under increasing anthropogenic pressure, severely threatening ocean health and marine life. Human dependency on and management of the ocean are disconnected, which is in part why the United Nations (UN) is launching the Decade of Ocean Science for Sustainable Development, 2021-2030 (\"Ocean Decade\"). Here we investigate how philosophy and literature can inspire us to change the relationship between humans and the ocean. The starting point is natural science and human exploration of the sea. Then we consider philosophy, starting from Aristotle's forms of knowledge-episteme, techne, and phronesis-focusing particularly on phronesis, or practical wisdom. Referring to Homer's Odyssey, we investigate the threats that the ocean may face during the UN's Ocean Decade. From this, we identify several things that will make for a successful Ocean Decade: practical wise leadership, clear vision, societal involvement, information sharing, admitting the vulnerability of both the ocean and humans, and storytelling.","publication_date":{"day":null,"month":null,"year":2022,"errors":{}},"publication_name":"Filosofia,"},"translated_abstract":"The ocean with its coastal seas is under increasing anthropogenic pressure, severely threatening ocean health and marine life. Human dependency on and management of the ocean are disconnected, which is in part why the United Nations (UN) is launching the Decade of Ocean Science for Sustainable Development, 2021-2030 (\"Ocean Decade\"). Here we investigate how philosophy and literature can inspire us to change the relationship between humans and the ocean. The starting point is natural science and human exploration of the sea. Then we consider philosophy, starting from Aristotle's forms of knowledge-episteme, techne, and phronesis-focusing particularly on phronesis, or practical wisdom. Referring to Homer's Odyssey, we investigate the threats that the ocean may face during the UN's Ocean Decade. From this, we identify several things that will make for a successful Ocean Decade: practical wise leadership, clear vision, societal involvement, information sharing, admitting the vulnerability of both the ocean and humans, and storytelling.","internal_url":"https://www.academia.edu/124218655/The_ocean_Excursion_and_return_The_ocean_Excursion_and_return","translated_internal_url":"","created_at":"2024-09-28T01:37:19.198-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":42455093,"work_id":124218655,"tagging_user_id":11956707,"tagged_user_id":295266502,"co_author_invite_id":null,"email":"a***t@gmail.com","display_order":1,"name":"Anders Omstedt","title":"The ocean: Excursion and return The ocean: Excursion and return"}],"downloadable_attachments":[{"id":118486198,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118486198/thumbnails/1.jpg","file_name":"Omstedt_and_Gustavsson_2022a.pdf","download_url":"https://www.academia.edu/attachments/118486198/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_ocean_Excursion_and_return_The_ocean.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118486198/Omstedt_and_Gustavsson_2022a-libre.pdf?1727513007=\u0026response-content-disposition=attachment%3B+filename%3DThe_ocean_Excursion_and_return_The_ocean.pdf\u0026Expires=1734108629\u0026Signature=MmyPLTi8DeMEWg6pJYMOeiAUmSPQS0VbokL5saZIHgzZuj0A~-lZ4R8S8QCxHHxnQf4qHlmXuTQRBNlXoiAtEnznDqpVDsM5unvUmoDUMA4YdAkP2dPmGEZ5zIlqrV3Nmm6RmjJMiqlCfXEr~uLHuZbswJ3h6Cat~ePt~uCbHhL4YAqm21Bb7f5JYQgUdwf4K6fe3coOcHgcn8~b-YHOFrALuR6lyzM~ZykNofZBYTEDNHVFt4KeV4x9j-NMxEs-NOaGC~oDMrBBhaviEfDXNw0ArXZjsyTj9X-yNJAkNY5NV5JxMQhmpga1yrXBzU1dz-GVcYydb7m3VXjcu5eSyA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_ocean_Excursion_and_return_The_ocean_Excursion_and_return","translated_slug":"","page_count":16,"language":"en","content_type":"Work","summary":"The ocean with its coastal seas is under increasing anthropogenic pressure, severely threatening ocean health and marine life. Human dependency on and management of the ocean are disconnected, which is in part why the United Nations (UN) is launching the Decade of Ocean Science for Sustainable Development, 2021-2030 (\"Ocean Decade\"). Here we investigate how philosophy and literature can inspire us to change the relationship between humans and the ocean. The starting point is natural science and human exploration of the sea. Then we consider philosophy, starting from Aristotle's forms of knowledge-episteme, techne, and phronesis-focusing particularly on phronesis, or practical wisdom. Referring to Homer's Odyssey, we investigate the threats that the ocean may face during the UN's Ocean Decade. From this, we identify several things that will make for a successful Ocean Decade: practical wise leadership, clear vision, societal involvement, information sharing, admitting the vulnerability of both the ocean and humans, and storytelling.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":118486198,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118486198/thumbnails/1.jpg","file_name":"Omstedt_and_Gustavsson_2022a.pdf","download_url":"https://www.academia.edu/attachments/118486198/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_ocean_Excursion_and_return_The_ocean.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118486198/Omstedt_and_Gustavsson_2022a-libre.pdf?1727513007=\u0026response-content-disposition=attachment%3B+filename%3DThe_ocean_Excursion_and_return_The_ocean.pdf\u0026Expires=1734108629\u0026Signature=MmyPLTi8DeMEWg6pJYMOeiAUmSPQS0VbokL5saZIHgzZuj0A~-lZ4R8S8QCxHHxnQf4qHlmXuTQRBNlXoiAtEnznDqpVDsM5unvUmoDUMA4YdAkP2dPmGEZ5zIlqrV3Nmm6RmjJMiqlCfXEr~uLHuZbswJ3h6Cat~ePt~uCbHhL4YAqm21Bb7f5JYQgUdwf4K6fe3coOcHgcn8~b-YHOFrALuR6lyzM~ZykNofZBYTEDNHVFt4KeV4x9j-NMxEs-NOaGC~oDMrBBhaviEfDXNw0ArXZjsyTj9X-yNJAkNY5NV5JxMQhmpga1yrXBzU1dz-GVcYydb7m3VXjcu5eSyA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":803,"name":"Philosophy","url":"https://www.academia.edu/Documents/in/Philosophy"},{"id":951,"name":"Humanities","url":"https://www.academia.edu/Documents/in/Humanities"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="124217854"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/124217854/A_Philosophic_View_of_the_Ocean_and_Humanity_Second_Edition"><img alt="Research paper thumbnail of A Philosophic View of the Ocean and Humanity. Second Edition" class="work-thumbnail" src="https://attachments.academia-assets.com/118485574/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/124217854/A_Philosophic_View_of_the_Ocean_and_Humanity_Second_Edition">A Philosophic View of the Ocean and Humanity. Second Edition</a></div><div class="wp-workCard_item"><span>Springer Nature</span><span>, 2024</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This new edition brings the reader into humans' challenges with the ocean and the future. It addr...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This new edition brings the reader into humans' challenges with the ocean and the future. It addresses the main questions in the United Nations Ocean Decade that aim to change how humans deal with the ocean. In the book's first part, art and dreaming are used as tools for connecting science and arts. This knowledge is applied in part II of the book, which is written in two modes: a concerned science mode and an intuitive, artistic mode in which the ocean is given a voice. Part II illustrates how science and art can be connected to increase our awareness of the state of the ocean and support behavioral change.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="f6e1789216b773f8e9d1f82f87c0288d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":118485574,"asset_id":124217854,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/118485574/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="124217854"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="124217854"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124217854; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124217854]").text(description); $(".js-view-count[data-work-id=124217854]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124217854; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124217854']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124217854, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "f6e1789216b773f8e9d1f82f87c0288d" } } $('.js-work-strip[data-work-id=124217854]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124217854,"title":"A Philosophic View of the Ocean and Humanity. Second Edition","translated_title":"","metadata":{"doi":"10.1007/978-3-031-64326-2","abstract":"This new edition brings the reader into humans' challenges with the ocean and the future. It addresses the main questions in the United Nations Ocean Decade that aim to change how humans deal with the ocean. In the book's first part, art and dreaming are used as tools for connecting science and arts. This knowledge is applied in part II of the book, which is written in two modes: a concerned science mode and an intuitive, artistic mode in which the ocean is given a voice. Part II illustrates how science and art can be connected to increase our awareness of the state of the ocean and support behavioral change.","publication_date":{"day":null,"month":null,"year":2024,"errors":{}},"publication_name":"Springer Nature"},"translated_abstract":"This new edition brings the reader into humans' challenges with the ocean and the future. It addresses the main questions in the United Nations Ocean Decade that aim to change how humans deal with the ocean. In the book's first part, art and dreaming are used as tools for connecting science and arts. This knowledge is applied in part II of the book, which is written in two modes: a concerned science mode and an intuitive, artistic mode in which the ocean is given a voice. Part II illustrates how science and art can be connected to increase our awareness of the state of the ocean and support behavioral change.","internal_url":"https://www.academia.edu/124217854/A_Philosophic_View_of_the_Ocean_and_Humanity_Second_Edition","translated_internal_url":"","created_at":"2024-09-28T00:57:25.118-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":118485574,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118485574/thumbnails/1.jpg","file_name":"New_book_Omstedt_2024.pdf","download_url":"https://www.academia.edu/attachments/118485574/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"A_Philosophic_View_of_the_Ocean_and_Huma.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118485574/New_book_Omstedt_2024-libre.pdf?1727512357=\u0026response-content-disposition=attachment%3B+filename%3DA_Philosophic_View_of_the_Ocean_and_Huma.pdf\u0026Expires=1734108629\u0026Signature=FUJ34K51LyoXy2JAf7HdWbeYCv~KcJn4THTeCa0ejw~4ZtSaBIzoS8gaxfxNHulHkMECsa8oIBKliDnIlwRJigKzbCailcFVMdL9uH6kXAdLQSs6Ve3-OKJR1fHFO-Mtvv2GVknZHhAJg6YouUQIT~cvF0VKradpwcIsNpKTtSdVed1JTvBkHM4VyjvsXr6KHc3j2XqH1bx2LvS8ok76pJqfjg0pd1Gmuqcbty0WUf-NxkJSYRJyr5aSipFcTEFS3XqNIyVY6wX2j4aumj4zpFHNqMVttFeQ7D~pq3B6MoAJ0zsge07I578LFCtQJUuYciZcgfPT7uogEDuzJ0EbdQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"A_Philosophic_View_of_the_Ocean_and_Humanity_Second_Edition","translated_slug":"","page_count":1,"language":"en","content_type":"Work","summary":"This new edition brings the reader into humans' challenges with the ocean and the future. It addresses the main questions in the United Nations Ocean Decade that aim to change how humans deal with the ocean. In the book's first part, art and dreaming are used as tools for connecting science and arts. This knowledge is applied in part II of the book, which is written in two modes: a concerned science mode and an intuitive, artistic mode in which the ocean is given a voice. Part II illustrates how science and art can be connected to increase our awareness of the state of the ocean and support behavioral change.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":118485574,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118485574/thumbnails/1.jpg","file_name":"New_book_Omstedt_2024.pdf","download_url":"https://www.academia.edu/attachments/118485574/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"A_Philosophic_View_of_the_Ocean_and_Huma.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118485574/New_book_Omstedt_2024-libre.pdf?1727512357=\u0026response-content-disposition=attachment%3B+filename%3DA_Philosophic_View_of_the_Ocean_and_Huma.pdf\u0026Expires=1734108629\u0026Signature=FUJ34K51LyoXy2JAf7HdWbeYCv~KcJn4THTeCa0ejw~4ZtSaBIzoS8gaxfxNHulHkMECsa8oIBKliDnIlwRJigKzbCailcFVMdL9uH6kXAdLQSs6Ve3-OKJR1fHFO-Mtvv2GVknZHhAJg6YouUQIT~cvF0VKradpwcIsNpKTtSdVed1JTvBkHM4VyjvsXr6KHc3j2XqH1bx2LvS8ok76pJqfjg0pd1Gmuqcbty0WUf-NxkJSYRJyr5aSipFcTEFS3XqNIyVY6wX2j4aumj4zpFHNqMVttFeQ7D~pq3B6MoAJ0zsge07I578LFCtQJUuYciZcgfPT7uogEDuzJ0EbdQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":3368098,"name":"UN Decade of Ocean Science for Sustainable Development 2021–2030","url":"https://www.academia.edu/Documents/in/UN_Decade_of_Ocean_Science_for_Sustainable_Development_2021_2030"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="124163370"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/124163370/Modeling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper"><img alt="Research paper thumbnail of Modeling the seasonal, interannual, and long-term variations of salinity and temperature in the Baltic proper" class="work-thumbnail" src="https://attachments.academia-assets.com/118437140/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/124163370/Modeling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper">Modeling the seasonal, interannual, and long-term variations of salinity and temperature in the Baltic proper</a></div><div class="wp-workCard_item"><span>Tellus A</span><span>, 1998</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with a numerical ocean model and a large amount of observational data. In the model, the Baltic Sea is divided into 13 sub-basins with high vertical resolution, horizontally coupled by barotropic and baroclinic flows and vertically coupled to a sea-ice model which includes dynamics as well as thermodynamics. The model was integrated for a 15-year period (1980-1995) by using observed meteorological forcing data, river-runoff data and sea-level data from the Kattegat. The calculated 15-year median profiles of salinity and temperature in the different sub-basins are in good agreement with observations. However, the calculated middepth salinities in the Arkona Basin and Bornholm Basin were somewhat overestimated, and the calculated deep-water temperatures in the Arkona Basin and the Bornholm Basin are somewhat lower than the observed values. Frontal mixing and movements in the Kattegat and the entrance area of the Arkona Basin were important to consider in the model. Water masses were simulated well, and prescribing constant deep-water properties in the Kattegat proved to be a reasonable lateral boundary condition. Further, comparisons were made between observed and calculated seasonal and interannual variations of the hydrographic properties in the Eastern Gotland Basin, as well as the interannual variations of the annual maximum ice extent. We conclude that the model can simulate these variations realistically. The major Baltic inflow of 1993 was also simulated by the model, but the inflowing water was 1-2°degrees too cold. Finally, the response times to changes in forcing of the Baltic proper and the Kattegat were investigated by performing the so-called lock-exchange experiment. Typical stratification spin-up times were of the order of 10 years for the Kattegat, and 100 years for the Baltic proper.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2ba3147406fab23bad91762e222a98e3" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":118437140,"asset_id":124163370,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/118437140/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="124163370"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="124163370"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124163370; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124163370]").text(description); $(".js-view-count[data-work-id=124163370]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124163370; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124163370']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124163370, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "2ba3147406fab23bad91762e222a98e3" } } $('.js-work-strip[data-work-id=124163370]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124163370,"title":"Modeling the seasonal, interannual, and long-term variations of salinity and temperature in the Baltic proper","translated_title":"","metadata":{"publisher":"Wiley-Blackwell","grobid_abstract":"Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with a numerical ocean model and a large amount of observational data. In the model, the Baltic Sea is divided into 13 sub-basins with high vertical resolution, horizontally coupled by barotropic and baroclinic flows and vertically coupled to a sea-ice model which includes dynamics as well as thermodynamics. The model was integrated for a 15-year period (1980-1995) by using observed meteorological forcing data, river-runoff data and sea-level data from the Kattegat. The calculated 15-year median profiles of salinity and temperature in the different sub-basins are in good agreement with observations. However, the calculated middepth salinities in the Arkona Basin and Bornholm Basin were somewhat overestimated, and the calculated deep-water temperatures in the Arkona Basin and the Bornholm Basin are somewhat lower than the observed values. Frontal mixing and movements in the Kattegat and the entrance area of the Arkona Basin were important to consider in the model. Water masses were simulated well, and prescribing constant deep-water properties in the Kattegat proved to be a reasonable lateral boundary condition. Further, comparisons were made between observed and calculated seasonal and interannual variations of the hydrographic properties in the Eastern Gotland Basin, as well as the interannual variations of the annual maximum ice extent. We conclude that the model can simulate these variations realistically. The major Baltic inflow of 1993 was also simulated by the model, but the inflowing water was 1-2°degrees too cold. Finally, the response times to changes in forcing of the Baltic proper and the Kattegat were investigated by performing the so-called lock-exchange experiment. Typical stratification spin-up times were of the order of 10 years for the Kattegat, and 100 years for the Baltic proper.","publication_date":{"day":null,"month":null,"year":1998,"errors":{}},"publication_name":"Tellus A","grobid_abstract_attachment_id":118437140},"translated_abstract":null,"internal_url":"https://www.academia.edu/124163370/Modeling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper","translated_internal_url":"","created_at":"2024-09-25T12:18:23.987-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":118437140,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118437140/thumbnails/1.jpg","file_name":"tellusa.v50i5.pdf","download_url":"https://www.academia.edu/attachments/118437140/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modeling_the_seasonal_interannual_and_lo.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118437140/tellusa.v50i5-libre.pdf?1727293002=\u0026response-content-disposition=attachment%3B+filename%3DModeling_the_seasonal_interannual_and_lo.pdf\u0026Expires=1734108629\u0026Signature=SpM1ljj~GH7Wi45QfnfWKsr9Aa9Y~-RFMPUAfKEbAQERywUhFXgB2pte4Cv3ytWr3zcRw1sanSlnzQqbPFBmXHvLz7ar1TinMAQokKB9Q1IyU4FducEr9mD9gd4Uw8sk~ybjZAQzOKwltaWx3fLuqSUosKHYXlnanTeOkjRlwcsz6Xl~H69x7dUnNSuSfThpec-ISzxnqDzDAImL1tT-EpyONhWMd2p5A5xm4xgI0Lgz1hUAwSEFhNrAOUMwiN05JEM~Y3hPRa69UtMu7tVDrLZCaICVvbU8ZXCW7p6VAYxqjnz1umnO~-KXUdC998ef8DIEPSJnZpOVMziWXOsQkw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Modeling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper","translated_slug":"","page_count":17,"language":"en","content_type":"Work","summary":"Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with a numerical ocean model and a large amount of observational data. In the model, the Baltic Sea is divided into 13 sub-basins with high vertical resolution, horizontally coupled by barotropic and baroclinic flows and vertically coupled to a sea-ice model which includes dynamics as well as thermodynamics. The model was integrated for a 15-year period (1980-1995) by using observed meteorological forcing data, river-runoff data and sea-level data from the Kattegat. The calculated 15-year median profiles of salinity and temperature in the different sub-basins are in good agreement with observations. However, the calculated middepth salinities in the Arkona Basin and Bornholm Basin were somewhat overestimated, and the calculated deep-water temperatures in the Arkona Basin and the Bornholm Basin are somewhat lower than the observed values. Frontal mixing and movements in the Kattegat and the entrance area of the Arkona Basin were important to consider in the model. Water masses were simulated well, and prescribing constant deep-water properties in the Kattegat proved to be a reasonable lateral boundary condition. Further, comparisons were made between observed and calculated seasonal and interannual variations of the hydrographic properties in the Eastern Gotland Basin, as well as the interannual variations of the annual maximum ice extent. We conclude that the model can simulate these variations realistically. The major Baltic inflow of 1993 was also simulated by the model, but the inflowing water was 1-2°degrees too cold. Finally, the response times to changes in forcing of the Baltic proper and the Kattegat were investigated by performing the so-called lock-exchange experiment. Typical stratification spin-up times were of the order of 10 years for the Kattegat, and 100 years for the Baltic proper.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":118437140,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118437140/thumbnails/1.jpg","file_name":"tellusa.v50i5.pdf","download_url":"https://www.academia.edu/attachments/118437140/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modeling_the_seasonal_interannual_and_lo.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118437140/tellusa.v50i5-libre.pdf?1727293002=\u0026response-content-disposition=attachment%3B+filename%3DModeling_the_seasonal_interannual_and_lo.pdf\u0026Expires=1734108629\u0026Signature=SpM1ljj~GH7Wi45QfnfWKsr9Aa9Y~-RFMPUAfKEbAQERywUhFXgB2pte4Cv3ytWr3zcRw1sanSlnzQqbPFBmXHvLz7ar1TinMAQokKB9Q1IyU4FducEr9mD9gd4Uw8sk~ybjZAQzOKwltaWx3fLuqSUosKHYXlnanTeOkjRlwcsz6Xl~H69x7dUnNSuSfThpec-ISzxnqDzDAImL1tT-EpyONhWMd2p5A5xm4xgI0Lgz1hUAwSEFhNrAOUMwiN05JEM~Y3hPRa69UtMu7tVDrLZCaICVvbU8ZXCW7p6VAYxqjnz1umnO~-KXUdC998ef8DIEPSJnZpOVMziWXOsQkw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":3754,"name":"Climatology","url":"https://www.academia.edu/Documents/in/Climatology"},{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences"},{"id":82107,"name":"Salinity","url":"https://www.academia.edu/Documents/in/Salinity"},{"id":410933,"name":"Baltic Sea","url":"https://www.academia.edu/Documents/in/Baltic_Sea"},{"id":597110,"name":"Tellus","url":"https://www.academia.edu/Documents/in/Tellus"}],"urls":[{"id":44824946,"url":"https://doi.org/10.3402/tellusa.v50i5.14563"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="124163369"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/124163369/Modelling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper"><img alt="Research paper thumbnail of Modelling the seasonal, interannual, and long-term variations of salinity and temperature in the Baltic proper" class="work-thumbnail" src="https://attachments.academia-assets.com/118437131/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/124163369/Modelling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper">Modelling the seasonal, interannual, and long-term variations of salinity and temperature in the Baltic proper</a></div><div class="wp-workCard_item"><span>Tellus A</span><span>, Oct 1, 1998</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with a numerical ocean model and a large amount of observational data. In the model, the Baltic Sea is divided into 13 sub-basins with high vertical resolution, horizontally coupled by barotropic and baroclinic flows and vertically coupled to a sea-ice model which includes dynamics as well as thermodynamics. The model was integrated for a 15-year period (1980-1995) by using observed meteorological forcing data, river-runoff data and sea-level data from the Kattegat. The calculated 15-year median profiles of salinity and temperature in the different sub-basins are in good agreement with observations. However, the calculated middepth salinities in the Arkona Basin and Bornholm Basin were somewhat overestimated, and the calculated deep-water temperatures in the Arkona Basin and the Bornholm Basin are somewhat lower than the observed values. Frontal mixing and movements in the Kattegat and the entrance area of the Arkona Basin were important to consider in the model. Water masses were simulated well, and prescribing constant deep-water properties in the Kattegat proved to be a reasonable lateral boundary condition. Further, comparisons were made between observed and calculated seasonal and interannual variations of the hydrographic properties in the Eastern Gotland Basin, as well as the interannual variations of the annual maximum ice extent. We conclude that the model can simulate these variations realistically. The major Baltic inflow of 1993 was also simulated by the model, but the inflowing water was 1-2°degrees too cold. Finally, the response times to changes in forcing of the Baltic proper and the Kattegat were investigated by performing the so-called lock-exchange experiment. Typical stratification spin-up times were of the order of 10 years for the Kattegat, and 100 years for the Baltic proper.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d637ae3d1f6ea7b38bff16a3014d3a1d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":118437131,"asset_id":124163369,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/118437131/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="124163369"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="124163369"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124163369; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124163369]").text(description); $(".js-view-count[data-work-id=124163369]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124163369; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124163369']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124163369, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "d637ae3d1f6ea7b38bff16a3014d3a1d" } } $('.js-work-strip[data-work-id=124163369]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124163369,"title":"Modelling the seasonal, interannual, and long-term variations of salinity and temperature in the Baltic proper","translated_title":"","metadata":{"publisher":"Wiley-Blackwell","ai_title_tag":"Modeling Salinity and Temperature Variations in the Baltic Sea","grobid_abstract":"Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with a numerical ocean model and a large amount of observational data. In the model, the Baltic Sea is divided into 13 sub-basins with high vertical resolution, horizontally coupled by barotropic and baroclinic flows and vertically coupled to a sea-ice model which includes dynamics as well as thermodynamics. The model was integrated for a 15-year period (1980-1995) by using observed meteorological forcing data, river-runoff data and sea-level data from the Kattegat. The calculated 15-year median profiles of salinity and temperature in the different sub-basins are in good agreement with observations. However, the calculated middepth salinities in the Arkona Basin and Bornholm Basin were somewhat overestimated, and the calculated deep-water temperatures in the Arkona Basin and the Bornholm Basin are somewhat lower than the observed values. Frontal mixing and movements in the Kattegat and the entrance area of the Arkona Basin were important to consider in the model. Water masses were simulated well, and prescribing constant deep-water properties in the Kattegat proved to be a reasonable lateral boundary condition. Further, comparisons were made between observed and calculated seasonal and interannual variations of the hydrographic properties in the Eastern Gotland Basin, as well as the interannual variations of the annual maximum ice extent. We conclude that the model can simulate these variations realistically. The major Baltic inflow of 1993 was also simulated by the model, but the inflowing water was 1-2°degrees too cold. Finally, the response times to changes in forcing of the Baltic proper and the Kattegat were investigated by performing the so-called lock-exchange experiment. Typical stratification spin-up times were of the order of 10 years for the Kattegat, and 100 years for the Baltic proper.","publication_date":{"day":1,"month":10,"year":1998,"errors":{}},"publication_name":"Tellus A","grobid_abstract_attachment_id":118437131},"translated_abstract":null,"internal_url":"https://www.academia.edu/124163369/Modelling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper","translated_internal_url":"","created_at":"2024-09-25T12:18:23.298-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":118437131,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118437131/thumbnails/1.jpg","file_name":"FULLTEXT01.pdf","download_url":"https://www.academia.edu/attachments/118437131/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modelling_the_seasonal_interannual_and_l.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118437131/FULLTEXT01-libre.pdf?1727292998=\u0026response-content-disposition=attachment%3B+filename%3DModelling_the_seasonal_interannual_and_l.pdf\u0026Expires=1734108629\u0026Signature=N2KqejAq3cG-esDgv3psiHiv4YulWJuHsgpk6A4UX9gljeQieBI83OCvy447T8-IY7d-qgWdD5hrXIB4xjRJRvHYz79c9jbcVMZ5ym45bRvEbHWQv2T1KbVhC6KTpRLv0MTYcUWnngI~dDYL~9Lok9c55jSL-C3MB9cMpAtKCAgzhLZeGCRL8l9rMhKltkRCd4Q59x-9rxUxN~zI8J7HxZwHTN1gQBplZzp~-UHekP4-5gfkXFOyBZG45wX~YQQ5G2xMR56xgdO6I26DhG5TEeFVWHzveKTLU1tm2UwPgyWTqPJ3~B0w5-lTbbyiwMAdul3MIOIfgJnS~wM6iVC93A__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Modelling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper","translated_slug":"","page_count":16,"language":"en","content_type":"Work","summary":"Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with a numerical ocean model and a large amount of observational data. In the model, the Baltic Sea is divided into 13 sub-basins with high vertical resolution, horizontally coupled by barotropic and baroclinic flows and vertically coupled to a sea-ice model which includes dynamics as well as thermodynamics. The model was integrated for a 15-year period (1980-1995) by using observed meteorological forcing data, river-runoff data and sea-level data from the Kattegat. The calculated 15-year median profiles of salinity and temperature in the different sub-basins are in good agreement with observations. However, the calculated middepth salinities in the Arkona Basin and Bornholm Basin were somewhat overestimated, and the calculated deep-water temperatures in the Arkona Basin and the Bornholm Basin are somewhat lower than the observed values. Frontal mixing and movements in the Kattegat and the entrance area of the Arkona Basin were important to consider in the model. Water masses were simulated well, and prescribing constant deep-water properties in the Kattegat proved to be a reasonable lateral boundary condition. Further, comparisons were made between observed and calculated seasonal and interannual variations of the hydrographic properties in the Eastern Gotland Basin, as well as the interannual variations of the annual maximum ice extent. We conclude that the model can simulate these variations realistically. The major Baltic inflow of 1993 was also simulated by the model, but the inflowing water was 1-2°degrees too cold. Finally, the response times to changes in forcing of the Baltic proper and the Kattegat were investigated by performing the so-called lock-exchange experiment. Typical stratification spin-up times were of the order of 10 years for the Kattegat, and 100 years for the Baltic proper.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":118437131,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118437131/thumbnails/1.jpg","file_name":"FULLTEXT01.pdf","download_url":"https://www.academia.edu/attachments/118437131/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modelling_the_seasonal_interannual_and_l.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118437131/FULLTEXT01-libre.pdf?1727292998=\u0026response-content-disposition=attachment%3B+filename%3DModelling_the_seasonal_interannual_and_l.pdf\u0026Expires=1734108629\u0026Signature=N2KqejAq3cG-esDgv3psiHiv4YulWJuHsgpk6A4UX9gljeQieBI83OCvy447T8-IY7d-qgWdD5hrXIB4xjRJRvHYz79c9jbcVMZ5ym45bRvEbHWQv2T1KbVhC6KTpRLv0MTYcUWnngI~dDYL~9Lok9c55jSL-C3MB9cMpAtKCAgzhLZeGCRL8l9rMhKltkRCd4Q59x-9rxUxN~zI8J7HxZwHTN1gQBplZzp~-UHekP4-5gfkXFOyBZG45wX~YQQ5G2xMR56xgdO6I26DhG5TEeFVWHzveKTLU1tm2UwPgyWTqPJ3~B0w5-lTbbyiwMAdul3MIOIfgJnS~wM6iVC93A__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":3754,"name":"Climatology","url":"https://www.academia.edu/Documents/in/Climatology"},{"id":57433,"name":"Seasonality","url":"https://www.academia.edu/Documents/in/Seasonality"},{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences"},{"id":82107,"name":"Salinity","url":"https://www.academia.edu/Documents/in/Salinity"},{"id":597110,"name":"Tellus","url":"https://www.academia.edu/Documents/in/Tellus"}],"urls":[{"id":44824945,"url":"http://smhi.diva-portal.org/smash/get/diva2:850981/FULLTEXT01"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="124163342"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/124163342/H%C3%A5llbara_kustsamh%C3%A4llen_i_l%C3%A5ngtidsperspektiv_G%C3%B6teborg_3_4_maj_och_1_2_november_2010"><img alt="Research paper thumbnail of Hållbara kustsamhällen i långtidsperspektiv, Göteborg 3–4 maj och 1–2 november 2010" class="work-thumbnail" src="https://attachments.academia-assets.com/118437110/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/124163342/H%C3%A5llbara_kustsamh%C3%A4llen_i_l%C3%A5ngtidsperspektiv_G%C3%B6teborg_3_4_maj_och_1_2_november_2010">Hållbara kustsamhällen i långtidsperspektiv, Göteborg 3–4 maj och 1–2 november 2010</a></div><div class="wp-workCard_item"><span>Historisk Tidsskrift</span><span>, Jun 7, 2011</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="9c2538ddea1f114606fd7a8647978587" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":118437110,"asset_id":124163342,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/118437110/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="124163342"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="124163342"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124163342; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124163342]").text(description); $(".js-view-count[data-work-id=124163342]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124163342; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124163342']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124163342, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "9c2538ddea1f114606fd7a8647978587" } } $('.js-work-strip[data-work-id=124163342]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124163342,"title":"Hållbara kustsamhällen i långtidsperspektiv, Göteborg 3–4 maj och 1–2 november 2010","translated_title":"","metadata":{"publisher":"Scandinavian University Press/Universitetsforlaget","publication_date":{"day":7,"month":6,"year":2011,"errors":{}},"publication_name":"Historisk Tidsskrift"},"translated_abstract":null,"internal_url":"https://www.academia.edu/124163342/H%C3%A5llbara_kustsamh%C3%A4llen_i_l%C3%A5ngtidsperspektiv_G%C3%B6teborg_3_4_maj_och_1_2_november_2010","translated_internal_url":"","created_at":"2024-09-25T12:16:46.893-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":118437110,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118437110/thumbnails/1.jpg","file_name":"HT_2011_2_417-418_hansson_omstedt.pdf","download_url":"https://www.academia.edu/attachments/118437110/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Hallbara_kustsamhallen_i_langtidsperspek.