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Hales</h1><div class="affiliations-container fake-truncate js-profile-affiliations"></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="B." data-follow-user-id="39578631" 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="39578631"><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 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src="https://0.academia-photos.com/610926/214174/475853/s200_olaf.j_ris.jpg" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://leiza.academia.edu/OlafJ%C3%B6ris">Olaf J枚ris</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">Leibniz-Zentrum f眉r Arch盲ologie</p></div></div><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a data-nosnippet="" href="https://nrm.academia.edu/SMcLoughlin"><img class="profile-avatar u-positionAbsolute" alt="Stephen McLoughlin related author profile picture" 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/872101/314429/20008173/s200_stephen.mcloughlin.jpg" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://nrm.academia.edu/SMcLoughlin">Stephen McLoughlin</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">Swedish Museum of Natural History</p></div></div><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a data-nosnippet="" href="https://unimelb.academia.edu/KaleSniderman"><img class="profile-avatar u-positionAbsolute" alt="Kale Sniderman related author profile picture" 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/1195054/431811/534568/s200_kale.sniderman.jpg" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://unimelb.academia.edu/KaleSniderman">Kale Sniderman</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">University of Melbourne</p></div></div><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a data-nosnippet="" href="https://aberdeen.academia.edu/WilliamMills"><img class="profile-avatar u-positionAbsolute" alt="William Mills related author profile picture" 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/1209516/435603/55143309/s200_william.mills.jpeg" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://aberdeen.academia.edu/WilliamMills">William Mills</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">University of Aberdeen</p></div></div><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a data-nosnippet="" href="https://uftm.academia.edu/AgustinMartinelli"><img class="profile-avatar u-positionAbsolute" alt="Agustin Martinelli related author profile picture" 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/1548291/798400/993634/s200_agustin.martinelli.jpg" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://uftm.academia.edu/AgustinMartinelli">Agustin Martinelli</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">Universidade Federal do Tri芒ngulo Mineiro (UFTM)</p></div></div><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a data-nosnippet="" href="https://illinois.academia.edu/KiranDasari"><img class="profile-avatar u-positionAbsolute" alt="Kiran Dasari related author profile picture" 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/1693440/585320/3191167/s200_kiran.dasari.jpg" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://illinois.academia.edu/KiranDasari">Kiran Dasari</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">University of Illinois at Urbana-Champaign</p></div></div><div class="suggested-user-card"><div class="suggested-user-card__avatar social-profile-avatar-container"><a data-nosnippet="" href="https://smu-ca.academia.edu/jaroslavdostal"><img class="profile-avatar u-positionAbsolute" alt="jaroslav dostal related author profile picture" 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/22026531/6022604/19329172/s200_jaroslav.dostal.jpg" /></a></div><div class="suggested-user-card__user-info"><a class="suggested-user-card__user-info__header ds2-5-body-sm-bold ds2-5-body-link" href="https://smu-ca.academia.edu/jaroslavdostal">jaroslav dostal</a><p class="suggested-user-card__user-info__subheader ds2-5-body-xs">Saint Mary's University (Canada)</p></div></div></ul></div><style type="text/css">.suggested-academics--header h3{font-size:16px;font-weight:500;line-height:20px}</style><div class="ri-section"><div class="ri-section-header"><span>Interests</span></div><div class="ri-tags-container"><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="39578631" href="https://www.academia.edu/Documents/in/Rare_Earth_Elements"><div id="js-react-on-rails-context" style="display:none" data-rails-context="{"inMailer":false,"i18nLocale":"en","i18nDefaultLocale":"en","href":"https://independent.academia.edu/HalesB","location":"/HalesB","scheme":"https","host":"independent.academia.edu","port":null,"pathname":"/HalesB","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":["Rare Earth Elements"]}" data-trace="false" data-dom-id="Pill-react-component-83dca702-ffdf-4e88-810d-1bcd59f0d2b9"></div> <div id="Pill-react-component-83dca702-ffdf-4e88-810d-1bcd59f0d2b9"></div> </a></div></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="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 B. Hales</h3></div><div class="js-work-strip profile--work_container" data-work-id="122803781"><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/122803781/SUCCES3_cruise_biogeochemical_dataset_1_SuperSucker_data_ammonium_and_nitrate_nitrite"><img alt="Research paper thumbnail of SUCCES3 cruise biogeochemical dataset (1): SuperSucker data, ammonium and nitrate+nitrite" 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">SUCCES3 cruise biogeochemical dataset (1): SuperSucker data, ammonium and nitrate+nitrite</div><div class="wp-workCard_item"><span>Zenodo (CERN European Organization for Nuclear Research)</span><span>, Oct 14, 2022</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="122803781"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="122803781"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 122803781; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=122