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118437110/HT_2011_2_417-418_hansson_omstedt-libre.pdf?1727293007=\u0026response-content-disposition=attachment%3B+filename%3DHallbara_kustsamhallen_i_langtidsperspek.pdf\u0026Expires=1734108629\u0026Signature=V7d6T0BV67iZKzFnrttP1Ki9Ajosd8MeRQ24jSrqGCKLr0G12Y9supiZXyPtLzdCQcBkyRDo-3blb3Ww3mcelL7u5sgodbUfBKtwVX-pLw3qns8GH5ouD9W3N7jISz7BgXDHPwq7g01ulU3TdI-oogqHMG~m4CxkeKqu6pTVr0UqwPUG8nlfg3-FTbqGKsJ3AvVwa5IbDdf~GiQiK05fpbDegg5JbFY-MQCx8y1J6z6YoayB5fu4FKrFg6HZsg0QENAw2NNl6Ay1nzyHyvFbyAtQjDow-y4VMTnimPONT9VPygW04BlG~7dVgSrvuoz8WORi5RDG74-Pd~Sz1u2UxQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Hållbara_kustsamhällen_i_långtidsperspektiv_Göteborg_3_4_maj_och_1_2_november_2010","translated_slug":"","page_count":3,"language":"sv","content_type":"Work","summary":null,"owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":118437110,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118437110/thumbnails/1.jpg","file_name":"HT_2011_2_417-418_hansson_omstedt.pdf","download_url":"https://www.academia.edu/attachments/118437110/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Hallbara_kustsamhallen_i_langtidsperspek.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118437110/HT_2011_2_417-418_hansson_omstedt-libre.pdf?1727293007=\u0026response-content-disposition=attachment%3B+filename%3DHallbara_kustsamhallen_i_langtidsperspek.pdf\u0026Expires=1734108629\u0026Signature=V7d6T0BV67iZKzFnrttP1Ki9Ajosd8MeRQ24jSrqGCKLr0G12Y9supiZXyPtLzdCQcBkyRDo-3blb3Ww3mcelL7u5sgodbUfBKtwVX-pLw3qns8GH5ouD9W3N7jISz7BgXDHPwq7g01ulU3TdI-oogqHMG~m4CxkeKqu6pTVr0UqwPUG8nlfg3-FTbqGKsJ3AvVwa5IbDdf~GiQiK05fpbDegg5JbFY-MQCx8y1J6z6YoayB5fu4FKrFg6HZsg0QENAw2NNl6Ay1nzyHyvFbyAtQjDow-y4VMTnimPONT9VPygW04BlG~7dVgSrvuoz8WORi5RDG74-Pd~Sz1u2UxQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"},{"id":118437111,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118437111/thumbnails/1.jpg","file_name":"HT_2011_2_417-418_hansson_omstedt.pdf","download_url":"https://www.academia.edu/attachments/118437111/download_file","bulk_download_file_name":"Hallbara_kustsamhallen_i_langtidsperspek.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118437111/HT_2011_2_417-418_hansson_omstedt-libre.pdf?1727293007=\u0026response-content-disposition=attachment%3B+filename%3DHallbara_kustsamhallen_i_langtidsperspek.pdf\u0026Expires=1734108629\u0026Signature=Lj0WCHSXHtyi~oo6dSQmUDaz9qGvQvyyIuAjGjO756aGylvLdXquQ~nMTd8-ZcitU2S3dUKdc2HYfih4VBJktQbCQCtq7Y0abrEzjS9dyCM0blKSWhhW2g1NUNRgvlzXA1PFILfyo0wTtD~LK2wcgqfbm8PlSPwJuA4X74mxhnvRPWaxQqilQm7eyRPVl4lSUIZe7nKvcxOGJgmkXyTyTNXlkoP8kXn5lAyMvHUncInXmsLKCR3VOyXckbH1~Rnq7xqBUsAoQ-TNltc0x40X17g30D0NN8in2u9EWSRpgKp6liw71UyKljsVMHUI25zwXAPFYllJH1~WUaIVforWqw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[],"urls":[{"id":44824927,"url":"http://www.historisktidskrift.se/fulltext/2011-2/pdf/HT_2011_2_417-418_hansson_omstedt.pdf"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="121518601"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/121518601/Deep_water_properties_in_the_Gulf_of_Bothnia"><img alt="Research paper thumbnail of Deep water properties in the Gulf of Bothnia" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/121518601/Deep_water_properties_in_the_Gulf_of_Bothnia">Deep water properties in the Gulf of Bothnia</a></div><div class="wp-workCard_item"><span>Continental Shelf Research</span><span>, Feb 1, 1993</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">ABSTRACT The northern extension of the Baltic Sea, the Gulf of Bothnia, is a weakly stratified se...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">ABSTRACT The northern extension of the Baltic Sea, the Gulf of Bothnia, is a weakly stratified sea. One would therefore expect that the deep water of the Gulf is easily renewed through deep thermal convection, or even through deep haline convection, as the Gulf is more or less covered with ice every winter. However, the present study shows, through analysis of historical temperature, salinity and density data, that the deep water in the Gulf of Bothnia is mainly renewed by major inflows of Baltic Proper surface water. The penetrating water forms a dense bottom current in the Gulf. In the southern part of the Gulf, the Bothnian Sea, the volume flow of the bottom current is found to increase by 10%. It is therefore not likely that the bottom current properties are changed to any appreciable extent. The bottom current properties in the Bothnian Bay, on the other hand, are highly affected, as the volume flow is estimated to increase by 150% in this basin.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="121518601"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="121518601"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 121518601; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=121518601]").text(description); $(".js-view-count[data-work-id=121518601]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 121518601; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='121518601']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 121518601, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=121518601]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":121518601,"title":"Deep water properties in the Gulf of Bothnia","translated_title":"","metadata":{"abstract":"ABSTRACT The northern extension of the Baltic Sea, the Gulf of Bothnia, is a weakly stratified sea. One would therefore expect that the deep water of the Gulf is easily renewed through deep thermal convection, or even through deep haline convection, as the Gulf is more or less covered with ice every winter. However, the present study shows, through analysis of historical temperature, salinity and density data, that the deep water in the Gulf of Bothnia is mainly renewed by major inflows of Baltic Proper surface water. The penetrating water forms a dense bottom current in the Gulf. In the southern part of the Gulf, the Bothnian Sea, the volume flow of the bottom current is found to increase by 10%. It is therefore not likely that the bottom current properties are changed to any appreciable extent. The bottom current properties in the Bothnian Bay, on the other hand, are highly affected, as the volume flow is estimated to increase by 150% in this basin.","publisher":"Elsevier BV","publication_date":{"day":1,"month":2,"year":1993,"errors":{}},"publication_name":"Continental Shelf Research"},"translated_abstract":"ABSTRACT The northern extension of the Baltic Sea, the Gulf of Bothnia, is a weakly stratified sea. One would therefore expect that the deep water of the Gulf is easily renewed through deep thermal convection, or even through deep haline convection, as the Gulf is more or less covered with ice every winter. However, the present study shows, through analysis of historical temperature, salinity and density data, that the deep water in the Gulf of Bothnia is mainly renewed by major inflows of Baltic Proper surface water. The penetrating water forms a dense bottom current in the Gulf. In the southern part of the Gulf, the Bothnian Sea, the volume flow of the bottom current is found to increase by 10%. It is therefore not likely that the bottom current properties are changed to any appreciable extent. The bottom current properties in the Bothnian Bay, on the other hand, are highly affected, as the volume flow is estimated to increase by 150% in this basin.","internal_url":"https://www.academia.edu/121518601/Deep_water_properties_in_the_Gulf_of_Bothnia","translated_internal_url":"","created_at":"2024-06-26T00:10:51.257-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Deep_water_properties_in_the_Gulf_of_Bothnia","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"ABSTRACT The northern extension of the Baltic Sea, the Gulf of Bothnia, is a weakly stratified sea. One would therefore expect that the deep water of the Gulf is easily renewed through deep thermal convection, or even through deep haline convection, as the Gulf is more or less covered with ice every winter. However, the present study shows, through analysis of historical temperature, salinity and density data, that the deep water in the Gulf of Bothnia is mainly renewed by major inflows of Baltic Proper surface water. The penetrating water forms a dense bottom current in the Gulf. In the southern part of the Gulf, the Bothnian Sea, the volume flow of the bottom current is found to increase by 10%. It is therefore not likely that the bottom current properties are changed to any appreciable extent. The bottom current properties in the Bothnian Bay, on the other hand, are highly affected, as the volume flow is estimated to increase by 150% in this basin.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":82107,"name":"Salinity","url":"https://www.academia.edu/Documents/in/Salinity"},{"id":230435,"name":"Continental shelf","url":"https://www.academia.edu/Documents/in/Continental_shelf"},{"id":322541,"name":"Deep water","url":"https://www.academia.edu/Documents/in/Deep_water"},{"id":1660649,"name":"Bay","url":"https://www.academia.edu/Documents/in/Bay"}],"urls":[{"id":43238854,"url":"https://doi.org/10.1016/0278-4343(93)90104-6"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275453"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/117275453/Modeling_the_variations_of_salinity_and_temperature_in_the_large_Gulfs_of_the_Baltic_Sea"><img alt="Research paper thumbnail of Modeling the variations of salinity and temperature in the large Gulfs of the Baltic Sea" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/117275453/Modeling_the_variations_of_salinity_and_temperature_in_the_large_Gulfs_of_the_Baltic_Sea">Modeling the variations of salinity and temperature in the large Gulfs of the Baltic Sea</a></div><div class="wp-workCard_item"><span>Continental Shelf Research</span><span>, Feb 1, 2003</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">ABSTRACT The modeling of salinity and temperature in Gulf of Bothnia, Gulf of Finland, and Gulf o...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">ABSTRACT The modeling of salinity and temperature in Gulf of Bothnia, Gulf of Finland, and Gulf of Riga is investigated by using a coupled sea ice-ocean Baltic Sea model. 18 years, from late 1980 to the end of 1998, have been investigated. The forcing data extracted taken from a gridded meteorological data base, sea level data from the Kattegat, and river runoff data to the different subbasins of the Baltic Sea from a hydrological data base. To improve the gridded meteorological data base a statistical model for the reduction of geostrophic winds to surface winds was developed. In the analysis it was shown that the calculated long-term salinity and temperature structures were stable and in good agreement with observations. This was made possible by using three different strait-flow models connecting the subbasins of the Baltic Sea. The seasonal and interannual variations of temperature and salinity were also well simulated by the model, implying that the coupling between the atmosphere and the Baltic Sea as well as the diapycnal mixing are reasonably well understood. The water cycle and the surface heat balance were calculated using the 18-year simulation. In the water-balance calculations it was shown that the volume flows from the large gulfs of the Baltic Sea were mainly due to baroclinic transports and that net precipitation added freshwater during the studied period, particularly to the large gulfs. From the heat-balance calculation it is concluded that the Baltic Sea is almost in local balance with the atmosphere. The Bothnian Bay, Gulf of Finland and Gulf of Riga loose heat, whereas the Bothnian Sea gains heat, calculated as long-term means.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275453"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275453"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275453; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275453]").text(description); $(".js-view-count[data-work-id=117275453]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275453; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275453']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275453, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275453]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275453,"title":"Modeling the variations of salinity and temperature in the large Gulfs of the Baltic Sea","translated_title":"","metadata":{"abstract":"ABSTRACT The modeling of salinity and temperature in Gulf of Bothnia, Gulf of Finland, and Gulf of Riga is investigated by using a coupled sea ice-ocean Baltic Sea model. 18 years, from late 1980 to the end of 1998, have been investigated. The forcing data extracted taken from a gridded meteorological data base, sea level data from the Kattegat, and river runoff data to the different subbasins of the Baltic Sea from a hydrological data base. To improve the gridded meteorological data base a statistical model for the reduction of geostrophic winds to surface winds was developed. In the analysis it was shown that the calculated long-term salinity and temperature structures were stable and in good agreement with observations. This was made possible by using three different strait-flow models connecting the subbasins of the Baltic Sea. The seasonal and interannual variations of temperature and salinity were also well simulated by the model, implying that the coupling between the atmosphere and the Baltic Sea as well as the diapycnal mixing are reasonably well understood. The water cycle and the surface heat balance were calculated using the 18-year simulation. In the water-balance calculations it was shown that the volume flows from the large gulfs of the Baltic Sea were mainly due to baroclinic transports and that net precipitation added freshwater during the studied period, particularly to the large gulfs. From the heat-balance calculation it is concluded that the Baltic Sea is almost in local balance with the atmosphere. The Bothnian Bay, Gulf of Finland and Gulf of Riga loose heat, whereas the Bothnian Sea gains heat, calculated as long-term means.","publisher":"Elsevier BV","publication_date":{"day":1,"month":2,"year":2003,"errors":{}},"publication_name":"Continental Shelf Research"},"translated_abstract":"ABSTRACT The modeling of salinity and temperature in Gulf of Bothnia, Gulf of Finland, and Gulf of Riga is investigated by using a coupled sea ice-ocean Baltic Sea model. 18 years, from late 1980 to the end of 1998, have been investigated. The forcing data extracted taken from a gridded meteorological data base, sea level data from the Kattegat, and river runoff data to the different subbasins of the Baltic Sea from a hydrological data base. To improve the gridded meteorological data base a statistical model for the reduction of geostrophic winds to surface winds was developed. In the analysis it was shown that the calculated long-term salinity and temperature structures were stable and in good agreement with observations. This was made possible by using three different strait-flow models connecting the subbasins of the Baltic Sea. The seasonal and interannual variations of temperature and salinity were also well simulated by the model, implying that the coupling between the atmosphere and the Baltic Sea as well as the diapycnal mixing are reasonably well understood. The water cycle and the surface heat balance were calculated using the 18-year simulation. In the water-balance calculations it was shown that the volume flows from the large gulfs of the Baltic Sea were mainly due to baroclinic transports and that net precipitation added freshwater during the studied period, particularly to the large gulfs. From the heat-balance calculation it is concluded that the Baltic Sea is almost in local balance with the atmosphere. The Bothnian Bay, Gulf of Finland and Gulf of Riga loose heat, whereas the Bothnian Sea gains heat, calculated as long-term means.","internal_url":"https://www.academia.edu/117275453/Modeling_the_variations_of_salinity_and_temperature_in_the_large_Gulfs_of_the_Baltic_Sea","translated_internal_url":"","created_at":"2024-04-09T07:54:16.818-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Modeling_the_variations_of_salinity_and_temperature_in_the_large_Gulfs_of_the_Baltic_Sea","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"ABSTRACT The modeling of salinity and temperature in Gulf of Bothnia, Gulf of Finland, and Gulf of Riga is investigated by using a coupled sea ice-ocean Baltic Sea model. 18 years, from late 1980 to the end of 1998, have been investigated. The forcing data extracted taken from a gridded meteorological data base, sea level data from the Kattegat, and river runoff data to the different subbasins of the Baltic Sea from a hydrological data base. To improve the gridded meteorological data base a statistical model for the reduction of geostrophic winds to surface winds was developed. In the analysis it was shown that the calculated long-term salinity and temperature structures were stable and in good agreement with observations. This was made possible by using three different strait-flow models connecting the subbasins of the Baltic Sea. The seasonal and interannual variations of temperature and salinity were also well simulated by the model, implying that the coupling between the atmosphere and the Baltic Sea as well as the diapycnal mixing are reasonably well understood. The water cycle and the surface heat balance were calculated using the 18-year simulation. In the water-balance calculations it was shown that the volume flows from the large gulfs of the Baltic Sea were mainly due to baroclinic transports and that net precipitation added freshwater during the studied period, particularly to the large gulfs. From the heat-balance calculation it is concluded that the Baltic Sea is almost in local balance with the atmosphere. The Bothnian Bay, Gulf of Finland and Gulf of Riga loose heat, whereas the Bothnian Sea gains heat, calculated as long-term means.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":82107,"name":"Salinity","url":"https://www.academia.edu/Documents/in/Salinity"},{"id":230435,"name":"Continental shelf","url":"https://www.academia.edu/Documents/in/Continental_shelf"},{"id":410933,"name":"Baltic Sea","url":"https://www.academia.edu/Documents/in/Baltic_Sea"}],"urls":[{"id":40966784,"url":"https://doi.org/10.1016/s0278-4343(02)00207-8"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275452"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275452/Sea_ICE_75_Dynamical_Report"><img alt="Research paper thumbnail of Sea ICE-75. Dynamical Report" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275452/Sea_ICE_75_Dynamical_Report">Sea ICE-75. Dynamical Report</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Field measurements on sea ice was carried out in the Bay of Bothnia during March 10-20, 1975. The...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Field measurements on sea ice was carried out in the Bay of Bothnia during March 10-20, 1975. The forces and parameters in the equation of motion for sea ice have been studied on the Mesoscale. Winds and currents were measured to calculate the wind and water stress, the ice mass distribution was studied, the tilting of the sea surface computed, vertical temperature and salinity soundings in the water made and surface temperatures at different ice types measured.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275452"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275452"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275452; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275452]").text(description); $(".js-view-count[data-work-id=117275452]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275452; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275452']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275452, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275452]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275452,"title":"Sea ICE-75. Dynamical Report","translated_title":"","metadata":{"abstract":"Field measurements on sea ice was carried out in the Bay of Bothnia during March 10-20, 1975. The forces and parameters in the equation of motion for sea ice have been studied on the Mesoscale. Winds and currents were measured to calculate the wind and water stress, the ice mass distribution was studied, the tilting of the sea surface computed, vertical temperature and salinity soundings in the water made and surface temperatures at different ice types measured.","publication_date":{"day":null,"month":null,"year":1976,"errors":{}}},"translated_abstract":"Field measurements on sea ice was carried out in the Bay of Bothnia during March 10-20, 1975. The forces and parameters in the equation of motion for sea ice have been studied on the Mesoscale. Winds and currents were measured to calculate the wind and water stress, the ice mass distribution was studied, the tilting of the sea surface computed, vertical temperature and salinity soundings in the water made and surface temperatures at different ice types measured.","internal_url":"https://www.academia.edu/117275452/Sea_ICE_75_Dynamical_Report","translated_internal_url":"","created_at":"2024-04-09T07:54:16.436-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Sea_ICE_75_Dynamical_Report","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Field measurements on sea ice was carried out in the Bay of Bothnia during March 10-20, 1975. The forces and parameters in the equation of motion for sea ice have been studied on the Mesoscale. Winds and currents were measured to calculate the wind and water stress, the ice mass distribution was studied, the tilting of the sea surface computed, vertical temperature and salinity soundings in the water made and surface temperatures at different ice types measured.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt","email":"eVZLQXFwL2JZcStJVG4yN0N2Z3dzeUNsRDl0bjBCbG13eittK3ZsMGpPb0VvVE5NcFQ2cnB3Wmc3NUk4YVVUbi0tVjROSmxKK0tEd3BCSDRCOUorclI0UT09--b13fb099a32cff0d392b5e31dfa4bd95e798ce39"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":29759,"name":"Sea Ice","url":"https://www.academia.edu/Documents/in/Sea_Ice"},{"id":73591,"name":"Mesoscale Meteorology","url":"https://www.academia.edu/Documents/in/Mesoscale_Meteorology"}],"urls":[{"id":40966782,"url":"https://trid.trb.org/view/57067"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275451"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275451/PEP_in_Baltex_A_pilot_study_of_evaporation_and_precipitation_in_the_Baltic_Sea"><img alt="Research paper thumbnail of PEP in Baltex. A pilot study of evaporation and precipitation in the Baltic Sea" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275451/PEP_in_Baltex_A_pilot_study_of_evaporation_and_precipitation_in_the_Baltic_Sea">PEP in Baltex. A pilot study of evaporation and precipitation in the Baltic Sea</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275451"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275451"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275451; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275451]").text(description); $(".js-view-count[data-work-id=117275451]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275451; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275451']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275451, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275451]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275451,"title":"PEP in Baltex. A pilot study of evaporation and precipitation in the Baltic Sea","translated_title":"","metadata":{"publication_date":{"day":null,"month":null,"year":1998,"errors":{}}},"translated_abstract":null,"internal_url":"https://www.academia.edu/117275451/PEP_in_Baltex_A_pilot_study_of_evaporation_and_precipitation_in_the_Baltic_Sea","translated_internal_url":"","created_at":"2024-04-09T07:54:16.214-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"PEP_in_Baltex_A_pilot_study_of_evaporation_and_precipitation_in_the_Baltic_Sea","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":null,"owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt","email":"NEVZRW9obXQyREVtMENCWk5RZitCZjNOWnIyUTllRzNpU003L2RtU05uS2dkMzg3VlNuYndCYXZFdEpZMld5Ni0tWjBMVVBOdzZnMWVGZlJNSXB5Z1Bydz09--cfcb616d0f4119db283e9fe797096b80cf00674a"},"attachments":[],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":13268,"name":"Evaporation","url":"https://www.academia.edu/Documents/in/Evaporation"},{"id":291658,"name":"Precipitation","url":"https://www.academia.edu/Documents/in/Precipitation"},{"id":410933,"name":"Baltic Sea","url":"https://www.academia.edu/Documents/in/Baltic_Sea"}],"urls":[{"id":40966781,"url":"https://dissem.in/p/16015199/pep-in-baltex-a-pilot-study-of-evaporation-and-precipitation-in-the-baltic-sea"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275449"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275449/On_cooling_and_initial_ice_formation_in_the_upper_layers_of_the_ocean"><img alt="Research paper thumbnail of On cooling and initial ice formation in the upper layers of the ocean" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275449/On_cooling_and_initial_ice_formation_in_the_upper_layers_of_the_ocean">On cooling and initial ice formation in the upper layers of the ocean</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275449"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275449"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275449; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275449]").text(description); $(".js-view-count[data-work-id=117275449]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275449; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275449']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275449, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275449]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275449,"title":"On cooling and initial ice formation in the upper layers of the ocean","translated_title":"","metadata":{"publication_date":{"day":null,"month":null,"year":1985,"errors":{}}},"translated_abstract":null,"internal_url":"https://www.academia.edu/117275449/On_cooling_and_initial_ice_formation_in_the_upper_layers_of_the_ocean","translated_internal_url":"","created_at":"2024-04-09T07:54:15.896-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"On_cooling_and_initial_ice_formation_in_the_upper_layers_of_the_ocean","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":null,"owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt","email":"VmJoaDNOMWticTNpcDIxR0JHSjhSSU10S0JpZDJBYzhVUDc1SFN4amYzVnlYMHh4VmZ5VWNZNzZpL01PL3VTTC0tNW9pTVJ4Z21xcHpHT1NSbzl1dkViZz09--b929e09b31687532af2a5c24d988cc8b98bb102f"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":29759,"name":"Sea Ice","url":"https://www.academia.edu/Documents/in/Sea_Ice"},{"id":77936,"name":"Text","url":"https://www.academia.edu/Documents/in/Text"},{"id":793808,"name":"Oceanografi","url":"https://www.academia.edu/Documents/in/Oceanografi"}],"urls":[{"id":40966780,"url":"https://gupea.ub.gu.se/handle/2077/13499"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275448"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275448/Forecasting_Ice_on_Lakes_Estuaries_and_Shelf_Seas"><img alt="Research paper thumbnail of Forecasting Ice on Lakes, Estuaries and Shelf Seas" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275448/Forecasting_Ice_on_Lakes_Estuaries_and_Shelf_Seas">Forecasting Ice on Lakes, Estuaries and Shelf Seas</a></div><div class="wp-workCard_item"><span>Springer eBooks</span><span>, 1999</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275448"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275448"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275448; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275448]").text(description); $(".js-view-count[data-work-id=117275448]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275448; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275448']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275448, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275448]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275448,"title":"Forecasting Ice on Lakes, Estuaries and Shelf Seas","translated_title":"","metadata":{"publisher":"Springer Nature","publication_date":{"day":null,"month":null,"year":1999,"errors":{}},"publication_name":"Springer eBooks"},"translated_abstract":null,"internal_url":"https://www.academia.edu/117275448/Forecasting_Ice_on_Lakes_Estuaries_and_Shelf_Seas","translated_internal_url":"","created_at":"2024-04-09T07:54:15.457-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Forecasting_Ice_on_Lakes_Estuaries_and_Shelf_Seas","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":null,"owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt","email":"WHZYSXRicmQ3c0IyVWtKaG50Z0xsbFMvVDNBcDJnVkJRT2pEUlZhcFdqRFBVQnRybkxCTUFUVUkxL3pjNTdpZS0tOEZKOTNQWFo4czBjaXF6bE4zZGMrdz09--98bf4ab95909fc140fe6c330564c08f493b56a1e"},"attachments":[],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":3755,"name":"Meteorology","url":"https://www.academia.edu/Documents/in/Meteorology"},{"id":905684,"name":"Shore","url":"https://www.academia.edu/Documents/in/Shore"},{"id":3647879,"name":"Springer Ebooks","url":"https://www.academia.edu/Documents/in/Springer_Ebooks"}],"urls":[{"id":40966779,"url":"https://doi.org/10.1007/978-3-642-60030-2_11"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275447"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275447/Parameterization_of_lake_thermodynamics_in_a_high_resolution_weather_forecasting_model"><img alt="Research paper thumbnail of Parameterization of lake thermodynamics in a high-resolution weather forecasting model" class="work-thumbnail" src="https://attachments.academia-assets.com/113175442/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275447/Parameterization_of_lake_thermodynamics_in_a_high_resolution_weather_forecasting_model">Parameterization of lake thermodynamics in a high-resolution weather forecasting model</a></div><div class="wp-workCard_item"><span>Tellus A</span><span>, Oct 1, 1996</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="44c5775b16cc24118032c7dcc3786e95" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":113175442,"asset_id":117275447,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/113175442/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275447"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275447"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275447; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275447]").text(description); $(".js-view-count[data-work-id=117275447]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275447; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275447']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275447, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "44c5775b16cc24118032c7dcc3786e95" } } $('.js-work-strip[data-work-id=117275447]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275447,"title":"Parameterization of lake thermodynamics in a high-resolution weather forecasting model","translated_title":"","metadata":{"publisher":"Wiley-Blackwell","publication_date":{"day":1,"month":10,"year":1996,"errors":{}},"publication_name":"Tellus A"},"translated_abstract":null,"internal_url":"https://www.academia.edu/117275447/Parameterization_of_lake_thermodynamics_in_a_high_resolution_weather_forecasting_model","translated_internal_url":"","created_at":"2024-04-09T07:54:14.796-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":113175442,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175442/thumbnails/1.jpg","file_name":"FULLTEXT01.pdf","download_url":"https://www.academia.edu/attachments/113175442/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Parameterization_of_lake_thermodynamics.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175442/FULLTEXT01-libre.pdf?1712674808=\u0026response-content-disposition=attachment%3B+filename%3DParameterization_of_lake_thermodynamics.pdf\u0026Expires=1734108629\u0026Signature=Bww2asKYXAc49r7-C2fFE~66zZeugVvbU3pwjOVX~mCZoSLOvmLEnYQtDYaATiD4rBGQHNGkmMdMlQHEe1xTgRRoyHh2GeVxztVd72f0dvYE-n3sQdE3fUIsmWVzJTIcikuE30U~Q5u4PQGqcc8CoDs8alR5TbiEzE0tuT630UKEeUvY6to0zosuU~C1AotRUHO-RWGsfV1hswMY1ckZybDqAaIqBc19LsD3KAfnhK7IViF7TNa5QIfxNUOuzqURhF7euRTDNfiwnhjENnleqT~JIF2GQpVkmVYi9iWpAZ83wtbTYEISxsb9VFTAoJsRNzkmoxnjaAo0UthKuMqTww__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Parameterization_of_lake_thermodynamics_in_a_high_resolution_weather_forecasting_model","translated_slug":"","page_count":14,"language":"en","content_type":"Work","summary":null,"owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":113175442,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175442/thumbnails/1.jpg","file_name":"FULLTEXT01.pdf","download_url":"https://www.academia.edu/attachments/113175442/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Parameterization_of_lake_thermodynamics.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175442/FULLTEXT01-libre.pdf?1712674808=\u0026response-content-disposition=attachment%3B+filename%3DParameterization_of_lake_thermodynamics.pdf\u0026Expires=1734108629\u0026Signature=Bww2asKYXAc49r7-C2fFE~66zZeugVvbU3pwjOVX~mCZoSLOvmLEnYQtDYaATiD4rBGQHNGkmMdMlQHEe1xTgRRoyHh2GeVxztVd72f0dvYE-n3sQdE3fUIsmWVzJTIcikuE30U~Q5u4PQGqcc8CoDs8alR5TbiEzE0tuT630UKEeUvY6to0zosuU~C1AotRUHO-RWGsfV1hswMY1ckZybDqAaIqBc19LsD3KAfnhK7IViF7TNa5QIfxNUOuzqURhF7euRTDNfiwnhjENnleqT~JIF2GQpVkmVYi9iWpAZ83wtbTYEISxsb9VFTAoJsRNzkmoxnjaAo0UthKuMqTww__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"},{"id":113175441,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175441/thumbnails/1.jpg","file_name":"FULLTEXT01.pdf","download_url":"https://www.academia.edu/attachments/113175441/download_file","bulk_download_file_name":"Parameterization_of_lake_thermodynamics.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175441/FULLTEXT01-libre.pdf?1712674810=\u0026response-content-disposition=attachment%3B+filename%3DParameterization_of_lake_thermodynamics.pdf\u0026Expires=1734108629\u0026Signature=NOF5Kae7Ah-Cnz1m8txSp7JNdrIHTkdYl1iGom-dIWmC3mnb1qngI6Ojai~tMeF9W2H0mEi3zfidZNgR6RnAXDzJuG13DGtkk~yOz8iRPcS6tawMnAn6VS1fRKU2S-v7jCa40ILlKI-UjyCDQvUbTaug2tuEFwjtczYWn4HtwJcj57jOrAzV6XkY1R5ADEKvwMGci4l5Da4lncxhzRnmRD4D5qfjFGCd2gi7puT3PJt-62Wv-rUTE-k3FEXQ3dvmca07JmjSEXRUi20xRqGF369baqpMslc-ApSYLLlklI3hGlu2m1qogxN3nwFd-I2bxInFS7HjhPOb~ZVjQ0pUnA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":522,"name":"Thermodynamics","url":"https://www.academia.edu/Documents/in/Thermodynamics"},{"id":3754,"name":"Climatology","url":"https://www.academia.edu/Documents/in/Climatology"},{"id":5980,"name":"Atmospheric Modeling","url":"https://www.academia.edu/Documents/in/Atmospheric_Modeling"},{"id":6962,"name":"Energy Conservation","url":"https://www.academia.edu/Documents/in/Energy_Conservation"},{"id":57433,"name":"Seasonality","url":"https://www.academia.edu/Documents/in/Seasonality"},{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences"},{"id":195260,"name":"Weather Forecasting","url":"https://www.academia.edu/Documents/in/Weather_Forecasting"},{"id":309086,"name":"High Resolution","url":"https://www.academia.edu/Documents/in/High_Resolution"},{"id":391216,"name":"Size Distribution","url":"https://www.academia.edu/Documents/in/Size_Distribution"},{"id":444096,"name":"Air Temperature","url":"https://www.academia.edu/Documents/in/Air_Temperature"},{"id":468734,"name":"Turbulent Mixing","url":"https://www.academia.edu/Documents/in/Turbulent_Mixing"},{"id":597110,"name":"Tellus","url":"https://www.academia.edu/Documents/in/Tellus"}],"urls":[{"id":40966778,"url":"https://smhi.diva-portal.org/smash/get/diva2:897786/FULLTEXT01"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275444"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275444/Stratification_Turbulence_and_Services"><img alt="Research paper thumbnail of Stratification, Turbulence, and Services" class="work-thumbnail" src="https://attachments.academia-assets.com/113175436/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275444/Stratification_Turbulence_and_Services">Stratification, Turbulence, and Services</a></div><div class="wp-workCard_item"><span>A Philosophical View of the Ocean and Humanity</span><span>, 2020</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This chapter continues the dialogue between science and the ocean, starting with a concerned scie...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This chapter continues the dialogue between science and the ocean, starting with a concerned science view. A great fear is that global warming may reduce areas of sinking water, reducing ocean ventilation. The ocean responds with an image of a kelp forest-among the most beautiful and biologically productive marine ecosystems, and one that has served the ocean for many millions of years. Interpreting the kelp forest as a metaphor suggests a need to listen better and realize that humans can develop a society in a similar way, as a rich habitat for human growth with diverse groups of people in a healthy environment. For this to happen, human attitudes need to change to create a society that serves the ocean as kelp forests do. Keywords Ocean • Coastal seas • Climate change • Environmental change • Connecting science and the arts • Sustainability • Oceanography • Psychology • Philosophy Voice of the ocean: It is such a joy to serve life. Some of you speak of 'green thumbs', but I have 'brown fingers' that for millions of years have protected and served life. Listen carefully.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="1dd1e10b214775637fd73efbdfce951d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":113175436,"asset_id":117275444,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/113175436/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275444"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275444"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275444; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275444]").text(description); $(".js-view-count[data-work-id=117275444]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275444; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275444']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275444, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "1dd1e10b214775637fd73efbdfce951d" } } $('.js-work-strip[data-work-id=117275444]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275444,"title":"Stratification, Turbulence, and Services","translated_title":"","metadata":{"publisher":"Springer International Publishing","grobid_abstract":"This chapter continues the dialogue between science and the ocean, starting with a concerned science view. A great fear is that global warming may reduce areas of sinking water, reducing ocean ventilation. The ocean responds with an image of a kelp forest-among the most beautiful and biologically productive marine ecosystems, and one that has served the ocean for many millions of years. Interpreting the kelp forest as a metaphor suggests a need to listen better and realize that humans can develop a society in a similar way, as a rich habitat for human growth with diverse groups of people in a healthy environment. For this to happen, human attitudes need to change to create a society that serves the ocean as kelp forests do. Keywords Ocean • Coastal seas • Climate change • Environmental change • Connecting science and the arts • Sustainability • Oceanography • Psychology • Philosophy Voice of the ocean: It is such a joy to serve life. Some of you speak of 'green thumbs', but I have 'brown fingers' that for millions of years have protected and served life. Listen carefully.","publication_date":{"day":null,"month":null,"year":2020,"errors":{}},"publication_name":"A Philosophical View of the Ocean and Humanity","grobid_abstract_attachment_id":113175436},"translated_abstract":null,"internal_url":"https://www.academia.edu/117275444/Stratification_Turbulence_and_Services","translated_internal_url":"","created_at":"2024-04-09T07:54:13.999-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":113175436,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175436/thumbnails/1.jpg","file_name":"978-3-030-36680-3_5.pdf","download_url":"https://www.academia.edu/attachments/113175436/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Stratification_Turbulence_and_Services.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175436/978-3-030-36680-3_5-libre.pdf?1712674805=\u0026response-content-disposition=attachment%3B+filename%3DStratification_Turbulence_and_Services.pdf\u0026Expires=1734108629\u0026Signature=SdGTPIwRNEIV1kUmZ5k84rqZuZAb3Z1iCgCxyLdIo3~yWr4ROmbAeu4QhkYdTIyYBFax7Oz4HZg6zPZL7KRh-njLLnm4-ayALSL9LnRsqBWfTJiabBT3HfG9xOR8p~fpdM8sVa7lWMhMsyazWHBrTImCNwwu6Y90CMr9eWFslc21DLeBto3BaPEAUuEqaCqYmU8VfmdzAWAKdmwpIWKikrRO6gBcM-OQ4ioerc~Eeb10QtrDobO~4SQOvsEJgaXnvAP0y8gMDeIWqw-2hFZryjtEWN-RZyZdqX63VwSaX3AM34xEDdhpF-uKlvuR27nRovLfxv7VJfmNEMiJiSeziA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Stratification_Turbulence_and_Services","translated_slug":"","page_count":5,"language":"en","content_type":"Work","summary":"This chapter continues the dialogue between science and the ocean, starting with a concerned science view. A great fear is that global warming may reduce areas of sinking water, reducing ocean ventilation. The ocean responds with an image of a kelp forest-among the most beautiful and biologically productive marine ecosystems, and one that has served the ocean for many millions of years. Interpreting the kelp forest as a metaphor suggests a need to listen better and realize that humans can develop a society in a similar way, as a rich habitat for human growth with diverse groups of people in a healthy environment. For this to happen, human attitudes need to change to create a society that serves the ocean as kelp forests do. Keywords Ocean • Coastal seas • Climate change • Environmental change • Connecting science and the arts • Sustainability • Oceanography • Psychology • Philosophy Voice of the ocean: It is such a joy to serve life. Some of you speak of 'green thumbs', but I have 'brown fingers' that for millions of years have protected and served life. Listen carefully.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":113175436,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175436/thumbnails/1.jpg","file_name":"978-3-030-36680-3_5.pdf","download_url":"https://www.academia.edu/attachments/113175436/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Stratification_Turbulence_and_Services.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175436/978-3-030-36680-3_5-libre.pdf?1712674805=\u0026response-content-disposition=attachment%3B+filename%3DStratification_Turbulence_and_Services.pdf\u0026Expires=1734108629\u0026Signature=SdGTPIwRNEIV1kUmZ5k84rqZuZAb3Z1iCgCxyLdIo3~yWr4ROmbAeu4QhkYdTIyYBFax7Oz4HZg6zPZL7KRh-njLLnm4-ayALSL9LnRsqBWfTJiabBT3HfG9xOR8p~fpdM8sVa7lWMhMsyazWHBrTImCNwwu6Y90CMr9eWFslc21DLeBto3BaPEAUuEqaCqYmU8VfmdzAWAKdmwpIWKikrRO6gBcM-OQ4ioerc~Eeb10QtrDobO~4SQOvsEJgaXnvAP0y8gMDeIWqw-2hFZryjtEWN-RZyZdqX63VwSaX3AM34xEDdhpF-uKlvuR27nRovLfxv7VJfmNEMiJiSeziA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"},{"id":113175435,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175435/thumbnails/1.jpg","file_name":"978-3-030-36680-3_5.pdf","download_url":"https://www.academia.edu/attachments/113175435/download_file","bulk_download_file_name":"Stratification_Turbulence_and_Services.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175435/978-3-030-36680-3_5-libre.pdf?1712674804=\u0026response-content-disposition=attachment%3B+filename%3DStratification_Turbulence_and_Services.pdf\u0026Expires=1734108629\u0026Signature=Igbm4yQSUm8W1I-fL5~-KGXMJKrHguHdg1PouApRUkRC2asXYoYazYrrEzRfKF~U8SOF-e~GcoiJ0zPd~Bzctgmo4aK-tJGmXm6xlzp~sgsJaVtCw1-TsQFY5Fa0mYJG~GwFCcVcX5Jmyilq-Og0tVXycRUo-a5-hMeBgybDtx6uEFye5OdrVGViY~2K3LpbSBttWmlIVMSKgPem3lx10vBBM6ZnnRPGo8NqJZpO6qUzPLHX8J-Y4vd-S9P9~47zkJOFh29R5KBvPjSYXu9kQ6uIdPNkspuizjM2DYz-XYmO4FLossljA6rdwWkRdQxl8d3XXDoH-sErtjaD4m7Xmw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":85707,"name":"Habitat","url":"https://www.academia.edu/Documents/in/Habitat"},{"id":104980,"name":"Kelp Forest","url":"https://www.academia.edu/Documents/in/Kelp_Forest"},{"id":740846,"name":"Kelp","url":"https://www.academia.edu/Documents/in/Kelp"}],"urls":[{"id":40966776,"url":"http://link.springer.com/content/pdf/10.1007/978-3-030-36680-3_5"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275442"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275442/Ecosystems_and_Listening"><img alt="Research paper thumbnail of Ecosystems and Listening" class="work-thumbnail" src="https://attachments.academia-assets.com/113175432/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275442/Ecosystems_and_Listening">Ecosystems and Listening</a></div><div class="wp-workCard_item"><span>A Philosophical View of the Ocean and Humanity</span><span>, 2020</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This chapter highlights the conflict between human activity and marine ecosystems. The decline of...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This chapter highlights the conflict between human activity and marine ecosystems. The decline of various marine species due to human impact goes back more than a millennium but accelerated markedly in the 1950s. Hemingway wrote about the shift from sustainable to unsustainable attitudes towards fishing in his 1952 novel The Old Man and the Sea. Beautiful living marine resources are now mismanaged as if humanity and the ocean no longer had any relationship with each other. The ocean responds with disappointment at human lifestyles and attitudes, and invites us to listen better and realize that marine resources could give much more back if managed properly. Keywords Ocean • Coastal seas • Climate change • Environmental change • Connecting science and the arts • Sustainability • Oceanography • Psychology • Philosophy Voice of the ocean: I am so disappointed with humans' greedy approach to my beautiful living resources. You must listen better to me and to your hearts, and realize my limits in supporting you. If you listen carefully to me, all my resources can be much better used and, yes, I loved the dories. The northwestern Atlantic Ocean, where the cold Arctic water meets the warm Atlantic water, is a biologically rich area with abundant phytoplankton, zooplankton, and krill and historically excellent fishing conditions. For many centuries, the Grand Banks of Newfoundland were the site of large-scale fishing efforts. From small dories, fishers could catch cod, haddock, and other species of fish, which were then brought to the main fishing vessel that could serve a large number of dories and fishers. Little changed for several centuries and the Grand Banks remained an area with abundant marine resources. Each dory was generally handled by one or two fishers, who filled it with fish caught using hooks and lines. Rowing and sailing these boats, about five to six metres long, required great skill, and the fishers were well known for handling these boats under difficult and dangerous conditions, sometimes during fog when they lost contact with the mother ship. The first documented single-handed sailing across the Atlantic was by Alfred Johnson in 1876 using a five-metre dory. His voyage went from Gloucester, Massachusetts, USA to Abercastle, Wales and lasted 58 days (Kurlansky 1999).</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="04ecbad08a41010069834faba5739e69" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":113175432,"asset_id":117275442,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/113175432/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275442"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275442"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275442; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275442]").text(description); $(".js-view-count[data-work-id=117275442]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275442; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275442']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275442, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "04ecbad08a41010069834faba5739e69" } } $('.js-work-strip[data-work-id=117275442]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275442,"title":"Ecosystems and Listening","translated_title":"","metadata":{"publisher":"Springer International Publishing","grobid_abstract":"This chapter highlights the conflict between human activity and marine ecosystems. The decline of various marine species due to human impact goes back more than a millennium but accelerated markedly in the 1950s. Hemingway wrote about the shift from sustainable to unsustainable attitudes towards fishing in his 1952 novel The Old Man and the Sea. Beautiful living marine resources are now mismanaged as if humanity and the ocean no longer had any relationship with each other. The ocean responds with disappointment at human lifestyles and attitudes, and invites us to listen better and realize that marine resources could give much more back if managed properly. Keywords Ocean • Coastal seas • Climate change • Environmental change • Connecting science and the arts • Sustainability • Oceanography • Psychology • Philosophy Voice of the ocean: I am so disappointed with humans' greedy approach to my beautiful living resources. You must listen better to me and to your hearts, and realize my limits in supporting you. If you listen carefully to me, all my resources can be much better used and, yes, I loved the dories. The northwestern Atlantic Ocean, where the cold Arctic water meets the warm Atlantic water, is a biologically rich area with abundant phytoplankton, zooplankton, and krill and historically excellent fishing conditions. For many centuries, the Grand Banks of Newfoundland were the site of large-scale fishing efforts. From small dories, fishers could catch cod, haddock, and other species of fish, which were then brought to the main fishing vessel that could serve a large number of dories and fishers. Little changed for several centuries and the Grand Banks remained an area with abundant marine resources. Each dory was generally handled by one or two fishers, who filled it with fish caught using hooks and lines. Rowing and sailing these boats, about five to six metres long, required great skill, and the fishers were well known for handling these boats under difficult and dangerous conditions, sometimes during fog when they lost contact with the mother ship. The first documented single-handed sailing across the Atlantic was by Alfred Johnson in 1876 using a five-metre dory. His voyage went from Gloucester, Massachusetts, USA to Abercastle, Wales and lasted 58 days (Kurlansky 1999).","publication_date":{"day":null,"month":null,"year":2020,"errors":{}},"publication_name":"A Philosophical View of the Ocean and Humanity","grobid_abstract_attachment_id":113175432},"translated_abstract":null,"internal_url":"https://www.academia.edu/117275442/Ecosystems_and_Listening","translated_internal_url":"","created_at":"2024-04-09T07:54:13.004-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":113175432,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175432/thumbnails/1.jpg","file_name":"978-3-030-36680-3_11.pdf","download_url":"https://www.academia.edu/attachments/113175432/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Ecosystems_and_Listening.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175432/978-3-030-36680-3_11-libre.pdf?1712674805=\u0026response-content-disposition=attachment%3B+filename%3DEcosystems_and_Listening.pdf\u0026Expires=1734108629\u0026Signature=UR5eu7FKWSaTm6biVyuAUJDUfsQgeahlqoUaoi-4wuNBX9a6Ghu3qIxiBfnQIjGYlz8dLmsqcP~End-sPooFaf-YYffdt4pt9xIyclr~LnUVBHS7ZJE7gY1YxV-Fx6U7QIbIpZ7u6GkH1RkYuxDKRYAEEZuFA9KHJL4lLPhrnEIcKak4EYlQUJKSF6WhnYJsfq4QeYaBdi4GgwL24i9-PZDAMnYMejEZsQBOYTwajvop1T0moXxUhcxCKoAo2ndVkcOM0GWNZ5UjGOWE33n1QpSG2SOXFVxSJAlDMymzCdf2l68fllYDl9gbChJVklFSGHeyXxie-BPqTRhpJGO-vw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Ecosystems_and_Listening","translated_slug":"","page_count":6,"language":"en","content_type":"Work","summary":"This chapter highlights the conflict between human activity and marine ecosystems. The decline of various marine species due to human impact goes back more than a millennium but accelerated markedly in the 1950s. Hemingway wrote about the shift from sustainable to unsustainable attitudes towards fishing in his 1952 novel The Old Man and the Sea. Beautiful living marine resources are now mismanaged as if humanity and the ocean no longer had any relationship with each other. The ocean responds with disappointment at human lifestyles and attitudes, and invites us to listen better and realize that marine resources could give much more back if managed properly. Keywords Ocean • Coastal seas • Climate change • Environmental change • Connecting science and the arts • Sustainability • Oceanography • Psychology • Philosophy Voice of the ocean: I am so disappointed with humans' greedy approach to my beautiful living resources. You must listen better to me and to your hearts, and realize my limits in supporting you. If you listen carefully to me, all my resources can be much better used and, yes, I loved the dories. The northwestern Atlantic Ocean, where the cold Arctic water meets the warm Atlantic water, is a biologically rich area with abundant phytoplankton, zooplankton, and krill and historically excellent fishing conditions. For many centuries, the Grand Banks of Newfoundland were the site of large-scale fishing efforts. From small dories, fishers could catch cod, haddock, and other species of fish, which were then brought to the main fishing vessel that could serve a large number of dories and fishers. Little changed for several centuries and the Grand Banks remained an area with abundant marine resources. Each dory was generally handled by one or two fishers, who filled it with fish caught using hooks and lines. Rowing and sailing these boats, about five to six metres long, required great skill, and the fishers were well known for handling these boats under difficult and dangerous conditions, sometimes during fog when they lost contact with the mother ship. The first documented single-handed sailing across the Atlantic was by Alfred Johnson in 1876 using a five-metre dory. His voyage went from Gloucester, Massachusetts, USA to Abercastle, Wales and lasted 58 days (Kurlansky 1999).","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":113175432,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175432/thumbnails/1.jpg","file_name":"978-3-030-36680-3_11.pdf","download_url":"https://www.academia.edu/attachments/113175432/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Ecosystems_and_Listening.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175432/978-3-030-36680-3_11-libre.pdf?1712674805=\u0026response-content-disposition=attachment%3B+filename%3DEcosystems_and_Listening.pdf\u0026Expires=1734108629\u0026Signature=UR5eu7FKWSaTm6biVyuAUJDUfsQgeahlqoUaoi-4wuNBX9a6Ghu3qIxiBfnQIjGYlz8dLmsqcP~End-sPooFaf-YYffdt4pt9xIyclr~LnUVBHS7ZJE7gY1YxV-Fx6U7QIbIpZ7u6GkH1RkYuxDKRYAEEZuFA9KHJL4lLPhrnEIcKak4EYlQUJKSF6WhnYJsfq4QeYaBdi4GgwL24i9-PZDAMnYMejEZsQBOYTwajvop1T0moXxUhcxCKoAo2ndVkcOM0GWNZ5UjGOWE33n1QpSG2SOXFVxSJAlDMymzCdf2l68fllYDl9gbChJVklFSGHeyXxie-BPqTRhpJGO-vw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"},{"id":113175431,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175431/thumbnails/1.jpg","file_name":"978-3-030-36680-3_11.pdf","download_url":"https://www.academia.edu/attachments/113175431/download_file","bulk_download_file_name":"Ecosystems_and_Listening.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175431/978-3-030-36680-3_11-libre.pdf?1712674804=\u0026response-content-disposition=attachment%3B+filename%3DEcosystems_and_Listening.pdf\u0026Expires=1734108629\u0026Signature=WyxnlEYXH6W~FvGZoHNcbr2jgfDVdben4jV1sUJaBw9MksauwZFl8Ts6-2xhsZG3HGH4g3KbwoPkd55t6625-L55jbVwZxRMBEivHJd1gdSWU2-E6lBYMp~FiVPCPPnwjyL6XWec4IOqIMvIdvC09RXDLH4iDDn1H4M0RQY5OilkaS2oeFe5Hu8JDLewMre4rvCNWw2N8kFLIXxTL6EMx4bYBh~21W76LJO9~IjeUGQZBsbgLp55TLqplWFiAfo9S4NItqrHow~OXSbjjiPHpgkOK7M1AyoFxSDtjwJgcPme9tKCarbuallPkVcdtuatP9q~lCI8CwlSoGRJ7CjLrQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":54534,"name":"Humanity","url":"https://www.academia.edu/Documents/in/Humanity"},{"id":79742,"name":"Fishing","url":"https://www.academia.edu/Documents/in/Fishing"},{"id":209760,"name":"Disappointment","url":"https://www.academia.edu/Documents/in/Disappointment"},{"id":1022026,"name":"Marine ecosystem","url":"https://www.academia.edu/Documents/in/Marine_ecosystem"}],"urls":[{"id":40966773,"url":"http://link.springer.com/content/pdf/10.1007/978-3-030-36680-3_11"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275438"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275438/Replication_Data_for_A_new_numerical_model_for_understanding_free_and_dissolved_gas_progression_towards_the_atmosphere_in_aquatic_methane_seepage_systems"><img alt="Research paper thumbnail of Replication Data for: A new numerical model for understanding free and dissolved gas progression towards the atmosphere in aquatic methane seepage systems" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275438/Replication_Data_for_A_new_numerical_model_for_understanding_free_and_dissolved_gas_progression_towards_the_atmosphere_in_aquatic_methane_seepage_systems">Replication Data for: A new numerical model for understanding free and dissolved gas progression towards the atmosphere in aquatic methane seepage systems</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This dataset contains the files needed to replicate the reference simulation results of the numer...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This dataset contains the files needed to replicate the reference simulation results of the numerical model M2PG1. Please refer to the README.txt file for detailed instructions on how to reproduce the simulation results.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275438"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275438"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275438; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275438]").text(description); $(".js-view-count[data-work-id=117275438]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275438; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275438']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275438, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275438]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275438,"title":"Replication Data for: A new numerical model for understanding free and dissolved gas progression towards the atmosphere in aquatic methane seepage systems","translated_title":"","metadata":{"abstract":"This dataset contains the files needed to replicate the reference simulation results of the numerical model M2PG1. Please refer to the README.txt file for detailed instructions on how to reproduce the simulation results.","publication_date":{"day":null,"month":null,"year":2019,"errors":{}}},"translated_abstract":"This dataset contains the files needed to replicate the reference simulation results of the numerical model M2PG1. Please refer to the README.txt file for detailed instructions on how to reproduce the simulation results.","internal_url":"https://www.academia.edu/117275438/Replication_Data_for_A_new_numerical_model_for_understanding_free_and_dissolved_gas_progression_towards_the_atmosphere_in_aquatic_methane_seepage_systems","translated_internal_url":"","created_at":"2024-04-09T07:54:06.718-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Replication_Data_for_A_new_numerical_model_for_understanding_free_and_dissolved_gas_progression_towards_the_atmosphere_in_aquatic_methane_seepage_systems","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"This dataset contains the files needed to replicate the reference simulation results of the numerical model M2PG1. Please refer to the README.txt file for detailed instructions on how to reproduce the simulation results.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt","email":"SFBpV0c3eHZUOHNoK3diUmR2eDRVc3F0QXhoeUZGcVhiSTRUTjJQWWxFd3ExdGozV0trK1JjRGpEeWtBQXFtMC0tVXRVam13Nm9PRlNSQ1RZQjU0cXU1Zz09--d03f91ee0a1c2cf5db286d15e8b4944546f3bf14"},"attachments":[],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":156347,"name":"Methane","url":"https://www.academia.edu/Documents/in/Methane"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275437"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275437/Currents_Circulation_and_Vulnerability"><img alt="Research paper thumbnail of Currents, Circulation, and Vulnerability" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275437/Currents_Circulation_and_Vulnerability">Currents, Circulation, and Vulnerability</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275437"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275437"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275437; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275437]").text(description); $(".js-view-count[data-work-id=117275437]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275437; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275437']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275437, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275437]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275437,"title":"Currents, Circulation, and Vulnerability","translated_title":"","metadata":{"publication_date":{"day":null,"month":null,"year":2020,"errors":{}}},"translated_abstract":null,"internal_url":"https://www.academia.edu/117275437/Currents_Circulation_and_Vulnerability","translated_internal_url":"","created_at":"2024-04-09T07:54:06.404-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Currents_Circulation_and_Vulnerability","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":null,"owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt","email":"bExBNzVTRGZ6U09HSjl6YnZrc29HbEFxM1RoTnJrNXVXM0Z2aWMzdDRVcGpzc0RvZ0tUWDdNMXlkSWxJNGdmZy0tRnRCdUhQNDNhbWY1aWVNUWg3RWFoQT09--9309c9f008c3836ac098a2fbb7f64b81d7db9d6e"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":604678,"name":"Eddy","url":"https://www.academia.edu/Documents/in/Eddy"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275436"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/117275436/Variations_of_ice_properties_in_an_ice_area_of_1x2_km_in_the_Gulf_of_Bothnia_March_1988"><img alt="Research paper thumbnail of Variations of ice properties in an ice area of 1x2 km in the Gulf of Bothnia March 1988" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/117275436/Variations_of_ice_properties_in_an_ice_area_of_1x2_km_in_the_Gulf_of_Bothnia_March_1988">Variations of ice properties in an ice area of 1x2 km in the Gulf of Bothnia March 1988</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">During the Bothnian Experiment in Preparation for ERS-1 (BEPERS-88), snow and ice thickness, sali...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">During the Bothnian Experiment in Preparation for ERS-1 (BEPERS-88), snow and ice thickness, salinity, density, crystal shape and ice strength were investigated. In a rectangular area of 1 x 2km, data from 12 stations is presented. The area covered level-ice, several pressure ridges and a belt of rafted and hummocked ice. The origin of the ice is discussed based on information given from vertical thin sections at different stations. Index values of ice strength were obtained from pressuremeter tests performed at six drilled holes at each station. The presence of weak ice in the area is discussed.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275436"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275436"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275436; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275436]").text(description); $(".js-view-count[data-work-id=117275436]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275436; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275436']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275436, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275436]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275436,"title":"Variations of ice properties in an ice area of 1x2 km in the Gulf of Bothnia March 1988","translated_title":"","metadata":{"abstract":"During the Bothnian Experiment in Preparation for ERS-1 (BEPERS-88), snow and ice thickness, salinity, density, crystal shape and ice strength were investigated. In a rectangular area of 1 x 2km, data from 12 stations is presented. The area covered level-ice, several pressure ridges and a belt of rafted and hummocked ice. The origin of the ice is discussed based on information given from vertical thin sections at different stations. Index values of ice strength were obtained from pressuremeter tests performed at six drilled holes at each station. The presence of weak ice in the area is discussed.","publication_date":{"day":null,"month":null,"year":1989,"errors":{}}},"translated_abstract":"During the Bothnian Experiment in Preparation for ERS-1 (BEPERS-88), snow and ice thickness, salinity, density, crystal shape and ice strength were investigated. In a rectangular area of 1 x 2km, data from 12 stations is presented. The area covered level-ice, several pressure ridges and a belt of rafted and hummocked ice. The origin of the ice is discussed based on information given from vertical thin sections at different stations. Index values of ice strength were obtained from pressuremeter tests performed at six drilled holes at each station. The presence of weak ice in the area is discussed.","internal_url":"https://www.academia.edu/117275436/Variations_of_ice_properties_in_an_ice_area_of_1x2_km_in_the_Gulf_of_Bothnia_March_1988","translated_internal_url":"","created_at":"2024-04-09T07:54:05.522-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Variations_of_ice_properties_in_an_ice_area_of_1x2_km_in_the_Gulf_of_Bothnia_March_1988","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"During the Bothnian Experiment in Preparation for ERS-1 (BEPERS-88), snow and ice thickness, salinity, density, crystal shape and ice strength were investigated. In a rectangular area of 1 x 2km, data from 12 stations is presented. The area covered level-ice, several pressure ridges and a belt of rafted and hummocked ice. The origin of the ice is discussed based on information given from vertical thin sections at different stations. Index values of ice strength were obtained from pressuremeter tests performed at six drilled holes at each station. The presence of weak ice in the area is discussed.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":29759,"name":"Sea Ice","url":"https://www.academia.edu/Documents/in/Sea_Ice"},{"id":197149,"name":"SNOW","url":"https://www.academia.edu/Documents/in/SNOW"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275435"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/117275435/Heat_Balance_Water_Temperature_and_Interpretations"><img alt="Research paper thumbnail of Heat Balance, Water Temperature, and Interpretations" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/117275435/Heat_Balance_Water_Temperature_and_Interpretations">Heat Balance, Water Temperature, and Interpretations</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The heat balance that determines the earth’s temperature represents an interesting and complex in...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The heat balance that determines the earth’s temperature represents an interesting and complex interplay between the sun, the earth, and our behaviour. The ocean plays many important roles in this, such as being the earth’s most important heat storage sink. Evaporation from the ocean surface due to latent heat flux works like a steam engine, driving large-scale atmospheric circulation. Long-wave radiation emitted from the earth’s surface is partly reflected back from the atmosphere by the GHGs that blanket the earth, protecting it from cooling. The human impact comes from anthropogenic landscape change and an increase in atmospheric GHG levels, for example, from fossil fuel burning, which influences the long-wave radiation reflected back to the surface. Today it is frighteningly clear that humans are influencing the ocean through global warming and ocean acidification. Will humans be able to reduce global warming or not? The ocean sends an image of a red jellyfish swimming slowly to...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275435"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275435"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275435; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275435]").text(description); $(".js-view-count[data-work-id=117275435]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275435; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275435']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275435, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275435]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275435,"title":"Heat Balance, Water Temperature, and Interpretations","translated_title":"","metadata":{"abstract":"The heat balance that determines the earth’s temperature represents an interesting and complex interplay between the sun, the earth, and our behaviour. The ocean plays many important roles in this, such as being the earth’s most important heat storage sink. Evaporation from the ocean surface due to latent heat flux works like a steam engine, driving large-scale atmospheric circulation. Long-wave radiation emitted from the earth’s surface is partly reflected back from the atmosphere by the GHGs that blanket the earth, protecting it from cooling. The human impact comes from anthropogenic landscape change and an increase in atmospheric GHG levels, for example, from fossil fuel burning, which influences the long-wave radiation reflected back to the surface. Today it is frighteningly clear that humans are influencing the ocean through global warming and ocean acidification. Will humans be able to reduce global warming or not? The ocean sends an image of a red jellyfish swimming slowly to...","publication_date":{"day":null,"month":null,"year":2020,"errors":{}}},"translated_abstract":"The heat balance that determines the earth’s temperature represents an interesting and complex interplay between the sun, the earth, and our behaviour. The ocean plays many important roles in this, such as being the earth’s most important heat storage sink. Evaporation from the ocean surface due to latent heat flux works like a steam engine, driving large-scale atmospheric circulation. Long-wave radiation emitted from the earth’s surface is partly reflected back from the atmosphere by the GHGs that blanket the earth, protecting it from cooling. The human impact comes from anthropogenic landscape change and an increase in atmospheric GHG levels, for example, from fossil fuel burning, which influences the long-wave radiation reflected back to the surface. Today it is frighteningly clear that humans are influencing the ocean through global warming and ocean acidification. Will humans be able to reduce global warming or not? The ocean sends an image of a red jellyfish swimming slowly to...","internal_url":"https://www.academia.edu/117275435/Heat_Balance_Water_Temperature_and_Interpretations","translated_internal_url":"","created_at":"2024-04-09T07:54:05.109-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Heat_Balance_Water_Temperature_and_Interpretations","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"The heat balance that determines the earth’s temperature represents an interesting and complex interplay between the sun, the earth, and our behaviour. The ocean plays many important roles in this, such as being the earth’s most important heat storage sink. Evaporation from the ocean surface due to latent heat flux works like a steam engine, driving large-scale atmospheric circulation. Long-wave radiation emitted from the earth’s surface is partly reflected back from the atmosphere by the GHGs that blanket the earth, protecting it from cooling. The human impact comes from anthropogenic landscape change and an increase in atmospheric GHG levels, for example, from fossil fuel burning, which influences the long-wave radiation reflected back to the surface. Today it is frighteningly clear that humans are influencing the ocean through global warming and ocean acidification. Will humans be able to reduce global warming or not? The ocean sends an image of a red jellyfish swimming slowly to...","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":681573,"name":"Heat Wave","url":"https://www.academia.edu/Documents/in/Heat_Wave"},{"id":2956968,"name":"Latent Heat","url":"https://www.academia.edu/Documents/in/Latent_Heat"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275434"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/117275434/Scenarios_the_Future_and_Simplicity"><img alt="Research paper thumbnail of Scenarios, the Future, and Simplicity" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/117275434/Scenarios_the_Future_and_Simplicity">Scenarios, the Future, and Simplicity</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Many are trying to foresee what will happen in the future. Numerical calculations of changes in s...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Many are trying to foresee what will happen in the future. Numerical calculations of changes in society often rely on statistical methods with no capacity to predict the future. Many try to relate various parameters to one another, hoping to gain knowledge of what is to come. Weather forecasting can provide information about conditions some days in advance. It is clear that emissions of carbon dioxide and other anthropogenic GHGs need to be reduced to prevent global warming. However, the global earth system models applied in climate change assessments rely on prescribed emission storylines and their projections are conditional on the assumed forcing. A major question for society is how to develop a greener and more sustainable future. The ocean responds by sending an image of barnacles adhering to a cliff, indicating that humans need to slow down, learn more from the ocean, and build durable and trusting relationships.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275434"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275434"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275434; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275434]").text(description); $(".js-view-count[data-work-id=117275434]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275434; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275434']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275434, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275434]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275434,"title":"Scenarios, the Future, and Simplicity","translated_title":"","metadata":{"abstract":"Many are trying to foresee what will happen in the future. Numerical calculations of changes in society often rely on statistical methods with no capacity to predict the future. Many try to relate various parameters to one another, hoping to gain knowledge of what is to come. Weather forecasting can provide information about conditions some days in advance. It is clear that emissions of carbon dioxide and other anthropogenic GHGs need to be reduced to prevent global warming. However, the global earth system models applied in climate change assessments rely on prescribed emission storylines and their projections are conditional on the assumed forcing. A major question for society is how to develop a greener and more sustainable future. The ocean responds by sending an image of barnacles adhering to a cliff, indicating that humans need to slow down, learn more from the ocean, and build durable and trusting relationships.","publication_date":{"day":null,"month":null,"year":2020,"errors":{}}},"translated_abstract":"Many are trying to foresee what will happen in the future. Numerical calculations of changes in society often rely on statistical methods with no capacity to predict the future. Many try to relate various parameters to one another, hoping to gain knowledge of what is to come. Weather forecasting can provide information about conditions some days in advance. It is clear that emissions of carbon dioxide and other anthropogenic GHGs need to be reduced to prevent global warming. However, the global earth system models applied in climate change assessments rely on prescribed emission storylines and their projections are conditional on the assumed forcing. A major question for society is how to develop a greener and more sustainable future. The ocean responds by sending an image of barnacles adhering to a cliff, indicating that humans need to slow down, learn more from the ocean, and build durable and trusting relationships.","internal_url":"https://www.academia.edu/117275434/Scenarios_the_Future_and_Simplicity","translated_internal_url":"","created_at":"2024-04-09T07:54:04.395-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Scenarios_the_Future_and_Simplicity","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Many are trying to foresee what will happen in the future. Numerical calculations of changes in society often rely on statistical methods with no capacity to predict the future. Many try to relate various parameters to one another, hoping to gain knowledge of what is to come. Weather forecasting can provide information about conditions some days in advance. It is clear that emissions of carbon dioxide and other anthropogenic GHGs need to be reduced to prevent global warming. However, the global earth system models applied in climate change assessments rely on prescribed emission storylines and their projections are conditional on the assumed forcing. A major question for society is how to develop a greener and more sustainable future. The ocean responds by sending an image of barnacles adhering to a cliff, indicating that humans need to slow down, learn more from the ocean, and build durable and trusting relationships.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[],"research_interests":[{"id":1512,"name":"Climate Change","url":"https://www.academia.edu/Documents/in/Climate_Change"},{"id":235683,"name":"Simplicity","url":"https://www.academia.edu/Documents/in/Simplicity"},{"id":251654,"name":"Greenhouse Gas","url":"https://www.academia.edu/Documents/in/Greenhouse_Gas"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275433"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/117275433/The_Development_of_Climate_Science_of_the_Baltic_Sea_Region"><img alt="Research paper thumbnail of The Development of Climate Science of the Baltic Sea Region" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/117275433/The_Development_of_Climate_Science_of_the_Baltic_Sea_Region">The Development of Climate Science of the Baltic Sea Region</a></div><div class="wp-workCard_item"><span>Oxford Research Encyclopedia of Climate Science</span><span>, 2017</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Dramatic climate changes have occurred in the Baltic Sea region caused by changes in orbital move...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Dramatic climate changes have occurred in the Baltic Sea region caused by changes in orbital movement in the earth–sun system and the melting of the Fennoscandian Ice Sheet. Added to these longer-term changes, changes have occurred at all timescales, caused mainly by variations in large-scale atmospheric pressure systems due to competition between the meandering midlatitude low-pressure systems and high-pressure systems. Here we follow the development of climate science of the Baltic Sea from when observations began in the 18th century to the early 21st century. The question of why the water level is sinking around the Baltic Sea coasts could not be answered until the ideas of postglacial uplift and the thermal history of the earth were better understood in the 19th century and periodic behavior in climate related time series attracted scientific interest. Herring and sardine fishing successes and failures have led to investigations of fishery and climate change and to the realizati...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275433"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275433"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275433; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275433]").text(description); $(".js-view-count[data-work-id=117275433]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275433; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275433']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275433, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275433]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275433,"title":"The Development of Climate Science of the Baltic Sea Region","translated_title":"","metadata":{"abstract":"Dramatic climate changes have occurred in the Baltic Sea region caused by changes in orbital movement in the earth–sun system and the melting of the Fennoscandian Ice Sheet. Added to these longer-term changes, changes have occurred at all timescales, caused mainly by variations in large-scale atmospheric pressure systems due to competition between the meandering midlatitude low-pressure systems and high-pressure systems. Here we follow the development of climate science of the Baltic Sea from when observations began in the 18th century to the early 21st century. The question of why the water level is sinking around the Baltic Sea coasts could not be answered until the ideas of postglacial uplift and the thermal history of the earth were better understood in the 19th century and periodic behavior in climate related time series attracted scientific interest. Herring and sardine fishing successes and failures have led to investigations of fishery and climate change and to the realizati...","publisher":"Oxford University Press","publication_date":{"day":null,"month":null,"year":2017,"errors":{}},"publication_name":"Oxford Research Encyclopedia of Climate Science"},"translated_abstract":"Dramatic climate changes have occurred in the Baltic Sea region caused by changes in orbital movement in the earth–sun system and the melting of the Fennoscandian Ice Sheet. Added to these longer-term changes, changes have occurred at all timescales, caused mainly by variations in large-scale atmospheric pressure systems due to competition between the meandering midlatitude low-pressure systems and high-pressure systems. Here we follow the development of climate science of the Baltic Sea from when observations began in the 18th century to the early 21st century. The question of why the water level is sinking around the Baltic Sea coasts could not be answered until the ideas of postglacial uplift and the thermal history of the earth were better understood in the 19th century and periodic behavior in climate related time series attracted scientific interest. Herring and sardine fishing successes and failures have led to investigations of fishery and climate change and to the realizati...","internal_url":"https://www.academia.edu/117275433/The_Development_of_Climate_Science_of_the_Baltic_Sea_Region","translated_internal_url":"","created_at":"2024-04-09T07:54:03.800-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"The_Development_of_Climate_Science_of_the_Baltic_Sea_Region","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Dramatic climate changes have occurred in the Baltic Sea region caused by changes in orbital movement in the earth–sun system and the melting of the Fennoscandian Ice Sheet. Added to these longer-term changes, changes have occurred at all timescales, caused mainly by variations in large-scale atmospheric pressure systems due to competition between the meandering midlatitude low-pressure systems and high-pressure systems. Here we follow the development of climate science of the Baltic Sea from when observations began in the 18th century to the early 21st century. The question of why the water level is sinking around the Baltic Sea coasts could not be answered until the ideas of postglacial uplift and the thermal history of the earth were better understood in the 19th century and periodic behavior in climate related time series attracted scientific interest. Herring and sardine fishing successes and failures have led to investigations of fishery and climate change and to the realizati...","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":1512,"name":"Climate Change","url":"https://www.academia.edu/Documents/in/Climate_Change"},{"id":45405,"name":"Global Warming","url":"https://www.academia.edu/Documents/in/Global_Warming"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="1424287" id="papers"><div class="js-work-strip profile--work_container" data-work-id="124218655"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/124218655/The_ocean_Excursion_and_return_The_ocean_Excursion_and_return"><img alt="Research paper thumbnail of The ocean: Excursion and return The ocean: Excursion and return" class="work-thumbnail" src="https://attachments.academia-assets.com/118486198/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/124218655/The_ocean_Excursion_and_return_The_ocean_Excursion_and_return">The ocean: Excursion and return The ocean: Excursion and return</a></div><div class="wp-workCard_item"><span>Filosofia,</span><span>, 2022</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The ocean with its coastal seas is under increasing anthropogenic pressure, severely threatening ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The ocean with its coastal seas is under increasing anthropogenic pressure, severely threatening ocean health and marine life. Human dependency on and management of the ocean are disconnected, which is in part why the United Nations (UN) is launching the Decade of Ocean Science for Sustainable Development, 2021-2030 ("Ocean Decade"). Here we investigate how philosophy and literature can inspire us to change the relationship between humans and the ocean. The starting point is natural science and human exploration of the sea. Then we consider philosophy, starting from Aristotle's forms of knowledge-episteme, techne, and phronesis-focusing particularly on phronesis, or practical wisdom. Referring to Homer's Odyssey, we investigate the threats that the ocean may face during the UN's Ocean Decade. From this, we identify several things that will make for a successful Ocean Decade: practical wise leadership, clear vision, societal involvement, information sharing, admitting the vulnerability of both the ocean and humans, and storytelling.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ac732a596bc430bdd4d58da23b308f46" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":118486198,"asset_id":124218655,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/118486198/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="124218655"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="124218655"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124218655; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124218655]").text(description); $(".js-view-count[data-work-id=124218655]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124218655; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124218655']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124218655, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "ac732a596bc430bdd4d58da23b308f46" } } $('.js-work-strip[data-work-id=124218655]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124218655,"title":"The ocean: Excursion and return The ocean: Excursion and return","translated_title":"","metadata":{"doi":"10.13135/2704-8195/7241","abstract":"The ocean with its coastal seas is under increasing anthropogenic pressure, severely threatening ocean health and marine life. Human dependency on and management of the ocean are disconnected, which is in part why the United Nations (UN) is launching the Decade of Ocean Science for Sustainable Development, 2021-2030 (\"Ocean Decade\"). Here we investigate how philosophy and literature can inspire us to change the relationship between humans and the ocean. The starting point is natural science and human exploration of the sea. Then we consider philosophy, starting from Aristotle's forms of knowledge-episteme, techne, and phronesis-focusing particularly on phronesis, or practical wisdom. Referring to Homer's Odyssey, we investigate the threats that the ocean may face during the UN's Ocean Decade. From this, we identify several things that will make for a successful Ocean Decade: practical wise leadership, clear vision, societal involvement, information sharing, admitting the vulnerability of both the ocean and humans, and storytelling.","publication_date":{"day":null,"month":null,"year":2022,"errors":{}},"publication_name":"Filosofia,"},"translated_abstract":"The ocean with its coastal seas is under increasing anthropogenic pressure, severely threatening ocean health and marine life. Human dependency on and management of the ocean are disconnected, which is in part why the United Nations (UN) is launching the Decade of Ocean Science for Sustainable Development, 2021-2030 (\"Ocean Decade\"). Here we investigate how philosophy and literature can inspire us to change the relationship between humans and the ocean. The starting point is natural science and human exploration of the sea. Then we consider philosophy, starting from Aristotle's forms of knowledge-episteme, techne, and phronesis-focusing particularly on phronesis, or practical wisdom. Referring to Homer's Odyssey, we investigate the threats that the ocean may face during the UN's Ocean Decade. From this, we identify several things that will make for a successful Ocean Decade: practical wise leadership, clear vision, societal involvement, information sharing, admitting the vulnerability of both the ocean and humans, and storytelling.","internal_url":"https://www.academia.edu/124218655/The_ocean_Excursion_and_return_The_ocean_Excursion_and_return","translated_internal_url":"","created_at":"2024-09-28T01:37:19.198-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":42455093,"work_id":124218655,"tagging_user_id":11956707,"tagged_user_id":295266502,"co_author_invite_id":null,"email":"a***t@gmail.com","display_order":1,"name":"Anders Omstedt","title":"The ocean: Excursion and return The ocean: Excursion and return"}],"downloadable_attachments":[{"id":118486198,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118486198/thumbnails/1.jpg","file_name":"Omstedt_and_Gustavsson_2022a.pdf","download_url":"https://www.academia.edu/attachments/118486198/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_ocean_Excursion_and_return_The_ocean.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118486198/Omstedt_and_Gustavsson_2022a-libre.pdf?1727513007=\u0026response-content-disposition=attachment%3B+filename%3DThe_ocean_Excursion_and_return_The_ocean.pdf\u0026Expires=1734108629\u0026Signature=MmyPLTi8DeMEWg6pJYMOeiAUmSPQS0VbokL5saZIHgzZuj0A~-lZ4R8S8QCxHHxnQf4qHlmXuTQRBNlXoiAtEnznDqpVDsM5unvUmoDUMA4YdAkP2dPmGEZ5zIlqrV3Nmm6RmjJMiqlCfXEr~uLHuZbswJ3h6Cat~ePt~uCbHhL4YAqm21Bb7f5JYQgUdwf4K6fe3coOcHgcn8~b-YHOFrALuR6lyzM~ZykNofZBYTEDNHVFt4KeV4x9j-NMxEs-NOaGC~oDMrBBhaviEfDXNw0ArXZjsyTj9X-yNJAkNY5NV5JxMQhmpga1yrXBzU1dz-GVcYydb7m3VXjcu5eSyA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_ocean_Excursion_and_return_The_ocean_Excursion_and_return","translated_slug":"","page_count":16,"language":"en","content_type":"Work","summary":"The ocean with its coastal seas is under increasing anthropogenic pressure, severely threatening ocean health and marine life. Human dependency on and management of the ocean are disconnected, which is in part why the United Nations (UN) is launching the Decade of Ocean Science for Sustainable Development, 2021-2030 (\"Ocean Decade\"). Here we investigate how philosophy and literature can inspire us to change the relationship between humans and the ocean. The starting point is natural science and human exploration of the sea. Then we consider philosophy, starting from Aristotle's forms of knowledge-episteme, techne, and phronesis-focusing particularly on phronesis, or practical wisdom. Referring to Homer's Odyssey, we investigate the threats that the ocean may face during the UN's Ocean Decade. From this, we identify several things that will make for a successful Ocean Decade: practical wise leadership, clear vision, societal involvement, information sharing, admitting the vulnerability of both the ocean and humans, and storytelling.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":118486198,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118486198/thumbnails/1.jpg","file_name":"Omstedt_and_Gustavsson_2022a.pdf","download_url":"https://www.academia.edu/attachments/118486198/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_ocean_Excursion_and_return_The_ocean.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118486198/Omstedt_and_Gustavsson_2022a-libre.pdf?1727513007=\u0026response-content-disposition=attachment%3B+filename%3DThe_ocean_Excursion_and_return_The_ocean.pdf\u0026Expires=1734108629\u0026Signature=MmyPLTi8DeMEWg6pJYMOeiAUmSPQS0VbokL5saZIHgzZuj0A~-lZ4R8S8QCxHHxnQf4qHlmXuTQRBNlXoiAtEnznDqpVDsM5unvUmoDUMA4YdAkP2dPmGEZ5zIlqrV3Nmm6RmjJMiqlCfXEr~uLHuZbswJ3h6Cat~ePt~uCbHhL4YAqm21Bb7f5JYQgUdwf4K6fe3coOcHgcn8~b-YHOFrALuR6lyzM~ZykNofZBYTEDNHVFt4KeV4x9j-NMxEs-NOaGC~oDMrBBhaviEfDXNw0ArXZjsyTj9X-yNJAkNY5NV5JxMQhmpga1yrXBzU1dz-GVcYydb7m3VXjcu5eSyA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":803,"name":"Philosophy","url":"https://www.academia.edu/Documents/in/Philosophy"},{"id":951,"name":"Humanities","url":"https://www.academia.edu/Documents/in/Humanities"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="124217854"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/124217854/A_Philosophic_View_of_the_Ocean_and_Humanity_Second_Edition"><img alt="Research paper thumbnail of A Philosophic View of the Ocean and Humanity. Second Edition" class="work-thumbnail" src="https://attachments.academia-assets.com/118485574/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/124217854/A_Philosophic_View_of_the_Ocean_and_Humanity_Second_Edition">A Philosophic View of the Ocean and Humanity. Second Edition</a></div><div class="wp-workCard_item"><span>Springer Nature</span><span>, 2024</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This new edition brings the reader into humans' challenges with the ocean and the future. It addr...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This new edition brings the reader into humans' challenges with the ocean and the future. It addresses the main questions in the United Nations Ocean Decade that aim to change how humans deal with the ocean. In the book's first part, art and dreaming are used as tools for connecting science and arts. This knowledge is applied in part II of the book, which is written in two modes: a concerned science mode and an intuitive, artistic mode in which the ocean is given a voice. Part II illustrates how science and art can be connected to increase our awareness of the state of the ocean and support behavioral change.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="f6e1789216b773f8e9d1f82f87c0288d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":118485574,"asset_id":124217854,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/118485574/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="124217854"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="124217854"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124217854; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124217854]").text(description); $(".js-view-count[data-work-id=124217854]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124217854; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124217854']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124217854, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "f6e1789216b773f8e9d1f82f87c0288d" } } $('.js-work-strip[data-work-id=124217854]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124217854,"title":"A Philosophic View of the Ocean and Humanity. Second Edition","translated_title":"","metadata":{"doi":"10.1007/978-3-031-64326-2","abstract":"This new edition brings the reader into humans' challenges with the ocean and the future. It addresses the main questions in the United Nations Ocean Decade that aim to change how humans deal with the ocean. In the book's first part, art and dreaming are used as tools for connecting science and arts. This knowledge is applied in part II of the book, which is written in two modes: a concerned science mode and an intuitive, artistic mode in which the ocean is given a voice. Part II illustrates how science and art can be connected to increase our awareness of the state of the ocean and support behavioral change.","publication_date":{"day":null,"month":null,"year":2024,"errors":{}},"publication_name":"Springer Nature"},"translated_abstract":"This new edition brings the reader into humans' challenges with the ocean and the future. It addresses the main questions in the United Nations Ocean Decade that aim to change how humans deal with the ocean. In the book's first part, art and dreaming are used as tools for connecting science and arts. This knowledge is applied in part II of the book, which is written in two modes: a concerned science mode and an intuitive, artistic mode in which the ocean is given a voice. Part II illustrates how science and art can be connected to increase our awareness of the state of the ocean and support behavioral change.","internal_url":"https://www.academia.edu/124217854/A_Philosophic_View_of_the_Ocean_and_Humanity_Second_Edition","translated_internal_url":"","created_at":"2024-09-28T00:57:25.118-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":118485574,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118485574/thumbnails/1.jpg","file_name":"New_book_Omstedt_2024.pdf","download_url":"https://www.academia.edu/attachments/118485574/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"A_Philosophic_View_of_the_Ocean_and_Huma.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118485574/New_book_Omstedt_2024-libre.pdf?1727512357=\u0026response-content-disposition=attachment%3B+filename%3DA_Philosophic_View_of_the_Ocean_and_Huma.pdf\u0026Expires=1734108629\u0026Signature=FUJ34K51LyoXy2JAf7HdWbeYCv~KcJn4THTeCa0ejw~4ZtSaBIzoS8gaxfxNHulHkMECsa8oIBKliDnIlwRJigKzbCailcFVMdL9uH6kXAdLQSs6Ve3-OKJR1fHFO-Mtvv2GVknZHhAJg6YouUQIT~cvF0VKradpwcIsNpKTtSdVed1JTvBkHM4VyjvsXr6KHc3j2XqH1bx2LvS8ok76pJqfjg0pd1Gmuqcbty0WUf-NxkJSYRJyr5aSipFcTEFS3XqNIyVY6wX2j4aumj4zpFHNqMVttFeQ7D~pq3B6MoAJ0zsge07I578LFCtQJUuYciZcgfPT7uogEDuzJ0EbdQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"A_Philosophic_View_of_the_Ocean_and_Humanity_Second_Edition","translated_slug":"","page_count":1,"language":"en","content_type":"Work","summary":"This new edition brings the reader into humans' challenges with the ocean and the future. It addresses the main questions in the United Nations Ocean Decade that aim to change how humans deal with the ocean. In the book's first part, art and dreaming are used as tools for connecting science and arts. This knowledge is applied in part II of the book, which is written in two modes: a concerned science mode and an intuitive, artistic mode in which the ocean is given a voice. Part II illustrates how science and art can be connected to increase our awareness of the state of the ocean and support behavioral change.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":118485574,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118485574/thumbnails/1.jpg","file_name":"New_book_Omstedt_2024.pdf","download_url":"https://www.academia.edu/attachments/118485574/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"A_Philosophic_View_of_the_Ocean_and_Huma.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118485574/New_book_Omstedt_2024-libre.pdf?1727512357=\u0026response-content-disposition=attachment%3B+filename%3DA_Philosophic_View_of_the_Ocean_and_Huma.pdf\u0026Expires=1734108629\u0026Signature=FUJ34K51LyoXy2JAf7HdWbeYCv~KcJn4THTeCa0ejw~4ZtSaBIzoS8gaxfxNHulHkMECsa8oIBKliDnIlwRJigKzbCailcFVMdL9uH6kXAdLQSs6Ve3-OKJR1fHFO-Mtvv2GVknZHhAJg6YouUQIT~cvF0VKradpwcIsNpKTtSdVed1JTvBkHM4VyjvsXr6KHc3j2XqH1bx2LvS8ok76pJqfjg0pd1Gmuqcbty0WUf-NxkJSYRJyr5aSipFcTEFS3XqNIyVY6wX2j4aumj4zpFHNqMVttFeQ7D~pq3B6MoAJ0zsge07I578LFCtQJUuYciZcgfPT7uogEDuzJ0EbdQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":3368098,"name":"UN Decade of Ocean Science for Sustainable Development 2021–2030","url":"https://www.academia.edu/Documents/in/UN_Decade_of_Ocean_Science_for_Sustainable_Development_2021_2030"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="124163370"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/124163370/Modeling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper"><img alt="Research paper thumbnail of Modeling the seasonal, interannual, and long-term variations of salinity and temperature in the Baltic proper" class="work-thumbnail" src="https://attachments.academia-assets.com/118437140/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/124163370/Modeling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper">Modeling the seasonal, interannual, and long-term variations of salinity and temperature in the Baltic proper</a></div><div class="wp-workCard_item"><span>Tellus A</span><span>, 1998</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with a numerical ocean model and a large amount of observational data. In the model, the Baltic Sea is divided into 13 sub-basins with high vertical resolution, horizontally coupled by barotropic and baroclinic flows and vertically coupled to a sea-ice model which includes dynamics as well as thermodynamics. The model was integrated for a 15-year period (1980-1995) by using observed meteorological forcing data, river-runoff data and sea-level data from the Kattegat. The calculated 15-year median profiles of salinity and temperature in the different sub-basins are in good agreement with observations. However, the calculated middepth salinities in the Arkona Basin and Bornholm Basin were somewhat overestimated, and the calculated deep-water temperatures in the Arkona Basin and the Bornholm Basin are somewhat lower than the observed values. Frontal mixing and movements in the Kattegat and the entrance area of the Arkona Basin were important to consider in the model. Water masses were simulated well, and prescribing constant deep-water properties in the Kattegat proved to be a reasonable lateral boundary condition. Further, comparisons were made between observed and calculated seasonal and interannual variations of the hydrographic properties in the Eastern Gotland Basin, as well as the interannual variations of the annual maximum ice extent. We conclude that the model can simulate these variations realistically. The major Baltic inflow of 1993 was also simulated by the model, but the inflowing water was 1-2°degrees too cold. Finally, the response times to changes in forcing of the Baltic proper and the Kattegat were investigated by performing the so-called lock-exchange experiment. Typical stratification spin-up times were of the order of 10 years for the Kattegat, and 100 years for the Baltic proper.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2ba3147406fab23bad91762e222a98e3" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":118437140,"asset_id":124163370,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/118437140/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="124163370"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="124163370"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124163370; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124163370]").text(description); $(".js-view-count[data-work-id=124163370]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124163370; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124163370']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124163370, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "2ba3147406fab23bad91762e222a98e3" } } $('.js-work-strip[data-work-id=124163370]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124163370,"title":"Modeling the seasonal, interannual, and long-term variations of salinity and temperature in the Baltic proper","translated_title":"","metadata":{"publisher":"Wiley-Blackwell","grobid_abstract":"Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with a numerical ocean model and a large amount of observational data. In the model, the Baltic Sea is divided into 13 sub-basins with high vertical resolution, horizontally coupled by barotropic and baroclinic flows and vertically coupled to a sea-ice model which includes dynamics as well as thermodynamics. The model was integrated for a 15-year period (1980-1995) by using observed meteorological forcing data, river-runoff data and sea-level data from the Kattegat. The calculated 15-year median profiles of salinity and temperature in the different sub-basins are in good agreement with observations. However, the calculated middepth salinities in the Arkona Basin and Bornholm Basin were somewhat overestimated, and the calculated deep-water temperatures in the Arkona Basin and the Bornholm Basin are somewhat lower than the observed values. Frontal mixing and movements in the Kattegat and the entrance area of the Arkona Basin were important to consider in the model. Water masses were simulated well, and prescribing constant deep-water properties in the Kattegat proved to be a reasonable lateral boundary condition. Further, comparisons were made between observed and calculated seasonal and interannual variations of the hydrographic properties in the Eastern Gotland Basin, as well as the interannual variations of the annual maximum ice extent. We conclude that the model can simulate these variations realistically. The major Baltic inflow of 1993 was also simulated by the model, but the inflowing water was 1-2°degrees too cold. Finally, the response times to changes in forcing of the Baltic proper and the Kattegat were investigated by performing the so-called lock-exchange experiment. Typical stratification spin-up times were of the order of 10 years for the Kattegat, and 100 years for the Baltic proper.","publication_date":{"day":null,"month":null,"year":1998,"errors":{}},"publication_name":"Tellus A","grobid_abstract_attachment_id":118437140},"translated_abstract":null,"internal_url":"https://www.academia.edu/124163370/Modeling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper","translated_internal_url":"","created_at":"2024-09-25T12:18:23.987-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":118437140,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118437140/thumbnails/1.jpg","file_name":"tellusa.v50i5.pdf","download_url":"https://www.academia.edu/attachments/118437140/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modeling_the_seasonal_interannual_and_lo.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118437140/tellusa.v50i5-libre.pdf?1727293002=\u0026response-content-disposition=attachment%3B+filename%3DModeling_the_seasonal_interannual_and_lo.pdf\u0026Expires=1734108629\u0026Signature=SpM1ljj~GH7Wi45QfnfWKsr9Aa9Y~-RFMPUAfKEbAQERywUhFXgB2pte4Cv3ytWr3zcRw1sanSlnzQqbPFBmXHvLz7ar1TinMAQokKB9Q1IyU4FducEr9mD9gd4Uw8sk~ybjZAQzOKwltaWx3fLuqSUosKHYXlnanTeOkjRlwcsz6Xl~H69x7dUnNSuSfThpec-ISzxnqDzDAImL1tT-EpyONhWMd2p5A5xm4xgI0Lgz1hUAwSEFhNrAOUMwiN05JEM~Y3hPRa69UtMu7tVDrLZCaICVvbU8ZXCW7p6VAYxqjnz1umnO~-KXUdC998ef8DIEPSJnZpOVMziWXOsQkw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Modeling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper","translated_slug":"","page_count":17,"language":"en","content_type":"Work","summary":"Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with a numerical ocean model and a large amount of observational data. In the model, the Baltic Sea is divided into 13 sub-basins with high vertical resolution, horizontally coupled by barotropic and baroclinic flows and vertically coupled to a sea-ice model which includes dynamics as well as thermodynamics. The model was integrated for a 15-year period (1980-1995) by using observed meteorological forcing data, river-runoff data and sea-level data from the Kattegat. The calculated 15-year median profiles of salinity and temperature in the different sub-basins are in good agreement with observations. However, the calculated middepth salinities in the Arkona Basin and Bornholm Basin were somewhat overestimated, and the calculated deep-water temperatures in the Arkona Basin and the Bornholm Basin are somewhat lower than the observed values. Frontal mixing and movements in the Kattegat and the entrance area of the Arkona Basin were important to consider in the model. Water masses were simulated well, and prescribing constant deep-water properties in the Kattegat proved to be a reasonable lateral boundary condition. Further, comparisons were made between observed and calculated seasonal and interannual variations of the hydrographic properties in the Eastern Gotland Basin, as well as the interannual variations of the annual maximum ice extent. We conclude that the model can simulate these variations realistically. The major Baltic inflow of 1993 was also simulated by the model, but the inflowing water was 1-2°degrees too cold. Finally, the response times to changes in forcing of the Baltic proper and the Kattegat were investigated by performing the so-called lock-exchange experiment. Typical stratification spin-up times were of the order of 10 years for the Kattegat, and 100 years for the Baltic proper.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":118437140,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118437140/thumbnails/1.jpg","file_name":"tellusa.v50i5.pdf","download_url":"https://www.academia.edu/attachments/118437140/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modeling_the_seasonal_interannual_and_lo.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118437140/tellusa.v50i5-libre.pdf?1727293002=\u0026response-content-disposition=attachment%3B+filename%3DModeling_the_seasonal_interannual_and_lo.pdf\u0026Expires=1734108629\u0026Signature=SpM1ljj~GH7Wi45QfnfWKsr9Aa9Y~-RFMPUAfKEbAQERywUhFXgB2pte4Cv3ytWr3zcRw1sanSlnzQqbPFBmXHvLz7ar1TinMAQokKB9Q1IyU4FducEr9mD9gd4Uw8sk~ybjZAQzOKwltaWx3fLuqSUosKHYXlnanTeOkjRlwcsz6Xl~H69x7dUnNSuSfThpec-ISzxnqDzDAImL1tT-EpyONhWMd2p5A5xm4xgI0Lgz1hUAwSEFhNrAOUMwiN05JEM~Y3hPRa69UtMu7tVDrLZCaICVvbU8ZXCW7p6VAYxqjnz1umnO~-KXUdC998ef8DIEPSJnZpOVMziWXOsQkw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":3754,"name":"Climatology","url":"https://www.academia.edu/Documents/in/Climatology"},{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences"},{"id":82107,"name":"Salinity","url":"https://www.academia.edu/Documents/in/Salinity"},{"id":410933,"name":"Baltic Sea","url":"https://www.academia.edu/Documents/in/Baltic_Sea"},{"id":597110,"name":"Tellus","url":"https://www.academia.edu/Documents/in/Tellus"}],"urls":[{"id":44824946,"url":"https://doi.org/10.3402/tellusa.v50i5.14563"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="124163369"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/124163369/Modelling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper"><img alt="Research paper thumbnail of Modelling the seasonal, interannual, and long-term variations of salinity and temperature in the Baltic proper" class="work-thumbnail" src="https://attachments.academia-assets.com/118437131/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/124163369/Modelling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper">Modelling the seasonal, interannual, and long-term variations of salinity and temperature in the Baltic proper</a></div><div class="wp-workCard_item"><span>Tellus A</span><span>, Oct 1, 1998</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with a numerical ocean model and a large amount of observational data. In the model, the Baltic Sea is divided into 13 sub-basins with high vertical resolution, horizontally coupled by barotropic and baroclinic flows and vertically coupled to a sea-ice model which includes dynamics as well as thermodynamics. The model was integrated for a 15-year period (1980-1995) by using observed meteorological forcing data, river-runoff data and sea-level data from the Kattegat. The calculated 15-year median profiles of salinity and temperature in the different sub-basins are in good agreement with observations. However, the calculated middepth salinities in the Arkona Basin and Bornholm Basin were somewhat overestimated, and the calculated deep-water temperatures in the Arkona Basin and the Bornholm Basin are somewhat lower than the observed values. Frontal mixing and movements in the Kattegat and the entrance area of the Arkona Basin were important to consider in the model. Water masses were simulated well, and prescribing constant deep-water properties in the Kattegat proved to be a reasonable lateral boundary condition. Further, comparisons were made between observed and calculated seasonal and interannual variations of the hydrographic properties in the Eastern Gotland Basin, as well as the interannual variations of the annual maximum ice extent. We conclude that the model can simulate these variations realistically. The major Baltic inflow of 1993 was also simulated by the model, but the inflowing water was 1-2°degrees too cold. Finally, the response times to changes in forcing of the Baltic proper and the Kattegat were investigated by performing the so-called lock-exchange experiment. Typical stratification spin-up times were of the order of 10 years for the Kattegat, and 100 years for the Baltic proper.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d637ae3d1f6ea7b38bff16a3014d3a1d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":118437131,"asset_id":124163369,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/118437131/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="124163369"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="124163369"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124163369; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124163369]").text(description); $(".js-view-count[data-work-id=124163369]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124163369; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124163369']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124163369, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "d637ae3d1f6ea7b38bff16a3014d3a1d" } } $('.js-work-strip[data-work-id=124163369]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124163369,"title":"Modelling the seasonal, interannual, and long-term variations of salinity and temperature in the Baltic proper","translated_title":"","metadata":{"publisher":"Wiley-Blackwell","ai_title_tag":"Modeling Salinity and Temperature Variations in the Baltic Sea","grobid_abstract":"Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with a numerical ocean model and a large amount of observational data. In the model, the Baltic Sea is divided into 13 sub-basins with high vertical resolution, horizontally coupled by barotropic and baroclinic flows and vertically coupled to a sea-ice model which includes dynamics as well as thermodynamics. The model was integrated for a 15-year period (1980-1995) by using observed meteorological forcing data, river-runoff data and sea-level data from the Kattegat. The calculated 15-year median profiles of salinity and temperature in the different sub-basins are in good agreement with observations. However, the calculated middepth salinities in the Arkona Basin and Bornholm Basin were somewhat overestimated, and the calculated deep-water temperatures in the Arkona Basin and the Bornholm Basin are somewhat lower than the observed values. Frontal mixing and movements in the Kattegat and the entrance area of the Arkona Basin were important to consider in the model. Water masses were simulated well, and prescribing constant deep-water properties in the Kattegat proved to be a reasonable lateral boundary condition. Further, comparisons were made between observed and calculated seasonal and interannual variations of the hydrographic properties in the Eastern Gotland Basin, as well as the interannual variations of the annual maximum ice extent. We conclude that the model can simulate these variations realistically. The major Baltic inflow of 1993 was also simulated by the model, but the inflowing water was 1-2°degrees too cold. Finally, the response times to changes in forcing of the Baltic proper and the Kattegat were investigated by performing the so-called lock-exchange experiment. Typical stratification spin-up times were of the order of 10 years for the Kattegat, and 100 years for the Baltic proper.","publication_date":{"day":1,"month":10,"year":1998,"errors":{}},"publication_name":"Tellus A","grobid_abstract_attachment_id":118437131},"translated_abstract":null,"internal_url":"https://www.academia.edu/124163369/Modelling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper","translated_internal_url":"","created_at":"2024-09-25T12:18:23.298-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":118437131,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118437131/thumbnails/1.jpg","file_name":"FULLTEXT01.pdf","download_url":"https://www.academia.edu/attachments/118437131/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modelling_the_seasonal_interannual_and_l.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118437131/FULLTEXT01-libre.pdf?1727292998=\u0026response-content-disposition=attachment%3B+filename%3DModelling_the_seasonal_interannual_and_l.pdf\u0026Expires=1734108629\u0026Signature=N2KqejAq3cG-esDgv3psiHiv4YulWJuHsgpk6A4UX9gljeQieBI83OCvy447T8-IY7d-qgWdD5hrXIB4xjRJRvHYz79c9jbcVMZ5ym45bRvEbHWQv2T1KbVhC6KTpRLv0MTYcUWnngI~dDYL~9Lok9c55jSL-C3MB9cMpAtKCAgzhLZeGCRL8l9rMhKltkRCd4Q59x-9rxUxN~zI8J7HxZwHTN1gQBplZzp~-UHekP4-5gfkXFOyBZG45wX~YQQ5G2xMR56xgdO6I26DhG5TEeFVWHzveKTLU1tm2UwPgyWTqPJ3~B0w5-lTbbyiwMAdul3MIOIfgJnS~wM6iVC93A__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Modelling_the_seasonal_interannual_and_long_term_variations_of_salinity_and_temperature_in_the_Baltic_proper","translated_slug":"","page_count":16,"language":"en","content_type":"Work","summary":"Salinity and temperature variations in the Baltic proper and the Kattegat have been analyzed with a numerical ocean model and a large amount of observational data. In the model, the Baltic Sea is divided into 13 sub-basins with high vertical resolution, horizontally coupled by barotropic and baroclinic flows and vertically coupled to a sea-ice model which includes dynamics as well as thermodynamics. The model was integrated for a 15-year period (1980-1995) by using observed meteorological forcing data, river-runoff data and sea-level data from the Kattegat. The calculated 15-year median profiles of salinity and temperature in the different sub-basins are in good agreement with observations. However, the calculated middepth salinities in the Arkona Basin and Bornholm Basin were somewhat overestimated, and the calculated deep-water temperatures in the Arkona Basin and the Bornholm Basin are somewhat lower than the observed values. Frontal mixing and movements in the Kattegat and the entrance area of the Arkona Basin were important to consider in the model. Water masses were simulated well, and prescribing constant deep-water properties in the Kattegat proved to be a reasonable lateral boundary condition. Further, comparisons were made between observed and calculated seasonal and interannual variations of the hydrographic properties in the Eastern Gotland Basin, as well as the interannual variations of the annual maximum ice extent. We conclude that the model can simulate these variations realistically. The major Baltic inflow of 1993 was also simulated by the model, but the inflowing water was 1-2°degrees too cold. Finally, the response times to changes in forcing of the Baltic proper and the Kattegat were investigated by performing the so-called lock-exchange experiment. Typical stratification spin-up times were of the order of 10 years for the Kattegat, and 100 years for the Baltic proper.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":118437131,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118437131/thumbnails/1.jpg","file_name":"FULLTEXT01.pdf","download_url":"https://www.academia.edu/attachments/118437131/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modelling_the_seasonal_interannual_and_l.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118437131/FULLTEXT01-libre.pdf?1727292998=\u0026response-content-disposition=attachment%3B+filename%3DModelling_the_seasonal_interannual_and_l.pdf\u0026Expires=1734108629\u0026Signature=N2KqejAq3cG-esDgv3psiHiv4YulWJuHsgpk6A4UX9gljeQieBI83OCvy447T8-IY7d-qgWdD5hrXIB4xjRJRvHYz79c9jbcVMZ5ym45bRvEbHWQv2T1KbVhC6KTpRLv0MTYcUWnngI~dDYL~9Lok9c55jSL-C3MB9cMpAtKCAgzhLZeGCRL8l9rMhKltkRCd4Q59x-9rxUxN~zI8J7HxZwHTN1gQBplZzp~-UHekP4-5gfkXFOyBZG45wX~YQQ5G2xMR56xgdO6I26DhG5TEeFVWHzveKTLU1tm2UwPgyWTqPJ3~B0w5-lTbbyiwMAdul3MIOIfgJnS~wM6iVC93A__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":3754,"name":"Climatology","url":"https://www.academia.edu/Documents/in/Climatology"},{"id":57433,"name":"Seasonality","url":"https://www.academia.edu/Documents/in/Seasonality"},{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences"},{"id":82107,"name":"Salinity","url":"https://www.academia.edu/Documents/in/Salinity"},{"id":597110,"name":"Tellus","url":"https://www.academia.edu/Documents/in/Tellus"}],"urls":[{"id":44824945,"url":"http://smhi.diva-portal.org/smash/get/diva2:850981/FULLTEXT01"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="124163342"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/124163342/H%C3%A5llbara_kustsamh%C3%A4llen_i_l%C3%A5ngtidsperspektiv_G%C3%B6teborg_3_4_maj_och_1_2_november_2010"><img alt="Research paper thumbnail of Hållbara kustsamhällen i långtidsperspektiv, Göteborg 3–4 maj och 1–2 november 2010" class="work-thumbnail" src="https://attachments.academia-assets.com/118437110/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/124163342/H%C3%A5llbara_kustsamh%C3%A4llen_i_l%C3%A5ngtidsperspektiv_G%C3%B6teborg_3_4_maj_och_1_2_november_2010">Hållbara kustsamhällen i långtidsperspektiv, Göteborg 3–4 maj och 1–2 november 2010</a></div><div class="wp-workCard_item"><span>Historisk Tidsskrift</span><span>, Jun 7, 2011</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="9c2538ddea1f114606fd7a8647978587" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":118437110,"asset_id":124163342,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/118437110/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="124163342"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="124163342"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124163342; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124163342]").text(description); $(".js-view-count[data-work-id=124163342]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124163342; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124163342']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124163342, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "9c2538ddea1f114606fd7a8647978587" } } $('.js-work-strip[data-work-id=124163342]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124163342,"title":"Hållbara kustsamhällen i långtidsperspektiv, Göteborg 3–4 maj och 1–2 november 2010","translated_title":"","metadata":{"publisher":"Scandinavian University Press/Universitetsforlaget","publication_date":{"day":7,"month":6,"year":2011,"errors":{}},"publication_name":"Historisk Tidsskrift"},"translated_abstract":null,"internal_url":"https://www.academia.edu/124163342/H%C3%A5llbara_kustsamh%C3%A4llen_i_l%C3%A5ngtidsperspektiv_G%C3%B6teborg_3_4_maj_och_1_2_november_2010","translated_internal_url":"","created_at":"2024-09-25T12:16:46.893-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":118437110,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118437110/thumbnails/1.jpg","file_name":"HT_2011_2_417-418_hansson_omstedt.pdf","download_url":"https://www.academia.edu/attachments/118437110/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Hallbara_kustsamhallen_i_langtidsperspek.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118437110/HT_2011_2_417-418_hansson_omstedt-libre.pdf?1727293007=\u0026response-content-disposition=attachment%3B+filename%3DHallbara_kustsamhallen_i_langtidsperspek.pdf\u0026Expires=1734108629\u0026Signature=V7d6T0BV67iZKzFnrttP1Ki9Ajosd8MeRQ24jSrqGCKLr0G12Y9supiZXyPtLzdCQcBkyRDo-3blb3Ww3mcelL7u5sgodbUfBKtwVX-pLw3qns8GH5ouD9W3N7jISz7BgXDHPwq7g01ulU3TdI-oogqHMG~m4CxkeKqu6pTVr0UqwPUG8nlfg3-FTbqGKsJ3AvVwa5IbDdf~GiQiK05fpbDegg5JbFY-MQCx8y1J6z6YoayB5fu4FKrFg6HZsg0QENAw2NNl6Ay1nzyHyvFbyAtQjDow-y4VMTnimPONT9VPygW04BlG~7dVgSrvuoz8WORi5RDG74-Pd~Sz1u2UxQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Hållbara_kustsamhällen_i_långtidsperspektiv_Göteborg_3_4_maj_och_1_2_november_2010","translated_slug":"","page_count":3,"language":"sv","content_type":"Work","summary":null,"owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":118437110,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118437110/thumbnails/1.jpg","file_name":"HT_2011_2_417-418_hansson_omstedt.pdf","download_url":"https://www.academia.edu/attachments/118437110/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Hallbara_kustsamhallen_i_langtidsperspek.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118437110/HT_2011_2_417-418_hansson_omstedt-libre.pdf?1727293007=\u0026response-content-disposition=attachment%3B+filename%3DHallbara_kustsamhallen_i_langtidsperspek.pdf\u0026Expires=1734108629\u0026Signature=V7d6T0BV67iZKzFnrttP1Ki9Ajosd8MeRQ24jSrqGCKLr0G12Y9supiZXyPtLzdCQcBkyRDo-3blb3Ww3mcelL7u5sgodbUfBKtwVX-pLw3qns8GH5ouD9W3N7jISz7BgXDHPwq7g01ulU3TdI-oogqHMG~m4CxkeKqu6pTVr0UqwPUG8nlfg3-FTbqGKsJ3AvVwa5IbDdf~GiQiK05fpbDegg5JbFY-MQCx8y1J6z6YoayB5fu4FKrFg6HZsg0QENAw2NNl6Ay1nzyHyvFbyAtQjDow-y4VMTnimPONT9VPygW04BlG~7dVgSrvuoz8WORi5RDG74-Pd~Sz1u2UxQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"},{"id":118437111,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/118437111/thumbnails/1.jpg","file_name":"HT_2011_2_417-418_hansson_omstedt.pdf","download_url":"https://www.academia.edu/attachments/118437111/download_file","bulk_download_file_name":"Hallbara_kustsamhallen_i_langtidsperspek.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/118437111/HT_2011_2_417-418_hansson_omstedt-libre.pdf?1727293007=\u0026response-content-disposition=attachment%3B+filename%3DHallbara_kustsamhallen_i_langtidsperspek.pdf\u0026Expires=1734108629\u0026Signature=Lj0WCHSXHtyi~oo6dSQmUDaz9qGvQvyyIuAjGjO756aGylvLdXquQ~nMTd8-ZcitU2S3dUKdc2HYfih4VBJktQbCQCtq7Y0abrEzjS9dyCM0blKSWhhW2g1NUNRgvlzXA1PFILfyo0wTtD~LK2wcgqfbm8PlSPwJuA4X74mxhnvRPWaxQqilQm7eyRPVl4lSUIZe7nKvcxOGJgmkXyTyTNXlkoP8kXn5lAyMvHUncInXmsLKCR3VOyXckbH1~Rnq7xqBUsAoQ-TNltc0x40X17g30D0NN8in2u9EWSRpgKp6liw71UyKljsVMHUI25zwXAPFYllJH1~WUaIVforWqw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[],"urls":[{"id":44824927,"url":"http://www.historisktidskrift.se/fulltext/2011-2/pdf/HT_2011_2_417-418_hansson_omstedt.pdf"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="121518601"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/121518601/Deep_water_properties_in_the_Gulf_of_Bothnia"><img alt="Research paper thumbnail of Deep water properties in the Gulf of Bothnia" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/121518601/Deep_water_properties_in_the_Gulf_of_Bothnia">Deep water properties in the Gulf of Bothnia</a></div><div class="wp-workCard_item"><span>Continental Shelf Research</span><span>, Feb 1, 1993</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">ABSTRACT The northern extension of the Baltic Sea, the Gulf of Bothnia, is a weakly stratified se...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">ABSTRACT The northern extension of the Baltic Sea, the Gulf of Bothnia, is a weakly stratified sea. One would therefore expect that the deep water of the Gulf is easily renewed through deep thermal convection, or even through deep haline convection, as the Gulf is more or less covered with ice every winter. However, the present study shows, through analysis of historical temperature, salinity and density data, that the deep water in the Gulf of Bothnia is mainly renewed by major inflows of Baltic Proper surface water. The penetrating water forms a dense bottom current in the Gulf. In the southern part of the Gulf, the Bothnian Sea, the volume flow of the bottom current is found to increase by 10%. It is therefore not likely that the bottom current properties are changed to any appreciable extent. The bottom current properties in the Bothnian Bay, on the other hand, are highly affected, as the volume flow is estimated to increase by 150% in this basin.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="121518601"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="121518601"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 121518601; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=121518601]").text(description); $(".js-view-count[data-work-id=121518601]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 121518601; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='121518601']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 121518601, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=121518601]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":121518601,"title":"Deep water properties in the Gulf of Bothnia","translated_title":"","metadata":{"abstract":"ABSTRACT The northern extension of the Baltic Sea, the Gulf of Bothnia, is a weakly stratified sea. One would therefore expect that the deep water of the Gulf is easily renewed through deep thermal convection, or even through deep haline convection, as the Gulf is more or less covered with ice every winter. However, the present study shows, through analysis of historical temperature, salinity and density data, that the deep water in the Gulf of Bothnia is mainly renewed by major inflows of Baltic Proper surface water. The penetrating water forms a dense bottom current in the Gulf. In the southern part of the Gulf, the Bothnian Sea, the volume flow of the bottom current is found to increase by 10%. It is therefore not likely that the bottom current properties are changed to any appreciable extent. The bottom current properties in the Bothnian Bay, on the other hand, are highly affected, as the volume flow is estimated to increase by 150% in this basin.","publisher":"Elsevier BV","publication_date":{"day":1,"month":2,"year":1993,"errors":{}},"publication_name":"Continental Shelf Research"},"translated_abstract":"ABSTRACT The northern extension of the Baltic Sea, the Gulf of Bothnia, is a weakly stratified sea. One would therefore expect that the deep water of the Gulf is easily renewed through deep thermal convection, or even through deep haline convection, as the Gulf is more or less covered with ice every winter. However, the present study shows, through analysis of historical temperature, salinity and density data, that the deep water in the Gulf of Bothnia is mainly renewed by major inflows of Baltic Proper surface water. The penetrating water forms a dense bottom current in the Gulf. In the southern part of the Gulf, the Bothnian Sea, the volume flow of the bottom current is found to increase by 10%. It is therefore not likely that the bottom current properties are changed to any appreciable extent. The bottom current properties in the Bothnian Bay, on the other hand, are highly affected, as the volume flow is estimated to increase by 150% in this basin.","internal_url":"https://www.academia.edu/121518601/Deep_water_properties_in_the_Gulf_of_Bothnia","translated_internal_url":"","created_at":"2024-06-26T00:10:51.257-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Deep_water_properties_in_the_Gulf_of_Bothnia","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"ABSTRACT The northern extension of the Baltic Sea, the Gulf of Bothnia, is a weakly stratified sea. One would therefore expect that the deep water of the Gulf is easily renewed through deep thermal convection, or even through deep haline convection, as the Gulf is more or less covered with ice every winter. However, the present study shows, through analysis of historical temperature, salinity and density data, that the deep water in the Gulf of Bothnia is mainly renewed by major inflows of Baltic Proper surface water. The penetrating water forms a dense bottom current in the Gulf. In the southern part of the Gulf, the Bothnian Sea, the volume flow of the bottom current is found to increase by 10%. It is therefore not likely that the bottom current properties are changed to any appreciable extent. The bottom current properties in the Bothnian Bay, on the other hand, are highly affected, as the volume flow is estimated to increase by 150% in this basin.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":82107,"name":"Salinity","url":"https://www.academia.edu/Documents/in/Salinity"},{"id":230435,"name":"Continental shelf","url":"https://www.academia.edu/Documents/in/Continental_shelf"},{"id":322541,"name":"Deep water","url":"https://www.academia.edu/Documents/in/Deep_water"},{"id":1660649,"name":"Bay","url":"https://www.academia.edu/Documents/in/Bay"}],"urls":[{"id":43238854,"url":"https://doi.org/10.1016/0278-4343(93)90104-6"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275453"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/117275453/Modeling_the_variations_of_salinity_and_temperature_in_the_large_Gulfs_of_the_Baltic_Sea"><img alt="Research paper thumbnail of Modeling the variations of salinity and temperature in the large Gulfs of the Baltic Sea" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/117275453/Modeling_the_variations_of_salinity_and_temperature_in_the_large_Gulfs_of_the_Baltic_Sea">Modeling the variations of salinity and temperature in the large Gulfs of the Baltic Sea</a></div><div class="wp-workCard_item"><span>Continental Shelf Research</span><span>, Feb 1, 2003</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">ABSTRACT The modeling of salinity and temperature in Gulf of Bothnia, Gulf of Finland, and Gulf o...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">ABSTRACT The modeling of salinity and temperature in Gulf of Bothnia, Gulf of Finland, and Gulf of Riga is investigated by using a coupled sea ice-ocean Baltic Sea model. 18 years, from late 1980 to the end of 1998, have been investigated. The forcing data extracted taken from a gridded meteorological data base, sea level data from the Kattegat, and river runoff data to the different subbasins of the Baltic Sea from a hydrological data base. To improve the gridded meteorological data base a statistical model for the reduction of geostrophic winds to surface winds was developed. In the analysis it was shown that the calculated long-term salinity and temperature structures were stable and in good agreement with observations. This was made possible by using three different strait-flow models connecting the subbasins of the Baltic Sea. The seasonal and interannual variations of temperature and salinity were also well simulated by the model, implying that the coupling between the atmosphere and the Baltic Sea as well as the diapycnal mixing are reasonably well understood. The water cycle and the surface heat balance were calculated using the 18-year simulation. In the water-balance calculations it was shown that the volume flows from the large gulfs of the Baltic Sea were mainly due to baroclinic transports and that net precipitation added freshwater during the studied period, particularly to the large gulfs. From the heat-balance calculation it is concluded that the Baltic Sea is almost in local balance with the atmosphere. The Bothnian Bay, Gulf of Finland and Gulf of Riga loose heat, whereas the Bothnian Sea gains heat, calculated as long-term means.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275453"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275453"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275453; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275453]").text(description); $(".js-view-count[data-work-id=117275453]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275453; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275453']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275453, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275453]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275453,"title":"Modeling the variations of salinity and temperature in the large Gulfs of the Baltic Sea","translated_title":"","metadata":{"abstract":"ABSTRACT The modeling of salinity and temperature in Gulf of Bothnia, Gulf of Finland, and Gulf of Riga is investigated by using a coupled sea ice-ocean Baltic Sea model. 18 years, from late 1980 to the end of 1998, have been investigated. The forcing data extracted taken from a gridded meteorological data base, sea level data from the Kattegat, and river runoff data to the different subbasins of the Baltic Sea from a hydrological data base. To improve the gridded meteorological data base a statistical model for the reduction of geostrophic winds to surface winds was developed. In the analysis it was shown that the calculated long-term salinity and temperature structures were stable and in good agreement with observations. This was made possible by using three different strait-flow models connecting the subbasins of the Baltic Sea. The seasonal and interannual variations of temperature and salinity were also well simulated by the model, implying that the coupling between the atmosphere and the Baltic Sea as well as the diapycnal mixing are reasonably well understood. The water cycle and the surface heat balance were calculated using the 18-year simulation. In the water-balance calculations it was shown that the volume flows from the large gulfs of the Baltic Sea were mainly due to baroclinic transports and that net precipitation added freshwater during the studied period, particularly to the large gulfs. From the heat-balance calculation it is concluded that the Baltic Sea is almost in local balance with the atmosphere. The Bothnian Bay, Gulf of Finland and Gulf of Riga loose heat, whereas the Bothnian Sea gains heat, calculated as long-term means.","publisher":"Elsevier BV","publication_date":{"day":1,"month":2,"year":2003,"errors":{}},"publication_name":"Continental Shelf Research"},"translated_abstract":"ABSTRACT The modeling of salinity and temperature in Gulf of Bothnia, Gulf of Finland, and Gulf of Riga is investigated by using a coupled sea ice-ocean Baltic Sea model. 18 years, from late 1980 to the end of 1998, have been investigated. The forcing data extracted taken from a gridded meteorological data base, sea level data from the Kattegat, and river runoff data to the different subbasins of the Baltic Sea from a hydrological data base. To improve the gridded meteorological data base a statistical model for the reduction of geostrophic winds to surface winds was developed. In the analysis it was shown that the calculated long-term salinity and temperature structures were stable and in good agreement with observations. This was made possible by using three different strait-flow models connecting the subbasins of the Baltic Sea. The seasonal and interannual variations of temperature and salinity were also well simulated by the model, implying that the coupling between the atmosphere and the Baltic Sea as well as the diapycnal mixing are reasonably well understood. The water cycle and the surface heat balance were calculated using the 18-year simulation. In the water-balance calculations it was shown that the volume flows from the large gulfs of the Baltic Sea were mainly due to baroclinic transports and that net precipitation added freshwater during the studied period, particularly to the large gulfs. From the heat-balance calculation it is concluded that the Baltic Sea is almost in local balance with the atmosphere. The Bothnian Bay, Gulf of Finland and Gulf of Riga loose heat, whereas the Bothnian Sea gains heat, calculated as long-term means.","internal_url":"https://www.academia.edu/117275453/Modeling_the_variations_of_salinity_and_temperature_in_the_large_Gulfs_of_the_Baltic_Sea","translated_internal_url":"","created_at":"2024-04-09T07:54:16.818-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Modeling_the_variations_of_salinity_and_temperature_in_the_large_Gulfs_of_the_Baltic_Sea","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"ABSTRACT The modeling of salinity and temperature in Gulf of Bothnia, Gulf of Finland, and Gulf of Riga is investigated by using a coupled sea ice-ocean Baltic Sea model. 18 years, from late 1980 to the end of 1998, have been investigated. The forcing data extracted taken from a gridded meteorological data base, sea level data from the Kattegat, and river runoff data to the different subbasins of the Baltic Sea from a hydrological data base. To improve the gridded meteorological data base a statistical model for the reduction of geostrophic winds to surface winds was developed. In the analysis it was shown that the calculated long-term salinity and temperature structures were stable and in good agreement with observations. This was made possible by using three different strait-flow models connecting the subbasins of the Baltic Sea. The seasonal and interannual variations of temperature and salinity were also well simulated by the model, implying that the coupling between the atmosphere and the Baltic Sea as well as the diapycnal mixing are reasonably well understood. The water cycle and the surface heat balance were calculated using the 18-year simulation. In the water-balance calculations it was shown that the volume flows from the large gulfs of the Baltic Sea were mainly due to baroclinic transports and that net precipitation added freshwater during the studied period, particularly to the large gulfs. From the heat-balance calculation it is concluded that the Baltic Sea is almost in local balance with the atmosphere. The Bothnian Bay, Gulf of Finland and Gulf of Riga loose heat, whereas the Bothnian Sea gains heat, calculated as long-term means.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":82107,"name":"Salinity","url":"https://www.academia.edu/Documents/in/Salinity"},{"id":230435,"name":"Continental shelf","url":"https://www.academia.edu/Documents/in/Continental_shelf"},{"id":410933,"name":"Baltic Sea","url":"https://www.academia.edu/Documents/in/Baltic_Sea"}],"urls":[{"id":40966784,"url":"https://doi.org/10.1016/s0278-4343(02)00207-8"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275452"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275452/Sea_ICE_75_Dynamical_Report"><img alt="Research paper thumbnail of Sea ICE-75. Dynamical Report" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275452/Sea_ICE_75_Dynamical_Report">Sea ICE-75. Dynamical Report</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Field measurements on sea ice was carried out in the Bay of Bothnia during March 10-20, 1975. The...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Field measurements on sea ice was carried out in the Bay of Bothnia during March 10-20, 1975. The forces and parameters in the equation of motion for sea ice have been studied on the Mesoscale. Winds and currents were measured to calculate the wind and water stress, the ice mass distribution was studied, the tilting of the sea surface computed, vertical temperature and salinity soundings in the water made and surface temperatures at different ice types measured.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275452"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275452"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275452; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275452]").text(description); $(".js-view-count[data-work-id=117275452]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275452; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275452']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275452, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275452]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275452,"title":"Sea ICE-75. Dynamical Report","translated_title":"","metadata":{"abstract":"Field measurements on sea ice was carried out in the Bay of Bothnia during March 10-20, 1975. The forces and parameters in the equation of motion for sea ice have been studied on the Mesoscale. Winds and currents were measured to calculate the wind and water stress, the ice mass distribution was studied, the tilting of the sea surface computed, vertical temperature and salinity soundings in the water made and surface temperatures at different ice types measured.","publication_date":{"day":null,"month":null,"year":1976,"errors":{}}},"translated_abstract":"Field measurements on sea ice was carried out in the Bay of Bothnia during March 10-20, 1975. The forces and parameters in the equation of motion for sea ice have been studied on the Mesoscale. Winds and currents were measured to calculate the wind and water stress, the ice mass distribution was studied, the tilting of the sea surface computed, vertical temperature and salinity soundings in the water made and surface temperatures at different ice types measured.","internal_url":"https://www.academia.edu/117275452/Sea_ICE_75_Dynamical_Report","translated_internal_url":"","created_at":"2024-04-09T07:54:16.436-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Sea_ICE_75_Dynamical_Report","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Field measurements on sea ice was carried out in the Bay of Bothnia during March 10-20, 1975. The forces and parameters in the equation of motion for sea ice have been studied on the Mesoscale. Winds and currents were measured to calculate the wind and water stress, the ice mass distribution was studied, the tilting of the sea surface computed, vertical temperature and salinity soundings in the water made and surface temperatures at different ice types measured.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt","email":"eVZLQXFwL2JZcStJVG4yN0N2Z3dzeUNsRDl0bjBCbG13eittK3ZsMGpPb0VvVE5NcFQ2cnB3Wmc3NUk4YVVUbi0tVjROSmxKK0tEd3BCSDRCOUorclI0UT09--b13fb099a32cff0d392b5e31dfa4bd95e798ce39"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":29759,"name":"Sea Ice","url":"https://www.academia.edu/Documents/in/Sea_Ice"},{"id":73591,"name":"Mesoscale Meteorology","url":"https://www.academia.edu/Documents/in/Mesoscale_Meteorology"}],"urls":[{"id":40966782,"url":"https://trid.trb.org/view/57067"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275451"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275451/PEP_in_Baltex_A_pilot_study_of_evaporation_and_precipitation_in_the_Baltic_Sea"><img alt="Research paper thumbnail of PEP in Baltex. A pilot study of evaporation and precipitation in the Baltic Sea" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275451/PEP_in_Baltex_A_pilot_study_of_evaporation_and_precipitation_in_the_Baltic_Sea">PEP in Baltex. A pilot study of evaporation and precipitation in the Baltic Sea</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275451"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275451"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275451; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275451]").text(description); $(".js-view-count[data-work-id=117275451]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275451; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275451']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275451, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275451]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275451,"title":"PEP in Baltex. A pilot study of evaporation and precipitation in the Baltic Sea","translated_title":"","metadata":{"publication_date":{"day":null,"month":null,"year":1998,"errors":{}}},"translated_abstract":null,"internal_url":"https://www.academia.edu/117275451/PEP_in_Baltex_A_pilot_study_of_evaporation_and_precipitation_in_the_Baltic_Sea","translated_internal_url":"","created_at":"2024-04-09T07:54:16.214-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"PEP_in_Baltex_A_pilot_study_of_evaporation_and_precipitation_in_the_Baltic_Sea","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":null,"owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt","email":"NEVZRW9obXQyREVtMENCWk5RZitCZjNOWnIyUTllRzNpU003L2RtU05uS2dkMzg3VlNuYndCYXZFdEpZMld5Ni0tWjBMVVBOdzZnMWVGZlJNSXB5Z1Bydz09--cfcb616d0f4119db283e9fe797096b80cf00674a"},"attachments":[],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":13268,"name":"Evaporation","url":"https://www.academia.edu/Documents/in/Evaporation"},{"id":291658,"name":"Precipitation","url":"https://www.academia.edu/Documents/in/Precipitation"},{"id":410933,"name":"Baltic Sea","url":"https://www.academia.edu/Documents/in/Baltic_Sea"}],"urls":[{"id":40966781,"url":"https://dissem.in/p/16015199/pep-in-baltex-a-pilot-study-of-evaporation-and-precipitation-in-the-baltic-sea"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275449"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275449/On_cooling_and_initial_ice_formation_in_the_upper_layers_of_the_ocean"><img alt="Research paper thumbnail of On cooling and initial ice formation in the upper layers of the ocean" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275449/On_cooling_and_initial_ice_formation_in_the_upper_layers_of_the_ocean">On cooling and initial ice formation in the upper layers of the ocean</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275449"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275449"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275449; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275449]").text(description); $(".js-view-count[data-work-id=117275449]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275449; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275449']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275449, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275449]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275449,"title":"On cooling and initial ice formation in the upper layers of the ocean","translated_title":"","metadata":{"publication_date":{"day":null,"month":null,"year":1985,"errors":{}}},"translated_abstract":null,"internal_url":"https://www.academia.edu/117275449/On_cooling_and_initial_ice_formation_in_the_upper_layers_of_the_ocean","translated_internal_url":"","created_at":"2024-04-09T07:54:15.896-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"On_cooling_and_initial_ice_formation_in_the_upper_layers_of_the_ocean","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":null,"owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt","email":"VmJoaDNOMWticTNpcDIxR0JHSjhSSU10S0JpZDJBYzhVUDc1SFN4amYzVnlYMHh4VmZ5VWNZNzZpL01PL3VTTC0tNW9pTVJ4Z21xcHpHT1NSbzl1dkViZz09--b929e09b31687532af2a5c24d988cc8b98bb102f"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":29759,"name":"Sea Ice","url":"https://www.academia.edu/Documents/in/Sea_Ice"},{"id":77936,"name":"Text","url":"https://www.academia.edu/Documents/in/Text"},{"id":793808,"name":"Oceanografi","url":"https://www.academia.edu/Documents/in/Oceanografi"}],"urls":[{"id":40966780,"url":"https://gupea.ub.gu.se/handle/2077/13499"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275448"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275448/Forecasting_Ice_on_Lakes_Estuaries_and_Shelf_Seas"><img alt="Research paper thumbnail of Forecasting Ice on Lakes, Estuaries and Shelf Seas" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275448/Forecasting_Ice_on_Lakes_Estuaries_and_Shelf_Seas">Forecasting Ice on Lakes, Estuaries and Shelf Seas</a></div><div class="wp-workCard_item"><span>Springer eBooks</span><span>, 1999</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275448"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275448"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275448; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275448]").text(description); $(".js-view-count[data-work-id=117275448]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275448; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275448']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275448, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275448]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275448,"title":"Forecasting Ice on Lakes, Estuaries and Shelf Seas","translated_title":"","metadata":{"publisher":"Springer Nature","publication_date":{"day":null,"month":null,"year":1999,"errors":{}},"publication_name":"Springer eBooks"},"translated_abstract":null,"internal_url":"https://www.academia.edu/117275448/Forecasting_Ice_on_Lakes_Estuaries_and_Shelf_Seas","translated_internal_url":"","created_at":"2024-04-09T07:54:15.457-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Forecasting_Ice_on_Lakes_Estuaries_and_Shelf_Seas","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":null,"owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt","email":"WHZYSXRicmQ3c0IyVWtKaG50Z0xsbFMvVDNBcDJnVkJRT2pEUlZhcFdqRFBVQnRybkxCTUFUVUkxL3pjNTdpZS0tOEZKOTNQWFo4czBjaXF6bE4zZGMrdz09--98bf4ab95909fc140fe6c330564c08f493b56a1e"},"attachments":[],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":3755,"name":"Meteorology","url":"https://www.academia.edu/Documents/in/Meteorology"},{"id":905684,"name":"Shore","url":"https://www.academia.edu/Documents/in/Shore"},{"id":3647879,"name":"Springer Ebooks","url":"https://www.academia.edu/Documents/in/Springer_Ebooks"}],"urls":[{"id":40966779,"url":"https://doi.org/10.1007/978-3-642-60030-2_11"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275447"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275447/Parameterization_of_lake_thermodynamics_in_a_high_resolution_weather_forecasting_model"><img alt="Research paper thumbnail of Parameterization of lake thermodynamics in a high-resolution weather forecasting model" class="work-thumbnail" src="https://attachments.academia-assets.com/113175442/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275447/Parameterization_of_lake_thermodynamics_in_a_high_resolution_weather_forecasting_model">Parameterization of lake thermodynamics in a high-resolution weather forecasting model</a></div><div class="wp-workCard_item"><span>Tellus A</span><span>, Oct 1, 1996</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="44c5775b16cc24118032c7dcc3786e95" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":113175442,"asset_id":117275447,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/113175442/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275447"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275447"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275447; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275447]").text(description); $(".js-view-count[data-work-id=117275447]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275447; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275447']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275447, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "44c5775b16cc24118032c7dcc3786e95" } } $('.js-work-strip[data-work-id=117275447]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275447,"title":"Parameterization of lake thermodynamics in a high-resolution weather forecasting model","translated_title":"","metadata":{"publisher":"Wiley-Blackwell","publication_date":{"day":1,"month":10,"year":1996,"errors":{}},"publication_name":"Tellus A"},"translated_abstract":null,"internal_url":"https://www.academia.edu/117275447/Parameterization_of_lake_thermodynamics_in_a_high_resolution_weather_forecasting_model","translated_internal_url":"","created_at":"2024-04-09T07:54:14.796-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":113175442,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175442/thumbnails/1.jpg","file_name":"FULLTEXT01.pdf","download_url":"https://www.academia.edu/attachments/113175442/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Parameterization_of_lake_thermodynamics.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175442/FULLTEXT01-libre.pdf?1712674808=\u0026response-content-disposition=attachment%3B+filename%3DParameterization_of_lake_thermodynamics.pdf\u0026Expires=1734108629\u0026Signature=Bww2asKYXAc49r7-C2fFE~66zZeugVvbU3pwjOVX~mCZoSLOvmLEnYQtDYaATiD4rBGQHNGkmMdMlQHEe1xTgRRoyHh2GeVxztVd72f0dvYE-n3sQdE3fUIsmWVzJTIcikuE30U~Q5u4PQGqcc8CoDs8alR5TbiEzE0tuT630UKEeUvY6to0zosuU~C1AotRUHO-RWGsfV1hswMY1ckZybDqAaIqBc19LsD3KAfnhK7IViF7TNa5QIfxNUOuzqURhF7euRTDNfiwnhjENnleqT~JIF2GQpVkmVYi9iWpAZ83wtbTYEISxsb9VFTAoJsRNzkmoxnjaAo0UthKuMqTww__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Parameterization_of_lake_thermodynamics_in_a_high_resolution_weather_forecasting_model","translated_slug":"","page_count":14,"language":"en","content_type":"Work","summary":null,"owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":113175442,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175442/thumbnails/1.jpg","file_name":"FULLTEXT01.pdf","download_url":"https://www.academia.edu/attachments/113175442/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Parameterization_of_lake_thermodynamics.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175442/FULLTEXT01-libre.pdf?1712674808=\u0026response-content-disposition=attachment%3B+filename%3DParameterization_of_lake_thermodynamics.pdf\u0026Expires=1734108629\u0026Signature=Bww2asKYXAc49r7-C2fFE~66zZeugVvbU3pwjOVX~mCZoSLOvmLEnYQtDYaATiD4rBGQHNGkmMdMlQHEe1xTgRRoyHh2GeVxztVd72f0dvYE-n3sQdE3fUIsmWVzJTIcikuE30U~Q5u4PQGqcc8CoDs8alR5TbiEzE0tuT630UKEeUvY6to0zosuU~C1AotRUHO-RWGsfV1hswMY1ckZybDqAaIqBc19LsD3KAfnhK7IViF7TNa5QIfxNUOuzqURhF7euRTDNfiwnhjENnleqT~JIF2GQpVkmVYi9iWpAZ83wtbTYEISxsb9VFTAoJsRNzkmoxnjaAo0UthKuMqTww__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"},{"id":113175441,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175441/thumbnails/1.jpg","file_name":"FULLTEXT01.pdf","download_url":"https://www.academia.edu/attachments/113175441/download_file","bulk_download_file_name":"Parameterization_of_lake_thermodynamics.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175441/FULLTEXT01-libre.pdf?1712674810=\u0026response-content-disposition=attachment%3B+filename%3DParameterization_of_lake_thermodynamics.pdf\u0026Expires=1734108629\u0026Signature=NOF5Kae7Ah-Cnz1m8txSp7JNdrIHTkdYl1iGom-dIWmC3mnb1qngI6Ojai~tMeF9W2H0mEi3zfidZNgR6RnAXDzJuG13DGtkk~yOz8iRPcS6tawMnAn6VS1fRKU2S-v7jCa40ILlKI-UjyCDQvUbTaug2tuEFwjtczYWn4HtwJcj57jOrAzV6XkY1R5ADEKvwMGci4l5Da4lncxhzRnmRD4D5qfjFGCd2gi7puT3PJt-62Wv-rUTE-k3FEXQ3dvmca07JmjSEXRUi20xRqGF369baqpMslc-ApSYLLlklI3hGlu2m1qogxN3nwFd-I2bxInFS7HjhPOb~ZVjQ0pUnA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":522,"name":"Thermodynamics","url":"https://www.academia.edu/Documents/in/Thermodynamics"},{"id":3754,"name":"Climatology","url":"https://www.academia.edu/Documents/in/Climatology"},{"id":5980,"name":"Atmospheric Modeling","url":"https://www.academia.edu/Documents/in/Atmospheric_Modeling"},{"id":6962,"name":"Energy Conservation","url":"https://www.academia.edu/Documents/in/Energy_Conservation"},{"id":57433,"name":"Seasonality","url":"https://www.academia.edu/Documents/in/Seasonality"},{"id":60285,"name":"Atmospheric sciences","url":"https://www.academia.edu/Documents/in/Atmospheric_sciences"},{"id":195260,"name":"Weather Forecasting","url":"https://www.academia.edu/Documents/in/Weather_Forecasting"},{"id":309086,"name":"High Resolution","url":"https://www.academia.edu/Documents/in/High_Resolution"},{"id":391216,"name":"Size Distribution","url":"https://www.academia.edu/Documents/in/Size_Distribution"},{"id":444096,"name":"Air Temperature","url":"https://www.academia.edu/Documents/in/Air_Temperature"},{"id":468734,"name":"Turbulent Mixing","url":"https://www.academia.edu/Documents/in/Turbulent_Mixing"},{"id":597110,"name":"Tellus","url":"https://www.academia.edu/Documents/in/Tellus"}],"urls":[{"id":40966778,"url":"https://smhi.diva-portal.org/smash/get/diva2:897786/FULLTEXT01"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275444"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275444/Stratification_Turbulence_and_Services"><img alt="Research paper thumbnail of Stratification, Turbulence, and Services" class="work-thumbnail" src="https://attachments.academia-assets.com/113175436/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275444/Stratification_Turbulence_and_Services">Stratification, Turbulence, and Services</a></div><div class="wp-workCard_item"><span>A Philosophical View of the Ocean and Humanity</span><span>, 2020</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This chapter continues the dialogue between science and the ocean, starting with a concerned scie...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This chapter continues the dialogue between science and the ocean, starting with a concerned science view. A great fear is that global warming may reduce areas of sinking water, reducing ocean ventilation. The ocean responds with an image of a kelp forest-among the most beautiful and biologically productive marine ecosystems, and one that has served the ocean for many millions of years. Interpreting the kelp forest as a metaphor suggests a need to listen better and realize that humans can develop a society in a similar way, as a rich habitat for human growth with diverse groups of people in a healthy environment. For this to happen, human attitudes need to change to create a society that serves the ocean as kelp forests do. Keywords Ocean • Coastal seas • Climate change • Environmental change • Connecting science and the arts • Sustainability • Oceanography • Psychology • Philosophy Voice of the ocean: It is such a joy to serve life. Some of you speak of 'green thumbs', but I have 'brown fingers' that for millions of years have protected and served life. Listen carefully.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="1dd1e10b214775637fd73efbdfce951d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":113175436,"asset_id":117275444,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/113175436/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275444"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275444"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275444; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275444]").text(description); $(".js-view-count[data-work-id=117275444]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275444; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275444']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275444, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "1dd1e10b214775637fd73efbdfce951d" } } $('.js-work-strip[data-work-id=117275444]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275444,"title":"Stratification, Turbulence, and Services","translated_title":"","metadata":{"publisher":"Springer International Publishing","grobid_abstract":"This chapter continues the dialogue between science and the ocean, starting with a concerned science view. A great fear is that global warming may reduce areas of sinking water, reducing ocean ventilation. The ocean responds with an image of a kelp forest-among the most beautiful and biologically productive marine ecosystems, and one that has served the ocean for many millions of years. Interpreting the kelp forest as a metaphor suggests a need to listen better and realize that humans can develop a society in a similar way, as a rich habitat for human growth with diverse groups of people in a healthy environment. For this to happen, human attitudes need to change to create a society that serves the ocean as kelp forests do. Keywords Ocean • Coastal seas • Climate change • Environmental change • Connecting science and the arts • Sustainability • Oceanography • Psychology • Philosophy Voice of the ocean: It is such a joy to serve life. Some of you speak of 'green thumbs', but I have 'brown fingers' that for millions of years have protected and served life. Listen carefully.","publication_date":{"day":null,"month":null,"year":2020,"errors":{}},"publication_name":"A Philosophical View of the Ocean and Humanity","grobid_abstract_attachment_id":113175436},"translated_abstract":null,"internal_url":"https://www.academia.edu/117275444/Stratification_Turbulence_and_Services","translated_internal_url":"","created_at":"2024-04-09T07:54:13.999-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":113175436,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175436/thumbnails/1.jpg","file_name":"978-3-030-36680-3_5.pdf","download_url":"https://www.academia.edu/attachments/113175436/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Stratification_Turbulence_and_Services.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175436/978-3-030-36680-3_5-libre.pdf?1712674805=\u0026response-content-disposition=attachment%3B+filename%3DStratification_Turbulence_and_Services.pdf\u0026Expires=1734108629\u0026Signature=SdGTPIwRNEIV1kUmZ5k84rqZuZAb3Z1iCgCxyLdIo3~yWr4ROmbAeu4QhkYdTIyYBFax7Oz4HZg6zPZL7KRh-njLLnm4-ayALSL9LnRsqBWfTJiabBT3HfG9xOR8p~fpdM8sVa7lWMhMsyazWHBrTImCNwwu6Y90CMr9eWFslc21DLeBto3BaPEAUuEqaCqYmU8VfmdzAWAKdmwpIWKikrRO6gBcM-OQ4ioerc~Eeb10QtrDobO~4SQOvsEJgaXnvAP0y8gMDeIWqw-2hFZryjtEWN-RZyZdqX63VwSaX3AM34xEDdhpF-uKlvuR27nRovLfxv7VJfmNEMiJiSeziA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Stratification_Turbulence_and_Services","translated_slug":"","page_count":5,"language":"en","content_type":"Work","summary":"This chapter continues the dialogue between science and the ocean, starting with a concerned science view. A great fear is that global warming may reduce areas of sinking water, reducing ocean ventilation. The ocean responds with an image of a kelp forest-among the most beautiful and biologically productive marine ecosystems, and one that has served the ocean for many millions of years. Interpreting the kelp forest as a metaphor suggests a need to listen better and realize that humans can develop a society in a similar way, as a rich habitat for human growth with diverse groups of people in a healthy environment. For this to happen, human attitudes need to change to create a society that serves the ocean as kelp forests do. Keywords Ocean • Coastal seas • Climate change • Environmental change • Connecting science and the arts • Sustainability • Oceanography • Psychology • Philosophy Voice of the ocean: It is such a joy to serve life. Some of you speak of 'green thumbs', but I have 'brown fingers' that for millions of years have protected and served life. Listen carefully.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":113175436,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175436/thumbnails/1.jpg","file_name":"978-3-030-36680-3_5.pdf","download_url":"https://www.academia.edu/attachments/113175436/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Stratification_Turbulence_and_Services.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175436/978-3-030-36680-3_5-libre.pdf?1712674805=\u0026response-content-disposition=attachment%3B+filename%3DStratification_Turbulence_and_Services.pdf\u0026Expires=1734108629\u0026Signature=SdGTPIwRNEIV1kUmZ5k84rqZuZAb3Z1iCgCxyLdIo3~yWr4ROmbAeu4QhkYdTIyYBFax7Oz4HZg6zPZL7KRh-njLLnm4-ayALSL9LnRsqBWfTJiabBT3HfG9xOR8p~fpdM8sVa7lWMhMsyazWHBrTImCNwwu6Y90CMr9eWFslc21DLeBto3BaPEAUuEqaCqYmU8VfmdzAWAKdmwpIWKikrRO6gBcM-OQ4ioerc~Eeb10QtrDobO~4SQOvsEJgaXnvAP0y8gMDeIWqw-2hFZryjtEWN-RZyZdqX63VwSaX3AM34xEDdhpF-uKlvuR27nRovLfxv7VJfmNEMiJiSeziA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"},{"id":113175435,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175435/thumbnails/1.jpg","file_name":"978-3-030-36680-3_5.pdf","download_url":"https://www.academia.edu/attachments/113175435/download_file","bulk_download_file_name":"Stratification_Turbulence_and_Services.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175435/978-3-030-36680-3_5-libre.pdf?1712674804=\u0026response-content-disposition=attachment%3B+filename%3DStratification_Turbulence_and_Services.pdf\u0026Expires=1734108629\u0026Signature=Igbm4yQSUm8W1I-fL5~-KGXMJKrHguHdg1PouApRUkRC2asXYoYazYrrEzRfKF~U8SOF-e~GcoiJ0zPd~Bzctgmo4aK-tJGmXm6xlzp~sgsJaVtCw1-TsQFY5Fa0mYJG~GwFCcVcX5Jmyilq-Og0tVXycRUo-a5-hMeBgybDtx6uEFye5OdrVGViY~2K3LpbSBttWmlIVMSKgPem3lx10vBBM6ZnnRPGo8NqJZpO6qUzPLHX8J-Y4vd-S9P9~47zkJOFh29R5KBvPjSYXu9kQ6uIdPNkspuizjM2DYz-XYmO4FLossljA6rdwWkRdQxl8d3XXDoH-sErtjaD4m7Xmw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":85707,"name":"Habitat","url":"https://www.academia.edu/Documents/in/Habitat"},{"id":104980,"name":"Kelp Forest","url":"https://www.academia.edu/Documents/in/Kelp_Forest"},{"id":740846,"name":"Kelp","url":"https://www.academia.edu/Documents/in/Kelp"}],"urls":[{"id":40966776,"url":"http://link.springer.com/content/pdf/10.1007/978-3-030-36680-3_5"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275442"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275442/Ecosystems_and_Listening"><img alt="Research paper thumbnail of Ecosystems and Listening" class="work-thumbnail" src="https://attachments.academia-assets.com/113175432/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275442/Ecosystems_and_Listening">Ecosystems and Listening</a></div><div class="wp-workCard_item"><span>A Philosophical View of the Ocean and Humanity</span><span>, 2020</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This chapter highlights the conflict between human activity and marine ecosystems. The decline of...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This chapter highlights the conflict between human activity and marine ecosystems. The decline of various marine species due to human impact goes back more than a millennium but accelerated markedly in the 1950s. Hemingway wrote about the shift from sustainable to unsustainable attitudes towards fishing in his 1952 novel The Old Man and the Sea. Beautiful living marine resources are now mismanaged as if humanity and the ocean no longer had any relationship with each other. The ocean responds with disappointment at human lifestyles and attitudes, and invites us to listen better and realize that marine resources could give much more back if managed properly. Keywords Ocean • Coastal seas • Climate change • Environmental change • Connecting science and the arts • Sustainability • Oceanography • Psychology • Philosophy Voice of the ocean: I am so disappointed with humans' greedy approach to my beautiful living resources. You must listen better to me and to your hearts, and realize my limits in supporting you. If you listen carefully to me, all my resources can be much better used and, yes, I loved the dories. The northwestern Atlantic Ocean, where the cold Arctic water meets the warm Atlantic water, is a biologically rich area with abundant phytoplankton, zooplankton, and krill and historically excellent fishing conditions. For many centuries, the Grand Banks of Newfoundland were the site of large-scale fishing efforts. From small dories, fishers could catch cod, haddock, and other species of fish, which were then brought to the main fishing vessel that could serve a large number of dories and fishers. Little changed for several centuries and the Grand Banks remained an area with abundant marine resources. Each dory was generally handled by one or two fishers, who filled it with fish caught using hooks and lines. Rowing and sailing these boats, about five to six metres long, required great skill, and the fishers were well known for handling these boats under difficult and dangerous conditions, sometimes during fog when they lost contact with the mother ship. The first documented single-handed sailing across the Atlantic was by Alfred Johnson in 1876 using a five-metre dory. His voyage went from Gloucester, Massachusetts, USA to Abercastle, Wales and lasted 58 days (Kurlansky 1999).</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="04ecbad08a41010069834faba5739e69" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":113175432,"asset_id":117275442,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/113175432/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275442"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275442"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275442; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275442]").text(description); $(".js-view-count[data-work-id=117275442]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275442; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275442']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275442, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "04ecbad08a41010069834faba5739e69" } } $('.js-work-strip[data-work-id=117275442]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275442,"title":"Ecosystems and Listening","translated_title":"","metadata":{"publisher":"Springer International Publishing","grobid_abstract":"This chapter highlights the conflict between human activity and marine ecosystems. The decline of various marine species due to human impact goes back more than a millennium but accelerated markedly in the 1950s. Hemingway wrote about the shift from sustainable to unsustainable attitudes towards fishing in his 1952 novel The Old Man and the Sea. Beautiful living marine resources are now mismanaged as if humanity and the ocean no longer had any relationship with each other. The ocean responds with disappointment at human lifestyles and attitudes, and invites us to listen better and realize that marine resources could give much more back if managed properly. Keywords Ocean • Coastal seas • Climate change • Environmental change • Connecting science and the arts • Sustainability • Oceanography • Psychology • Philosophy Voice of the ocean: I am so disappointed with humans' greedy approach to my beautiful living resources. You must listen better to me and to your hearts, and realize my limits in supporting you. If you listen carefully to me, all my resources can be much better used and, yes, I loved the dories. The northwestern Atlantic Ocean, where the cold Arctic water meets the warm Atlantic water, is a biologically rich area with abundant phytoplankton, zooplankton, and krill and historically excellent fishing conditions. For many centuries, the Grand Banks of Newfoundland were the site of large-scale fishing efforts. From small dories, fishers could catch cod, haddock, and other species of fish, which were then brought to the main fishing vessel that could serve a large number of dories and fishers. Little changed for several centuries and the Grand Banks remained an area with abundant marine resources. Each dory was generally handled by one or two fishers, who filled it with fish caught using hooks and lines. Rowing and sailing these boats, about five to six metres long, required great skill, and the fishers were well known for handling these boats under difficult and dangerous conditions, sometimes during fog when they lost contact with the mother ship. The first documented single-handed sailing across the Atlantic was by Alfred Johnson in 1876 using a five-metre dory. His voyage went from Gloucester, Massachusetts, USA to Abercastle, Wales and lasted 58 days (Kurlansky 1999).","publication_date":{"day":null,"month":null,"year":2020,"errors":{}},"publication_name":"A Philosophical View of the Ocean and Humanity","grobid_abstract_attachment_id":113175432},"translated_abstract":null,"internal_url":"https://www.academia.edu/117275442/Ecosystems_and_Listening","translated_internal_url":"","created_at":"2024-04-09T07:54:13.004-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":113175432,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175432/thumbnails/1.jpg","file_name":"978-3-030-36680-3_11.pdf","download_url":"https://www.academia.edu/attachments/113175432/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Ecosystems_and_Listening.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175432/978-3-030-36680-3_11-libre.pdf?1712674805=\u0026response-content-disposition=attachment%3B+filename%3DEcosystems_and_Listening.pdf\u0026Expires=1734108629\u0026Signature=UR5eu7FKWSaTm6biVyuAUJDUfsQgeahlqoUaoi-4wuNBX9a6Ghu3qIxiBfnQIjGYlz8dLmsqcP~End-sPooFaf-YYffdt4pt9xIyclr~LnUVBHS7ZJE7gY1YxV-Fx6U7QIbIpZ7u6GkH1RkYuxDKRYAEEZuFA9KHJL4lLPhrnEIcKak4EYlQUJKSF6WhnYJsfq4QeYaBdi4GgwL24i9-PZDAMnYMejEZsQBOYTwajvop1T0moXxUhcxCKoAo2ndVkcOM0GWNZ5UjGOWE33n1QpSG2SOXFVxSJAlDMymzCdf2l68fllYDl9gbChJVklFSGHeyXxie-BPqTRhpJGO-vw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Ecosystems_and_Listening","translated_slug":"","page_count":6,"language":"en","content_type":"Work","summary":"This chapter highlights the conflict between human activity and marine ecosystems. The decline of various marine species due to human impact goes back more than a millennium but accelerated markedly in the 1950s. Hemingway wrote about the shift from sustainable to unsustainable attitudes towards fishing in his 1952 novel The Old Man and the Sea. Beautiful living marine resources are now mismanaged as if humanity and the ocean no longer had any relationship with each other. The ocean responds with disappointment at human lifestyles and attitudes, and invites us to listen better and realize that marine resources could give much more back if managed properly. Keywords Ocean • Coastal seas • Climate change • Environmental change • Connecting science and the arts • Sustainability • Oceanography • Psychology • Philosophy Voice of the ocean: I am so disappointed with humans' greedy approach to my beautiful living resources. You must listen better to me and to your hearts, and realize my limits in supporting you. If you listen carefully to me, all my resources can be much better used and, yes, I loved the dories. The northwestern Atlantic Ocean, where the cold Arctic water meets the warm Atlantic water, is a biologically rich area with abundant phytoplankton, zooplankton, and krill and historically excellent fishing conditions. For many centuries, the Grand Banks of Newfoundland were the site of large-scale fishing efforts. From small dories, fishers could catch cod, haddock, and other species of fish, which were then brought to the main fishing vessel that could serve a large number of dories and fishers. Little changed for several centuries and the Grand Banks remained an area with abundant marine resources. Each dory was generally handled by one or two fishers, who filled it with fish caught using hooks and lines. Rowing and sailing these boats, about five to six metres long, required great skill, and the fishers were well known for handling these boats under difficult and dangerous conditions, sometimes during fog when they lost contact with the mother ship. The first documented single-handed sailing across the Atlantic was by Alfred Johnson in 1876 using a five-metre dory. His voyage went from Gloucester, Massachusetts, USA to Abercastle, Wales and lasted 58 days (Kurlansky 1999).","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":113175432,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175432/thumbnails/1.jpg","file_name":"978-3-030-36680-3_11.pdf","download_url":"https://www.academia.edu/attachments/113175432/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Ecosystems_and_Listening.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175432/978-3-030-36680-3_11-libre.pdf?1712674805=\u0026response-content-disposition=attachment%3B+filename%3DEcosystems_and_Listening.pdf\u0026Expires=1734108629\u0026Signature=UR5eu7FKWSaTm6biVyuAUJDUfsQgeahlqoUaoi-4wuNBX9a6Ghu3qIxiBfnQIjGYlz8dLmsqcP~End-sPooFaf-YYffdt4pt9xIyclr~LnUVBHS7ZJE7gY1YxV-Fx6U7QIbIpZ7u6GkH1RkYuxDKRYAEEZuFA9KHJL4lLPhrnEIcKak4EYlQUJKSF6WhnYJsfq4QeYaBdi4GgwL24i9-PZDAMnYMejEZsQBOYTwajvop1T0moXxUhcxCKoAo2ndVkcOM0GWNZ5UjGOWE33n1QpSG2SOXFVxSJAlDMymzCdf2l68fllYDl9gbChJVklFSGHeyXxie-BPqTRhpJGO-vw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"},{"id":113175431,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/113175431/thumbnails/1.jpg","file_name":"978-3-030-36680-3_11.pdf","download_url":"https://www.academia.edu/attachments/113175431/download_file","bulk_download_file_name":"Ecosystems_and_Listening.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/113175431/978-3-030-36680-3_11-libre.pdf?1712674804=\u0026response-content-disposition=attachment%3B+filename%3DEcosystems_and_Listening.pdf\u0026Expires=1734108629\u0026Signature=WyxnlEYXH6W~FvGZoHNcbr2jgfDVdben4jV1sUJaBw9MksauwZFl8Ts6-2xhsZG3HGH4g3KbwoPkd55t6625-L55jbVwZxRMBEivHJd1gdSWU2-E6lBYMp~FiVPCPPnwjyL6XWec4IOqIMvIdvC09RXDLH4iDDn1H4M0RQY5OilkaS2oeFe5Hu8JDLewMre4rvCNWw2N8kFLIXxTL6EMx4bYBh~21W76LJO9~IjeUGQZBsbgLp55TLqplWFiAfo9S4NItqrHow~OXSbjjiPHpgkOK7M1AyoFxSDtjwJgcPme9tKCarbuallPkVcdtuatP9q~lCI8CwlSoGRJ7CjLrQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":54534,"name":"Humanity","url":"https://www.academia.edu/Documents/in/Humanity"},{"id":79742,"name":"Fishing","url":"https://www.academia.edu/Documents/in/Fishing"},{"id":209760,"name":"Disappointment","url":"https://www.academia.edu/Documents/in/Disappointment"},{"id":1022026,"name":"Marine ecosystem","url":"https://www.academia.edu/Documents/in/Marine_ecosystem"}],"urls":[{"id":40966773,"url":"http://link.springer.com/content/pdf/10.1007/978-3-030-36680-3_11"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275438"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275438/Replication_Data_for_A_new_numerical_model_for_understanding_free_and_dissolved_gas_progression_towards_the_atmosphere_in_aquatic_methane_seepage_systems"><img alt="Research paper thumbnail of Replication Data for: A new numerical model for understanding free and dissolved gas progression towards the atmosphere in aquatic methane seepage systems" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275438/Replication_Data_for_A_new_numerical_model_for_understanding_free_and_dissolved_gas_progression_towards_the_atmosphere_in_aquatic_methane_seepage_systems">Replication Data for: A new numerical model for understanding free and dissolved gas progression towards the atmosphere in aquatic methane seepage systems</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This dataset contains the files needed to replicate the reference simulation results of the numer...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This dataset contains the files needed to replicate the reference simulation results of the numerical model M2PG1. Please refer to the README.txt file for detailed instructions on how to reproduce the simulation results.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275438"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275438"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275438; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275438]").text(description); $(".js-view-count[data-work-id=117275438]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275438; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275438']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275438, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275438]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275438,"title":"Replication Data for: A new numerical model for understanding free and dissolved gas progression towards the atmosphere in aquatic methane seepage systems","translated_title":"","metadata":{"abstract":"This dataset contains the files needed to replicate the reference simulation results of the numerical model M2PG1. Please refer to the README.txt file for detailed instructions on how to reproduce the simulation results.","publication_date":{"day":null,"month":null,"year":2019,"errors":{}}},"translated_abstract":"This dataset contains the files needed to replicate the reference simulation results of the numerical model M2PG1. Please refer to the README.txt file for detailed instructions on how to reproduce the simulation results.","internal_url":"https://www.academia.edu/117275438/Replication_Data_for_A_new_numerical_model_for_understanding_free_and_dissolved_gas_progression_towards_the_atmosphere_in_aquatic_methane_seepage_systems","translated_internal_url":"","created_at":"2024-04-09T07:54:06.718-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Replication_Data_for_A_new_numerical_model_for_understanding_free_and_dissolved_gas_progression_towards_the_atmosphere_in_aquatic_methane_seepage_systems","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"This dataset contains the files needed to replicate the reference simulation results of the numerical model M2PG1. Please refer to the README.txt file for detailed instructions on how to reproduce the simulation results.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt","email":"SFBpV0c3eHZUOHNoK3diUmR2eDRVc3F0QXhoeUZGcVhiSTRUTjJQWWxFd3ExdGozV0trK1JjRGpEeWtBQXFtMC0tVXRVam13Nm9PRlNSQ1RZQjU0cXU1Zz09--d03f91ee0a1c2cf5db286d15e8b4944546f3bf14"},"attachments":[],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":156347,"name":"Methane","url":"https://www.academia.edu/Documents/in/Methane"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275437"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/117275437/Currents_Circulation_and_Vulnerability"><img alt="Research paper thumbnail of Currents, Circulation, and Vulnerability" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/117275437/Currents_Circulation_and_Vulnerability">Currents, Circulation, and Vulnerability</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275437"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275437"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275437; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275437]").text(description); $(".js-view-count[data-work-id=117275437]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275437; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275437']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275437, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275437]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275437,"title":"Currents, Circulation, and Vulnerability","translated_title":"","metadata":{"publication_date":{"day":null,"month":null,"year":2020,"errors":{}}},"translated_abstract":null,"internal_url":"https://www.academia.edu/117275437/Currents_Circulation_and_Vulnerability","translated_internal_url":"","created_at":"2024-04-09T07:54:06.404-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Currents_Circulation_and_Vulnerability","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":null,"owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt","email":"bExBNzVTRGZ6U09HSjl6YnZrc29HbEFxM1RoTnJrNXVXM0Z2aWMzdDRVcGpzc0RvZ0tUWDdNMXlkSWxJNGdmZy0tRnRCdUhQNDNhbWY1aWVNUWg3RWFoQT09--9309c9f008c3836ac098a2fbb7f64b81d7db9d6e"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":604678,"name":"Eddy","url":"https://www.academia.edu/Documents/in/Eddy"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275436"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/117275436/Variations_of_ice_properties_in_an_ice_area_of_1x2_km_in_the_Gulf_of_Bothnia_March_1988"><img alt="Research paper thumbnail of Variations of ice properties in an ice area of 1x2 km in the Gulf of Bothnia March 1988" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/117275436/Variations_of_ice_properties_in_an_ice_area_of_1x2_km_in_the_Gulf_of_Bothnia_March_1988">Variations of ice properties in an ice area of 1x2 km in the Gulf of Bothnia March 1988</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">During the Bothnian Experiment in Preparation for ERS-1 (BEPERS-88), snow and ice thickness, sali...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">During the Bothnian Experiment in Preparation for ERS-1 (BEPERS-88), snow and ice thickness, salinity, density, crystal shape and ice strength were investigated. In a rectangular area of 1 x 2km, data from 12 stations is presented. The area covered level-ice, several pressure ridges and a belt of rafted and hummocked ice. The origin of the ice is discussed based on information given from vertical thin sections at different stations. Index values of ice strength were obtained from pressuremeter tests performed at six drilled holes at each station. The presence of weak ice in the area is discussed.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275436"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275436"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275436; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275436]").text(description); $(".js-view-count[data-work-id=117275436]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275436; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275436']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275436, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275436]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275436,"title":"Variations of ice properties in an ice area of 1x2 km in the Gulf of Bothnia March 1988","translated_title":"","metadata":{"abstract":"During the Bothnian Experiment in Preparation for ERS-1 (BEPERS-88), snow and ice thickness, salinity, density, crystal shape and ice strength were investigated. In a rectangular area of 1 x 2km, data from 12 stations is presented. The area covered level-ice, several pressure ridges and a belt of rafted and hummocked ice. The origin of the ice is discussed based on information given from vertical thin sections at different stations. Index values of ice strength were obtained from pressuremeter tests performed at six drilled holes at each station. The presence of weak ice in the area is discussed.","publication_date":{"day":null,"month":null,"year":1989,"errors":{}}},"translated_abstract":"During the Bothnian Experiment in Preparation for ERS-1 (BEPERS-88), snow and ice thickness, salinity, density, crystal shape and ice strength were investigated. In a rectangular area of 1 x 2km, data from 12 stations is presented. The area covered level-ice, several pressure ridges and a belt of rafted and hummocked ice. The origin of the ice is discussed based on information given from vertical thin sections at different stations. Index values of ice strength were obtained from pressuremeter tests performed at six drilled holes at each station. The presence of weak ice in the area is discussed.","internal_url":"https://www.academia.edu/117275436/Variations_of_ice_properties_in_an_ice_area_of_1x2_km_in_the_Gulf_of_Bothnia_March_1988","translated_internal_url":"","created_at":"2024-04-09T07:54:05.522-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Variations_of_ice_properties_in_an_ice_area_of_1x2_km_in_the_Gulf_of_Bothnia_March_1988","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"During the Bothnian Experiment in Preparation for ERS-1 (BEPERS-88), snow and ice thickness, salinity, density, crystal shape and ice strength were investigated. In a rectangular area of 1 x 2km, data from 12 stations is presented. The area covered level-ice, several pressure ridges and a belt of rafted and hummocked ice. The origin of the ice is discussed based on information given from vertical thin sections at different stations. Index values of ice strength were obtained from pressuremeter tests performed at six drilled holes at each station. The presence of weak ice in the area is discussed.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":29759,"name":"Sea Ice","url":"https://www.academia.edu/Documents/in/Sea_Ice"},{"id":197149,"name":"SNOW","url":"https://www.academia.edu/Documents/in/SNOW"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275435"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/117275435/Heat_Balance_Water_Temperature_and_Interpretations"><img alt="Research paper thumbnail of Heat Balance, Water Temperature, and Interpretations" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/117275435/Heat_Balance_Water_Temperature_and_Interpretations">Heat Balance, Water Temperature, and Interpretations</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The heat balance that determines the earth’s temperature represents an interesting and complex in...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The heat balance that determines the earth’s temperature represents an interesting and complex interplay between the sun, the earth, and our behaviour. The ocean plays many important roles in this, such as being the earth’s most important heat storage sink. Evaporation from the ocean surface due to latent heat flux works like a steam engine, driving large-scale atmospheric circulation. Long-wave radiation emitted from the earth’s surface is partly reflected back from the atmosphere by the GHGs that blanket the earth, protecting it from cooling. The human impact comes from anthropogenic landscape change and an increase in atmospheric GHG levels, for example, from fossil fuel burning, which influences the long-wave radiation reflected back to the surface. Today it is frighteningly clear that humans are influencing the ocean through global warming and ocean acidification. Will humans be able to reduce global warming or not? The ocean sends an image of a red jellyfish swimming slowly to...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275435"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275435"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275435; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275435]").text(description); $(".js-view-count[data-work-id=117275435]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275435; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275435']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275435, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275435]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275435,"title":"Heat Balance, Water Temperature, and Interpretations","translated_title":"","metadata":{"abstract":"The heat balance that determines the earth’s temperature represents an interesting and complex interplay between the sun, the earth, and our behaviour. The ocean plays many important roles in this, such as being the earth’s most important heat storage sink. Evaporation from the ocean surface due to latent heat flux works like a steam engine, driving large-scale atmospheric circulation. Long-wave radiation emitted from the earth’s surface is partly reflected back from the atmosphere by the GHGs that blanket the earth, protecting it from cooling. The human impact comes from anthropogenic landscape change and an increase in atmospheric GHG levels, for example, from fossil fuel burning, which influences the long-wave radiation reflected back to the surface. Today it is frighteningly clear that humans are influencing the ocean through global warming and ocean acidification. Will humans be able to reduce global warming or not? The ocean sends an image of a red jellyfish swimming slowly to...","publication_date":{"day":null,"month":null,"year":2020,"errors":{}}},"translated_abstract":"The heat balance that determines the earth’s temperature represents an interesting and complex interplay between the sun, the earth, and our behaviour. The ocean plays many important roles in this, such as being the earth’s most important heat storage sink. Evaporation from the ocean surface due to latent heat flux works like a steam engine, driving large-scale atmospheric circulation. Long-wave radiation emitted from the earth’s surface is partly reflected back from the atmosphere by the GHGs that blanket the earth, protecting it from cooling. The human impact comes from anthropogenic landscape change and an increase in atmospheric GHG levels, for example, from fossil fuel burning, which influences the long-wave radiation reflected back to the surface. Today it is frighteningly clear that humans are influencing the ocean through global warming and ocean acidification. Will humans be able to reduce global warming or not? The ocean sends an image of a red jellyfish swimming slowly to...","internal_url":"https://www.academia.edu/117275435/Heat_Balance_Water_Temperature_and_Interpretations","translated_internal_url":"","created_at":"2024-04-09T07:54:05.109-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Heat_Balance_Water_Temperature_and_Interpretations","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"The heat balance that determines the earth’s temperature represents an interesting and complex interplay between the sun, the earth, and our behaviour. The ocean plays many important roles in this, such as being the earth’s most important heat storage sink. Evaporation from the ocean surface due to latent heat flux works like a steam engine, driving large-scale atmospheric circulation. Long-wave radiation emitted from the earth’s surface is partly reflected back from the atmosphere by the GHGs that blanket the earth, protecting it from cooling. The human impact comes from anthropogenic landscape change and an increase in atmospheric GHG levels, for example, from fossil fuel burning, which influences the long-wave radiation reflected back to the surface. Today it is frighteningly clear that humans are influencing the ocean through global warming and ocean acidification. Will humans be able to reduce global warming or not? The ocean sends an image of a red jellyfish swimming slowly to...","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":681573,"name":"Heat Wave","url":"https://www.academia.edu/Documents/in/Heat_Wave"},{"id":2956968,"name":"Latent Heat","url":"https://www.academia.edu/Documents/in/Latent_Heat"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275434"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/117275434/Scenarios_the_Future_and_Simplicity"><img alt="Research paper thumbnail of Scenarios, the Future, and Simplicity" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/117275434/Scenarios_the_Future_and_Simplicity">Scenarios, the Future, and Simplicity</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Many are trying to foresee what will happen in the future. Numerical calculations of changes in s...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Many are trying to foresee what will happen in the future. Numerical calculations of changes in society often rely on statistical methods with no capacity to predict the future. Many try to relate various parameters to one another, hoping to gain knowledge of what is to come. Weather forecasting can provide information about conditions some days in advance. It is clear that emissions of carbon dioxide and other anthropogenic GHGs need to be reduced to prevent global warming. However, the global earth system models applied in climate change assessments rely on prescribed emission storylines and their projections are conditional on the assumed forcing. A major question for society is how to develop a greener and more sustainable future. The ocean responds by sending an image of barnacles adhering to a cliff, indicating that humans need to slow down, learn more from the ocean, and build durable and trusting relationships.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275434"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275434"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275434; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275434]").text(description); $(".js-view-count[data-work-id=117275434]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275434; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275434']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275434, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275434]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275434,"title":"Scenarios, the Future, and Simplicity","translated_title":"","metadata":{"abstract":"Many are trying to foresee what will happen in the future. Numerical calculations of changes in society often rely on statistical methods with no capacity to predict the future. Many try to relate various parameters to one another, hoping to gain knowledge of what is to come. Weather forecasting can provide information about conditions some days in advance. It is clear that emissions of carbon dioxide and other anthropogenic GHGs need to be reduced to prevent global warming. However, the global earth system models applied in climate change assessments rely on prescribed emission storylines and their projections are conditional on the assumed forcing. A major question for society is how to develop a greener and more sustainable future. The ocean responds by sending an image of barnacles adhering to a cliff, indicating that humans need to slow down, learn more from the ocean, and build durable and trusting relationships.","publication_date":{"day":null,"month":null,"year":2020,"errors":{}}},"translated_abstract":"Many are trying to foresee what will happen in the future. Numerical calculations of changes in society often rely on statistical methods with no capacity to predict the future. Many try to relate various parameters to one another, hoping to gain knowledge of what is to come. Weather forecasting can provide information about conditions some days in advance. It is clear that emissions of carbon dioxide and other anthropogenic GHGs need to be reduced to prevent global warming. However, the global earth system models applied in climate change assessments rely on prescribed emission storylines and their projections are conditional on the assumed forcing. A major question for society is how to develop a greener and more sustainable future. The ocean responds by sending an image of barnacles adhering to a cliff, indicating that humans need to slow down, learn more from the ocean, and build durable and trusting relationships.","internal_url":"https://www.academia.edu/117275434/Scenarios_the_Future_and_Simplicity","translated_internal_url":"","created_at":"2024-04-09T07:54:04.395-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Scenarios_the_Future_and_Simplicity","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Many are trying to foresee what will happen in the future. Numerical calculations of changes in society often rely on statistical methods with no capacity to predict the future. Many try to relate various parameters to one another, hoping to gain knowledge of what is to come. Weather forecasting can provide information about conditions some days in advance. It is clear that emissions of carbon dioxide and other anthropogenic GHGs need to be reduced to prevent global warming. However, the global earth system models applied in climate change assessments rely on prescribed emission storylines and their projections are conditional on the assumed forcing. A major question for society is how to develop a greener and more sustainable future. The ocean responds by sending an image of barnacles adhering to a cliff, indicating that humans need to slow down, learn more from the ocean, and build durable and trusting relationships.","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[],"research_interests":[{"id":1512,"name":"Climate Change","url":"https://www.academia.edu/Documents/in/Climate_Change"},{"id":235683,"name":"Simplicity","url":"https://www.academia.edu/Documents/in/Simplicity"},{"id":251654,"name":"Greenhouse Gas","url":"https://www.academia.edu/Documents/in/Greenhouse_Gas"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="117275433"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/117275433/The_Development_of_Climate_Science_of_the_Baltic_Sea_Region"><img alt="Research paper thumbnail of The Development of Climate Science of the Baltic Sea Region" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/117275433/The_Development_of_Climate_Science_of_the_Baltic_Sea_Region">The Development of Climate Science of the Baltic Sea Region</a></div><div class="wp-workCard_item"><span>Oxford Research Encyclopedia of Climate Science</span><span>, 2017</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Dramatic climate changes have occurred in the Baltic Sea region caused by changes in orbital move...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Dramatic climate changes have occurred in the Baltic Sea region caused by changes in orbital movement in the earth–sun system and the melting of the Fennoscandian Ice Sheet. Added to these longer-term changes, changes have occurred at all timescales, caused mainly by variations in large-scale atmospheric pressure systems due to competition between the meandering midlatitude low-pressure systems and high-pressure systems. Here we follow the development of climate science of the Baltic Sea from when observations began in the 18th century to the early 21st century. The question of why the water level is sinking around the Baltic Sea coasts could not be answered until the ideas of postglacial uplift and the thermal history of the earth were better understood in the 19th century and periodic behavior in climate related time series attracted scientific interest. Herring and sardine fishing successes and failures have led to investigations of fishery and climate change and to the realizati...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="117275433"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="117275433"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 117275433; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=117275433]").text(description); $(".js-view-count[data-work-id=117275433]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 117275433; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='117275433']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 117275433, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=117275433]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":117275433,"title":"The Development of Climate Science of the Baltic Sea Region","translated_title":"","metadata":{"abstract":"Dramatic climate changes have occurred in the Baltic Sea region caused by changes in orbital movement in the earth–sun system and the melting of the Fennoscandian Ice Sheet. Added to these longer-term changes, changes have occurred at all timescales, caused mainly by variations in large-scale atmospheric pressure systems due to competition between the meandering midlatitude low-pressure systems and high-pressure systems. Here we follow the development of climate science of the Baltic Sea from when observations began in the 18th century to the early 21st century. The question of why the water level is sinking around the Baltic Sea coasts could not be answered until the ideas of postglacial uplift and the thermal history of the earth were better understood in the 19th century and periodic behavior in climate related time series attracted scientific interest. Herring and sardine fishing successes and failures have led to investigations of fishery and climate change and to the realizati...","publisher":"Oxford University Press","publication_date":{"day":null,"month":null,"year":2017,"errors":{}},"publication_name":"Oxford Research Encyclopedia of Climate Science"},"translated_abstract":"Dramatic climate changes have occurred in the Baltic Sea region caused by changes in orbital movement in the earth–sun system and the melting of the Fennoscandian Ice Sheet. Added to these longer-term changes, changes have occurred at all timescales, caused mainly by variations in large-scale atmospheric pressure systems due to competition between the meandering midlatitude low-pressure systems and high-pressure systems. Here we follow the development of climate science of the Baltic Sea from when observations began in the 18th century to the early 21st century. The question of why the water level is sinking around the Baltic Sea coasts could not be answered until the ideas of postglacial uplift and the thermal history of the earth were better understood in the 19th century and periodic behavior in climate related time series attracted scientific interest. Herring and sardine fishing successes and failures have led to investigations of fishery and climate change and to the realizati...","internal_url":"https://www.academia.edu/117275433/The_Development_of_Climate_Science_of_the_Baltic_Sea_Region","translated_internal_url":"","created_at":"2024-04-09T07:54:03.800-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"The_Development_of_Climate_Science_of_the_Baltic_Sea_Region","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Dramatic climate changes have occurred in the Baltic Sea region caused by changes in orbital movement in the earth–sun system and the melting of the Fennoscandian Ice Sheet. Added to these longer-term changes, changes have occurred at all timescales, caused mainly by variations in large-scale atmospheric pressure systems due to competition between the meandering midlatitude low-pressure systems and high-pressure systems. Here we follow the development of climate science of the Baltic Sea from when observations began in the 18th century to the early 21st century. The question of why the water level is sinking around the Baltic Sea coasts could not be answered until the ideas of postglacial uplift and the thermal history of the earth were better understood in the 19th century and periodic behavior in climate related time series attracted scientific interest. Herring and sardine fishing successes and failures have led to investigations of fishery and climate change and to the realizati...","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":1512,"name":"Climate Change","url":"https://www.academia.edu/Documents/in/Climate_Change"},{"id":45405,"name":"Global Warming","url":"https://www.academia.edu/Documents/in/Global_Warming"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="2852664" id="books"><div class="js-work-strip profile--work_container" data-work-id="43057604"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/43057604/A_Philosophical_View_of_the_Ocean_and_Humanity"><img alt="Research paper thumbnail of A Philosophical View of the Ocean and Humanity" class="work-thumbnail" src="https://attachments.academia-assets.com/63317430/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/43057604/A_Philosophical_View_of_the_Ocean_and_Humanity">A Philosophical View of the Ocean and Humanity</a></div><div class="wp-workCard_item"><span>Springer Nature</span><span>, 2020</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This book is about the ocean and about the future. It is written in two modes, a concerned analyt...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This book is about the ocean and about the future. It is written in two modes, a concerned analytical scientific mode and an intuitive artistic mode in which the ocean is given a voice. The disconnect in the relationship between human dependency on and feelings about the ocean is examined in a dialogue between these two modes. The book illustrates how science and the arts can be connected to increase our awareness of the state of the ocean and support behavioural change. The book is intended for university students and researchers, but will speak to anyone who would like to contribute to the sustainable use of the ocean. <br /> <br />The ocean’s services to humankind are enormous and fundamental, and their value is inestimable. A change in human attitudes towards the ocean should be based on something other than simplistic and reductive economic costing. The attitude change needs to be based on a fundamental shift in our understanding of human values and how we interact with one another and with our environment. Antidotes to narrow thinking, fragmented vision, alienation, despair, and fear involve the integration of curiosity, courage, listening, hope, and simplicity in daily life. The beauty and vulnerability of both the ocean and humanity are facts that can inspire improved health and harmony, a vision well formulated by the United Nations in its 17 Sustainable Development Goals.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c94b2d03d4597941766f01d80b27843b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":63317430,"asset_id":43057604,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/63317430/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="43057604"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="43057604"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 43057604; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=43057604]").text(description); $(".js-view-count[data-work-id=43057604]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 43057604; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='43057604']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 43057604, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "c94b2d03d4597941766f01d80b27843b" } } $('.js-work-strip[data-work-id=43057604]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":43057604,"title":"A Philosophical View of the Ocean and Humanity","translated_title":"","metadata":{"doi":"10.1007/978-3-030-36680-3.","abstract":"This book is about the ocean and about the future. It is written in two modes, a concerned analytical scientific mode and an intuitive artistic mode in which the ocean is given a voice. The disconnect in the relationship between human dependency on and feelings about the ocean is examined in a dialogue between these two modes. The book illustrates how science and the arts can be connected to increase our awareness of the state of the ocean and support behavioural change. The book is intended for university students and researchers, but will speak to anyone who would like to contribute to the sustainable use of the ocean.\r\n\r\nThe ocean’s services to humankind are enormous and fundamental, and their value is inestimable. A change in human attitudes towards the ocean should be based on something other than simplistic and reductive economic costing. The attitude change needs to be based on a fundamental shift in our understanding of human values and how we interact with one another and with our environment. Antidotes to narrow thinking, fragmented vision, alienation, despair, and fear involve the integration of curiosity, courage, listening, hope, and simplicity in daily life. The beauty and vulnerability of both the ocean and humanity are facts that can inspire improved health and harmony, a vision well formulated by the United Nations in its 17 Sustainable Development Goals. \r\n","publication_date":{"day":null,"month":null,"year":2020,"errors":{}},"publication_name":"Springer Nature"},"translated_abstract":"This book is about the ocean and about the future. It is written in two modes, a concerned analytical scientific mode and an intuitive artistic mode in which the ocean is given a voice. The disconnect in the relationship between human dependency on and feelings about the ocean is examined in a dialogue between these two modes. The book illustrates how science and the arts can be connected to increase our awareness of the state of the ocean and support behavioural change. The book is intended for university students and researchers, but will speak to anyone who would like to contribute to the sustainable use of the ocean.\r\n\r\nThe ocean’s services to humankind are enormous and fundamental, and their value is inestimable. A change in human attitudes towards the ocean should be based on something other than simplistic and reductive economic costing. The attitude change needs to be based on a fundamental shift in our understanding of human values and how we interact with one another and with our environment. Antidotes to narrow thinking, fragmented vision, alienation, despair, and fear involve the integration of curiosity, courage, listening, hope, and simplicity in daily life. The beauty and vulnerability of both the ocean and humanity are facts that can inspire improved health and harmony, a vision well formulated by the United Nations in its 17 Sustainable Development Goals. \r\n","internal_url":"https://www.academia.edu/43057604/A_Philosophical_View_of_the_Ocean_and_Humanity","translated_internal_url":"","created_at":"2020-05-15T02:02:24.079-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":11956707,"coauthors_can_edit":true,"document_type":"book","co_author_tags":[],"downloadable_attachments":[{"id":63317430,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/63317430/thumbnails/1.jpg","file_name":"ProductFlyer_978303036679720200515-127059-1bef4im.pdf","download_url":"https://www.academia.edu/attachments/63317430/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"A_Philosophical_View_of_the_Ocean_and_Hu.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/63317430/ProductFlyer_978303036679720200515-127059-1bef4im-libre.pdf?1589534422=\u0026response-content-disposition=attachment%3B+filename%3DA_Philosophical_View_of_the_Ocean_and_Hu.pdf\u0026Expires=1734108629\u0026Signature=GxTxxstLC1Ao8-87rG4HJrXBe6WgglfCfpZgmFPTCrM09~4e10QltjFAvyckm9DCUN37PyTvDeLCOZ9tdQ44VMMib1~nBg8kCC-vkrovAJwZER4Y6SL1YklqaBbInKZN3fxUmwW3NQAQUuUMfKZ1-c04D-aQqBbmV06jNUEpLgEYnZFyb0qkgwU-rYILH9lRZL70tAuaD6Pvo72LstMtDyN6ms-9NcA4pJkSQ6VnIBuTEvhH~LwleLWvobZjDlLhUSmLi84KFMqW1OD6VFZrtK8NWqYGyV-MsLCGgkIG4JUIEUQHckt2Tr2k0vJnUJTq65QRA0qlck7XQLpnPUQ9Og__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"A_Philosophical_View_of_the_Ocean_and_Humanity","translated_slug":"","page_count":1,"language":"en","content_type":"Work","summary":"This book is about the ocean and about the future. It is written in two modes, a concerned analytical scientific mode and an intuitive artistic mode in which the ocean is given a voice. The disconnect in the relationship between human dependency on and feelings about the ocean is examined in a dialogue between these two modes. The book illustrates how science and the arts can be connected to increase our awareness of the state of the ocean and support behavioural change. The book is intended for university students and researchers, but will speak to anyone who would like to contribute to the sustainable use of the ocean.\r\n\r\nThe ocean’s services to humankind are enormous and fundamental, and their value is inestimable. A change in human attitudes towards the ocean should be based on something other than simplistic and reductive economic costing. The attitude change needs to be based on a fundamental shift in our understanding of human values and how we interact with one another and with our environment. Antidotes to narrow thinking, fragmented vision, alienation, despair, and fear involve the integration of curiosity, courage, listening, hope, and simplicity in daily life. The beauty and vulnerability of both the ocean and humanity are facts that can inspire improved health and harmony, a vision well formulated by the United Nations in its 17 Sustainable Development Goals. \r\n","owner":{"id":11956707,"first_name":"Anders","middle_initials":"","last_name":"Omstedt","page_name":"AndersOmstedt","domain_name":"gu-se","created_at":"2014-05-11T22:16:00.755-07:00","display_name":"Anders Omstedt","url":"https://gu-se.academia.edu/AndersOmstedt"},"attachments":[{"id":63317430,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/63317430/thumbnails/1.jpg","file_name":"ProductFlyer_978303036679720200515-127059-1bef4im.pdf","download_url":"https://www.academia.edu/attachments/63317430/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"A_Philosophical_View_of_the_Ocean_and_Hu.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/63317430/ProductFlyer_978303036679720200515-127059-1bef4im-libre.pdf?1589534422=\u0026response-content-disposition=attachment%3B+filename%3DA_Philosophical_View_of_the_Ocean_and_Hu.pdf\u0026Expires=1734108629\u0026Signature=GxTxxstLC1Ao8-87rG4HJrXBe6WgglfCfpZgmFPTCrM09~4e10QltjFAvyckm9DCUN37PyTvDeLCOZ9tdQ44VMMib1~nBg8kCC-vkrovAJwZER4Y6SL1YklqaBbInKZN3fxUmwW3NQAQUuUMfKZ1-c04D-aQqBbmV06jNUEpLgEYnZFyb0qkgwU-rYILH9lRZL70tAuaD6Pvo72LstMtDyN6ms-9NcA4pJkSQ6VnIBuTEvhH~LwleLWvobZjDlLhUSmLi84KFMqW1OD6VFZrtK8NWqYGyV-MsLCGgkIG4JUIEUQHckt2Tr2k0vJnUJTq65QRA0qlck7XQLpnPUQ9Og__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="11965332"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/11965332/Second_Assessment_of_Climate_Change_for_the_Baltic_Sea_Basin"><img alt="Research paper thumbnail of Second Assessment of Climate Change for the Baltic Sea Basin" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/11965332/Second_Assessment_of_Climate_Change_for_the_Baltic_Sea_Basin">Second Assessment of Climate Change for the Baltic Sea Basin</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://hzg.academia.edu/HansvonStorch">Hans von Storch</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://gu-se.academia.edu/AndersOmstedt">Anders Omstedt</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/AnnaRutgersson">Anna Rutgersson</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/BirgitHuenicke">Birgit Huenicke</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://hzg.academia.edu/EduardoZorita">Eduardo Zorita</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/JyriElken">Jüri Elken</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/JanetPawlak">Janet Pawlak</a></span></div><div class="wp-workCard_item"><span> ISBN: 978-3-319-16005-4 (Print) 978-3-319-16006-1 (Online) </span><span>, Apr 15, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This book is an update of the first BACC assessment, published in 2008. It offers new and update...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This book is an update of the first BACC assessment, published in 2008. It offers new and updated scientific findings in regional climate research for the Baltic Sea basin. These include climate changes since the last glaciation (approx. 12,000 years ago), changes in the recent past (the last 200 years), climate projections up until 2100 using state-of-the-art regional climate models and an assessment of climate-change impacts on terrestrial, freshwater and marine ecosystems. There are dedicated new chapters on sea-level rise, coastal erosion and impacts on urban areas. A new set of chapters deals with possible causes of regional climate change along with the global effects of increased greenhouse gas concentrations, namely atmospheric aerosols and land-cover change. <br /> <br />The evidence collected and presented in this book shows that the regional climate has already started to change and this is expected to continue. Projections of potential future climates show that the region will probably become considerably warmer and wetter in some parts, but dryer in others. Terrestrial and aquatic ecosystems have already shown adjustments to increased temperatures and are expected to undergo further changes in the near future. <br /> <br />The BACC II Author Team consists of 141 scientists from 12 countries, covering various disciplines related to climate research and related impacts. BACC II is a project of the Baltic Earth research network and contributes to the World Climate Research Programme</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a45da2919fa64e5b389eb2321555614b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":37319734,"asset_id":11965332,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/37319734/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="11965332"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="11965332"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 11965332; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=11965332]").text(description); $(".js-view-count[data-work-id=11965332]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 11965332; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='11965332']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 11965332, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "a45da2919fa64e5b389eb2321555614b" } } $('.js-work-strip[data-work-id=11965332]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":11965332,"title":"Second Assessment of Climate Change for the Baltic Sea Basin","translated_title":"","metadata":{"abstract":"This book is an update of the first BACC assessment, published in 2008. It offers new and updated scientific findings in regional climate research for the Baltic Sea basin. These include climate changes since the last glaciation (approx. 12,000 years ago), changes in the recent past (the last 200 years), climate projections up until 2100 using state-of-the-art regional climate models and an assessment of climate-change impacts on terrestrial, freshwater and marine ecosystems. There are dedicated new chapters on sea-level rise, coastal erosion and impacts on urban areas. A new set of chapters deals with possible causes of regional climate change along with the global effects of increased greenhouse gas concentrations, namely atmospheric aerosols and land-cover change.\r\n\r\nThe evidence collected and presented in this book shows that the regional climate has already started to change and this is expected to continue. Projections of potential future climates show that the region will probably become considerably warmer and wetter in some parts, but dryer in others. Terrestrial and aquatic ecosystems have already shown adjustments to increased temperatures and are expected to undergo further changes in the near future.\r\n\r\nThe BACC II Author Team consists of 141 scientists from 12 countries, covering various disciplines related to climate research and related impacts. BACC II is a project of the Baltic Earth research network and contributes to the World Climate Research Programme","more_info":" The BACC II Author Team (Eds): Second Assessment of Climate Change for the Baltic Sea Basin","publisher":"Springer Verlag, Regional Climate Studies","publication_date":{"day":15,"month":4,"year":2015,"errors":{}},"publication_name":" ISBN: 978-3-319-16005-4 (Print) 978-3-319-16006-1 (Online) "},"translated_abstract":"This book is an update of the first BACC assessment, published in 2008. It offers new and updated scientific findings in regional climate research for the Baltic Sea basin. These include climate changes since the last glaciation (approx. 12,000 years ago), changes in the recent past (the last 200 years), climate projections up until 2100 using state-of-the-art regional climate models and an assessment of climate-change impacts on terrestrial, freshwater and marine ecosystems. There are dedicated new chapters on sea-level rise, coastal erosion and impacts on urban areas. A new set of chapters deals with possible causes of regional climate change along with the global effects of increased greenhouse gas concentrations, namely atmospheric aerosols and land-cover change.\r\n\r\nThe evidence collected and presented in this book shows that the regional climate has already started to change and this is expected to continue. Projections of potential future climates show that the region will probably become considerably warmer and wetter in some parts, but dryer in others. Terrestrial and aquatic ecosystems have already shown adjustments to increased temperatures and are expected to undergo further changes in the near future.\r\n\r\nThe BACC II Author Team consists of 141 scientists from 12 countries, covering various disciplines related to climate research and related impacts. BACC II is a project of the Baltic Earth research network and contributes to the World Climate Research Programme","internal_url":"https://www.academia.edu/11965332/Second_Assessment_of_Climate_Change_for_the_Baltic_Sea_Basin","translated_internal_url":"","created_at":"2015-04-15T19:22:30.539-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":329412,"coauthors_can_edit":true,"document_type":"book","co_author_tags":[{"id":6565368,"work_id":11965332,"tagging_user_id":11956707,"tagged_user_id":37046740,"co_author_invite_id":407401,"email":"e***m@smhi.se","affiliation":"Stockholm University","display_order":-5033164,"name":"Erik Kjellstr","title":"Second Assessment of Climate Change for the Baltic Sea Basin"},{"id":6565367,"work_id":11965332,"tagging_user_id":11956707,"tagged_user_id":31778669,"co_author_invite_id":null,"email":"o***c@dmi.dk","display_order":-1677721,"name":"O. Christensen","title":"Second Assessment of Climate Change for the Baltic Sea Basin"},{"id":421083,"work_id":11965332,"tagging_user_id":329412,"tagged_user_id":11956707,"co_author_invite_id":null,"email":"a***t@gvc.gu.se","affiliation":"University of Gothenburg","display_order":5033165,"name":"Anders Omstedt","title":"Second Assessment of Climate Change for the Baltic Sea Basin"},{"id":6565369,"work_id":11965332,"tagging_user_id":11956707,"tagged_user_id":35637326,"co_author_invite_id":530173,"email":"a***n@met.uu.se","display_order":6710886,"name":"Anna Rutgersson","title":"Second Assessment of Climate Change for the Baltic Sea Basin"},{"id":6565370,"work_id":11965332,"tagging_user_id":11956707,"tagged_user_id":null,"co_author_invite_id":1023304,"email":"z***o@uni.lodz.pl","display_order":7549747,"name":"Joanna Wibig","title":"Second Assessment of Climate Change for the Baltic Sea Basin"},{"id":6565371,"work_id":11965332,"tagging_user_id":11956707,"tagged_user_id":40471146,"co_author_invite_id":1461992,"email":"b***e@hzg.de","display_order":7969177,"name":"Birgit Huenicke","title":"Second Assessment of Climate Change for the Baltic Sea Basin"},{"id":6565372,"work_id":11965332,"tagging_user_id":11956707,"tagged_user_id":2710649,"co_author_invite_id":null,"email":"e***a@hzg.de","affiliation":"Helmholtz-Zentrum Geesthacht","display_order":8178892,"name":"Eduardo Zorita","title":"Second Assessment of Climate Change for the Baltic Sea Basin"},{"id":6565373,"work_id":11965332,"tagging_user_id":11956707,"tagged_user_id":88223014,"co_author_invite_id":1260392,"email":"i***n@mail.ru","affiliation":"State Hydrological Institute","display_order":8283750,"name":"Ирэна Борзенкова","title":"Second Assessment of Climate Change for the Baltic Sea Basin"},{"id":6565374,"work_id":11965332,"tagging_user_id":11956707,"tagged_user_id":34861195,"co_author_invite_id":null,"email":"o***a@gmail.com","display_order":8336179,"name":"Olga Borisova","title":"Second Assessment of Climate Change for the Baltic Sea Basin"},{"id":6565375,"work_id":11965332,"tagging_user_id":11956707,"tagged_user_id":137920247,"co_author_invite_id":90733,"email":"t***z@us.edu.pl","display_order":8362393,"name":"Tadeusz Niedźwiedź","title":"Second Assessment of Climate Change for the Baltic Sea Basin"},{"id":6565376,"work_id":11965332,"tagging_user_id":11956707,"tagged_user_id":43612352,"co_author_invite_id":1461993,"email":"j***n@msi.ttu.ee","display_order":8375500,"name":"Jüri Elken","title":"Second Assessment of Climate Change for the Baltic Sea Basin"},{"id":6565377,"work_id":11965332,"tagging_user_id":11956707,"tagged_user_id":null,"co_author_invite_id":458300,"email":"s***h@gkss.de","display_order":8382054,"name":"Hvon Storch","title":"Second Assessment of Climate Change for the Baltic Sea Basin"},{"id":13649099,"work_id":11965332,"tagging_user_id":11956707,"tagged_user_id":42325364,"co_author_invite_id":2824832,"email":"j***k@dahm.dk","display_order":8385331,"name":"Janet Pawlak","title":"Second Assessment of Climate Change for the Baltic Sea Basin"},{"id":13649112,"work_id":11965332,"tagging_user_id":11956707,"tagged_user_id":null,"co_author_invite_id":1450965,"email":"h***h@privat.dk","display_order":8386969,"name":"Hans Von Storch","title":"Second Assessment of Climate Change for the Baltic Sea Basin"},{"id":41712456,"work_id":11965332,"tagging_user_id":11956707,"tagged_user_id":32862499,"co_author_invite_id":null,"email":"m***l@lnu.se","affiliation":"Linnaeus University","display_order":1077935308,"name":"Marie-jose Gaillard-lemdahl","title":"Second Assessment of Climate Change for the Baltic Sea Basin"},{"id":41712457,"work_id":11965332,"tagging_user_id":11956707,"tagged_user_id":null,"co_author_invite_id":8151410,"email":"s***h@hcu-hamburg.de","display_order":1612709478,"name":"Sonja Deppisch","title":"Second Assessment of Climate Change for the Baltic Sea Basin"}],"downloadable_attachments":[{"id":37319734,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://a.academia-assets.com/images/blank-paper.jpg","file_name":"BACC-2.pdf","download_url":"https://www.academia.edu/attachments/37319734/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Second_Assessment_of_Climate_Change_for.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/37319734/BACC-2.pdf?1429153948=\u0026response-content-disposition=attachment%3B+filename%3DSecond_Assessment_of_Climate_Change_for.pdf\u0026Expires=1733881666\u0026Signature=Ajl~jPRe6QghFj3emc7uf0pEeplFZoSL5WFL~ZczXfcN146aMKtopGlQJtprxnptTuQ0XeZl2WKu2gcObWbvVZhXYZdHxalFu48pUwTIKASqVRgbTksuMhsNXWW~AEWv6v7Xj10ns-u4zZSg31pS7Oucl0Eef4kagwd3tG3YAHAX1z7JumlwNEGiRZ2d~i1V-8sXmd8feQ-AOF5t0dtu9Lh9mbR0IPpfHQNkRr3TrNIAR09weU11gKaNii0FTeqUUAju3OSvTX8NVTeHwUlGG0kdI7U4eSagJoMbyAwmuXkb1EgHEjQV9hCrlPKS2TjrYg1VCNPTawDXkr~HqXigqA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Second_Assessment_of_Climate_Change_for_the_Baltic_Sea_Basin","translated_slug":"","page_count":515,"language":"en","content_type":"Work","summary":"This book is an update of the first BACC assessment, published in 2008. It offers new and updated scientific findings in regional climate research for the Baltic Sea basin. These include climate changes since the last glaciation (approx. 12,000 years ago), changes in the recent past (the last 200 years), climate projections up until 2100 using state-of-the-art regional climate models and an assessment of climate-change impacts on terrestrial, freshwater and marine ecosystems. There are dedicated new chapters on sea-level rise, coastal erosion and impacts on urban areas. A new set of chapters deals with possible causes of regional climate change along with the global effects of increased greenhouse gas concentrations, namely atmospheric aerosols and land-cover change.\r\n\r\nThe evidence collected and presented in this book shows that the regional climate has already started to change and this is expected to continue. Projections of potential future climates show that the region will probably become considerably warmer and wetter in some parts, but dryer in others. Terrestrial and aquatic ecosystems have already shown adjustments to increased temperatures and are expected to undergo further changes in the near future.\r\n\r\nThe BACC II Author Team consists of 141 scientists from 12 countries, covering various disciplines related to climate research and related impacts. BACC II is a project of the Baltic Earth research network and contributes to the World Climate Research Programme","owner":{"id":329412,"first_name":"Hans","middle_initials":"","last_name":"von Storch","page_name":"HansvonStorch","domain_name":"hzg","created_at":"2011-02-11T04:04:39.946-08:00","display_name":"Hans von Storch","url":"https://hzg.academia.edu/HansvonStorch"},"attachments":[{"id":37319734,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://a.academia-assets.com/images/blank-paper.jpg","file_name":"BACC-2.pdf","download_url":"https://www.academia.edu/attachments/37319734/download_file?st=MTczNDExMTgzMCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Second_Assessment_of_Climate_Change_for.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/37319734/BACC-2.pdf?1429153948=\u0026response-content-disposition=attachment%3B+filename%3DSecond_Assessment_of_Climate_Change_for.pdf\u0026Expires=1733881666\u0026Signature=Ajl~jPRe6QghFj3emc7uf0pEeplFZoSL5WFL~ZczXfcN146aMKtopGlQJtprxnptTuQ0XeZl2WKu2gcObWbvVZhXYZdHxalFu48pUwTIKASqVRgbTksuMhsNXWW~AEWv6v7Xj10ns-u4zZSg31pS7Oucl0Eef4kagwd3tG3YAHAX1z7JumlwNEGiRZ2d~i1V-8sXmd8feQ-AOF5t0dtu9Lh9mbR0IPpfHQNkRr3TrNIAR09weU11gKaNii0FTeqUUAju3OSvTX8NVTeHwUlGG0kdI7U4eSagJoMbyAwmuXkb1EgHEjQV9hCrlPKS2TjrYg1VCNPTawDXkr~HqXigqA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":1512,"name":"Climate Change","url":"https://www.academia.edu/Documents/in/Climate_Change"},{"id":35801,"name":"Climate Change Impacts","url":"https://www.academia.edu/Documents/in/Climate_Change_Impacts"},{"id":276491,"name":"Baltic Sea region","url":"https://www.academia.edu/Documents/in/Baltic_Sea_region"}],"urls":[{"id":4679469,"url":"http://link.springer.com/content/pdf/10.1007%2F978-3-319-16006-1.pdf"},{"id":4679506,"url":"http://www.springer.com/de/book/9783319160054"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/google_contacts-0dfb882d836b94dbcb4a2d123d6933fc9533eda5be911641f20b4eb428429600.js"], function() { // from javascript_helper.rb $('.js-google-connect-button').click(function(e) { e.preventDefault(); GoogleContacts.authorize_and_show_contacts(); Aedu.Dismissibles.recordClickthrough("WowProfileImportContactsPrompt"); }); $('.js-update-biography-button').click(function(e) { e.preventDefault(); Aedu.Dismissibles.recordClickthrough("UpdateUserBiographyPrompt"); $.ajax({ url: $r.api_v0_profiles_update_about_path({ subdomain_param: 'api', about: "", }), type: 'PUT', success: function(response) { location.reload(); } }); }); $('.js-work-creator-button').click(function (e) { e.preventDefault(); window.location = $r.upload_funnel_document_path({ source: encodeURIComponent(""), }); }); $('.js-video-upload-button').click(function (e) { e.preventDefault(); window.location = $r.upload_funnel_video_path({ source: encodeURIComponent(""), }); }); $('.js-do-this-later-button').click(function() { $(this).closest('.js-profile-nag-panel').remove(); Aedu.Dismissibles.recordDismissal("WowProfileImportContactsPrompt"); }); $('.js-update-biography-do-this-later-button').click(function(){ $(this).closest('.js-profile-nag-panel').remove(); Aedu.Dismissibles.recordDismissal("UpdateUserBiographyPrompt"); }); $('.wow-profile-mentions-upsell--close').click(function(){ $('.wow-profile-mentions-upsell--panel').hide(); Aedu.Dismissibles.recordDismissal("WowProfileMentionsUpsell"); }); $('.wow-profile-mentions-upsell--button').click(function(){ Aedu.Dismissibles.recordClickthrough("WowProfileMentionsUpsell"); }); new WowProfile.SocialRedesignUserWorks({ initialWorksOffset: 20, allWorksOffset: 20, maxSections: 2 }) }); </script> </div></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile_edit-5ea339ee107c863779f560dd7275595239fed73f1a13d279d2b599a28c0ecd33.js","https://a.academia-assets.com/assets/add_coauthor-22174b608f9cb871d03443cafa7feac496fb50d7df2d66a53f5ee3c04ba67f53.js","https://a.academia-assets.com/assets/tab-dcac0130902f0cc2d8cb403714dd47454f11fc6fb0e99ae6a0827b06613abc20.js","https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js"], function() { // from javascript_helper.rb window.ae = window.ae || {}; window.ae.WowProfile = window.ae.WowProfile || {}; if(Aedu.User.current && Aedu.User.current.id === $viewedUser.id) { window.ae.WowProfile.current_user_edit = {}; new WowProfileEdit.EditUploadView({ el: '.js-edit-upload-button-wrapper', model: window.$current_user, }); new AddCoauthor.AddCoauthorsController(); } var userInfoView = new WowProfile.SocialRedesignUserInfo({ recaptcha_key: "6LdxlRMTAAAAADnu_zyLhLg0YF9uACwz78shpjJB" }); WowProfile.router = new WowProfile.Router({ userInfoView: userInfoView }); Backbone.history.start({ pushState: true, root: "/" + $viewedUser.page_name }); new WowProfile.UserWorksNav() }); </script> </div> <div class="bootstrap login"><div class="modal fade login-modal" id="login-modal"><div class="login-modal-dialog modal-dialog"><div class="modal-content"><div class="modal-header"><button class="close close" data-dismiss="modal" type="button"><span aria-hidden="true">×</span><span class="sr-only">Close</span></button><h4 class="modal-title text-center"><strong>Log In</strong></h4></div><div class="modal-body"><div class="row"><div class="col-xs-10 col-xs-offset-1"><button class="btn btn-fb btn-lg btn-block btn-v-center-content" id="login-facebook-oauth-button"><svg style="float: left; width: 19px; line-height: 1em; margin-right: .3em;" aria-hidden="true" focusable="false" data-prefix="fab" data-icon="facebook-square" class="svg-inline--fa fa-facebook-square fa-w-14" role="img" xmlns="http://www.w3.org/2000/svg" viewBox="0 0 448 512"><path fill="currentColor" d="M400 32H48A48 48 0 0 0 0 80v352a48 48 0 0 0 48 48h137.25V327.69h-63V256h63v-54.64c0-62.15 37-96.48 93.67-96.48 27.14 0 55.52 4.84 55.52 4.84v61h-31.27c-30.81 0-40.42 19.12-40.42 38.73V256h68.78l-11 71.69h-57.78V480H400a48 48 0 0 0 48-48V80a48 48 0 0 0-48-48z"></path></svg><small><strong>Log in</strong> with <strong>Facebook</strong></small></button><br /><button class="btn btn-google btn-lg btn-block btn-v-center-content" id="login-google-oauth-button"><svg style="float: left; width: 22px; line-height: 1em; margin-right: .3em;" aria-hidden="true" focusable="false" data-prefix="fab" data-icon="google-plus" class="svg-inline--fa fa-google-plus fa-w-16" role="img" xmlns="http://www.w3.org/2000/svg" viewBox="0 0 512 512"><path fill="currentColor" d="M256,8C119.1,8,8,119.1,8,256S119.1,504,256,504,504,392.9,504,256,392.9,8,256,8ZM185.3,380a124,124,0,0,1,0-248c31.3,0,60.1,11,83,32.3l-33.6,32.6c-13.2-12.9-31.3-19.1-49.4-19.1-42.9,0-77.2,35.5-77.2,78.1S142.3,334,185.3,334c32.6,0,64.9-19.1,70.1-53.3H185.3V238.1H302.2a109.2,109.2,0,0,1,1.9,20.7c0,70.8-47.5,121.2-118.8,121.2ZM415.5,273.8v35.5H380V273.8H344.5V238.3H380V202.8h35.5v35.5h35.2v35.5Z"></path></svg><small><strong>Log in</strong> with <strong>Google</strong></small></button><br /><style type="text/css">.sign-in-with-apple-button { width: 100%; height: 52px; border-radius: 3px; border: 1px solid black; cursor: pointer; }</style><script src="https://appleid.cdn-apple.com/appleauth/static/jsapi/appleid/1/en_US/appleid.auth.js" type="text/javascript"></script><div class="sign-in-with-apple-button" data-border="false" data-color="white" id="appleid-signin"><span   ="Sign Up with Apple" class="u-fs11"></span></div><script>AppleID.auth.init({ clientId: 'edu.academia.applesignon', scope: 'name email', redirectURI: 'https://www.academia.edu/sessions', state: "3119cc978f6b8a885250379bf684ddef1660f97f55ab1f60415f7d421a61506b", });</script><script>// Hacky way of checking if on fast loswp if (window.loswp == null) { (function() { const Google = window?.Aedu?.Auth?.OauthButton?.Login?.Google; const Facebook = window?.Aedu?.Auth?.OauthButton?.Login?.Facebook; if (Google) { new Google({ el: '#login-google-oauth-button', rememberMeCheckboxId: 'remember_me', track: null }); } if (Facebook) { new Facebook({ el: '#login-facebook-oauth-button', rememberMeCheckboxId: 'remember_me', track: null }); } })(); }</script></div></div></div><div class="modal-body"><div class="row"><div class="col-xs-10 col-xs-offset-1"><div class="hr-heading login-hr-heading"><span class="hr-heading-text">or</span></div></div></div></div><div class="modal-body"><div class="row"><div class="col-xs-10 col-xs-offset-1"><form class="js-login-form" action="https://www.academia.edu/sessions" accept-charset="UTF-8" method="post"><input name="utf8" type="hidden" value="✓" autocomplete="off" /><input type="hidden" name="authenticity_token" value="xWWXdfgmrB9P5tYYI5BTYzvMACN8thyyRkGWND4PKmq98FeHcOCr0o2urvFKz5O1qLTToKycDBt8zBlBjT6OOg==" autocomplete="off" /><div class="form-group"><label class="control-label" for="login-modal-email-input" style="font-size: 14px;">Email</label><input class="form-control" id="login-modal-email-input" name="login" type="email" /></div><div class="form-group"><label class="control-label" for="login-modal-password-input" style="font-size: 14px;">Password</label><input class="form-control" id="login-modal-password-input" name="password" type="password" /></div><input type="hidden" name="post_login_redirect_url" id="post_login_redirect_url" value="https://gu-se.academia.edu/AndersOmstedt" autocomplete="off" /><div class="checkbox"><label><input type="checkbox" name="remember_me" id="remember_me" value="1" checked="checked" /><small style="font-size: 12px; margin-top: 2px; display: inline-block;">Remember me on this computer</small></label></div><br><input type="submit" name="commit" value="Log In" class="btn btn-primary btn-block btn-lg js-login-submit" data-disable-with="Log In" /></br></form><script>typeof window?.Aedu?.recaptchaManagedForm === 'function' && window.Aedu.recaptchaManagedForm( document.querySelector('.js-login-form'), document.querySelector('.js-login-submit') );</script><small style="font-size: 12px;"><br />or <a data-target="#login-modal-reset-password-container" data-toggle="collapse" href="javascript:void(0)">reset password</a></small><div class="collapse" id="login-modal-reset-password-container"><br /><div class="well margin-0x"><form class="js-password-reset-form" action="https://www.academia.edu/reset_password" accept-charset="UTF-8" method="post"><input name="utf8" type="hidden" value="✓" autocomplete="off" /><input type="hidden" name="authenticity_token" value="hFojboYr35MBpbrriT1ghhHsK6bR5VEP4nrWj8WSiNH8z+OcDu3YXsPtwgLgYqBQgpT4JQHPQabY91n6dqMsgQ==" autocomplete="off" /><p>Enter the email address you signed up with and we'll email you a reset link.</p><div class="form-group"><input class="form-control" name="email" type="email" /></div><script src="https://recaptcha.net/recaptcha/api.js" async defer></script> <script> var invisibleRecaptchaSubmit = function () { var closestForm = function (ele) { var curEle = ele.parentNode; while (curEle.nodeName !== 'FORM' && curEle.nodeName !== 'BODY'){ curEle = curEle.parentNode; } return curEle.nodeName === 'FORM' ? curEle : null }; var eles = document.getElementsByClassName('g-recaptcha'); if (eles.length > 0) { var form = closestForm(eles[0]); if (form) { form.submit(); } } }; </script> <input type="submit" data-sitekey="6Lf3KHUUAAAAACggoMpmGJdQDtiyrjVlvGJ6BbAj" data-callback="invisibleRecaptchaSubmit" class="g-recaptcha btn btn-primary btn-block" value="Email me a link" value=""/> </form></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/collapse-45805421cf446ca5adf7aaa1935b08a3a8d1d9a6cc5d91a62a2a3a00b20b3e6a.js"], function() { // from javascript_helper.rb $("#login-modal-reset-password-container").on("shown.bs.collapse", function() { $(this).find("input[type=email]").focus(); }); }); </script> </div></div></div><div class="modal-footer"><div class="text-center"><small style="font-size: 12px;">Need an account? <a rel="nofollow" href="https://www.academia.edu/signup">Click here to sign up</a></small></div></div></div></div></div></div><script>// If we are on subdomain or non-bootstrapped page, redirect to login page instead of showing modal (function(){ if (typeof $ === 'undefined') return; var host = window.location.hostname; if ((host === $domain || host === "www."+$domain) && (typeof $().modal === 'function')) { $("#nav_log_in").click(function(e) { // Don't follow the link and open the modal e.preventDefault(); $("#login-modal").on('shown.bs.modal', function() { $(this).find("#login-modal-email-input").focus() }).modal('show'); }); } })()</script> <div class="bootstrap" id="footer"><div class="footer-content clearfix text-center padding-top-7x" style="width:100%;"><ul class="footer-links-secondary footer-links-wide list-inline margin-bottom-1x"><li><a href="https://www.academia.edu/about">About</a></li><li><a href="https://www.academia.edu/press">Press</a></li><li><a href="https://www.academia.edu/documents">Papers</a></li><li><a href="https://www.academia.edu/topics">Topics</a></li><li><a href="https://www.academia.edu/journals">Academia.edu Journals</a></li><li><a rel="nofollow" href="https://www.academia.edu/hiring"><svg style="width: 13px; height: 13px;" aria-hidden="true" focusable="false" data-prefix="fas" data-icon="briefcase" class="svg-inline--fa fa-briefcase fa-w-16" role="img" xmlns="http://www.w3.org/2000/svg" viewBox="0 0 512 512"><path fill="currentColor" d="M320 336c0 8.84-7.16 16-16 16h-96c-8.84 0-16-7.16-16-16v-48H0v144c0 25.6 22.4 48 48 48h416c25.6 0 48-22.4 48-48V288H320v48zm144-208h-80V80c0-25.6-22.4-48-48-48H176c-25.6 0-48 22.4-48 48v48H48c-25.6 0-48 22.4-48 48v80h512v-80c0-25.6-22.4-48-48-48zm-144 0H192V96h128v32z"></path></svg> <strong>We're Hiring!</strong></a></li><li><a rel="nofollow" href="https://support.academia.edu/"><svg style="width: 12px; height: 12px;" aria-hidden="true" focusable="false" data-prefix="fas" data-icon="question-circle" class="svg-inline--fa fa-question-circle fa-w-16" role="img" xmlns="http://www.w3.org/2000/svg" viewBox="0 0 512 512"><path fill="currentColor" d="M504 256c0 136.997-111.043 248-248 248S8 392.997 8 256C8 119.083 119.043 8 256 8s248 111.083 248 248zM262.655 90c-54.497 0-89.255 22.957-116.549 63.758-3.536 5.286-2.353 12.415 2.715 16.258l34.699 26.31c5.205 3.947 12.621 3.008 16.665-2.122 17.864-22.658 30.113-35.797 57.303-35.797 20.429 0 45.698 13.148 45.698 32.958 0 14.976-12.363 22.667-32.534 33.976C247.128 238.528 216 254.941 216 296v4c0 6.627 5.373 12 12 12h56c6.627 0 12-5.373 12-12v-1.333c0-28.462 83.186-29.647 83.186-106.667 0-58.002-60.165-102-116.531-102zM256 338c-25.365 0-46 20.635-46 46 0 25.364 20.635 46 46 46s46-20.636 46-46c0-25.365-20.635-46-46-46z"></path></svg> <strong>Help Center</strong></a></li></ul><ul class="footer-links-tertiary list-inline margin-bottom-1x"><li class="small">Find new research papers in:</li><li class="small"><a href="https://www.academia.edu/Documents/in/Physics">Physics</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Chemistry">Chemistry</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Biology">Biology</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Health_Sciences">Health Sciences</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Ecology">Ecology</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Earth_Sciences">Earth Sciences</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Cognitive_Science">Cognitive Science</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Mathematics">Mathematics</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Computer_Science">Computer Science</a></li></ul></div></div><div class="DesignSystem" id="credit" style="width:100%;"><ul class="u-pl0x footer-links-legal list-inline"><li><a rel="nofollow" href="https://www.academia.edu/terms">Terms</a></li><li><a rel="nofollow" href="https://www.academia.edu/privacy">Privacy</a></li><li><a rel="nofollow" href="https://www.academia.edu/copyright">Copyright</a></li><li>Academia ©2024</li></ul></div><script> //<![CDATA[ window.detect_gmtoffset = true; window.Academia && window.Academia.set_gmtoffset && Academia.set_gmtoffset('/gmtoffset'); //]]> </script> <div id='overlay_background'></div> <div id='bootstrap-modal-container' class='bootstrap'></div> <div id='ds-modal-container' class='bootstrap DesignSystem'></div> <div id='full-screen-modal'></div> </div> </body> </html>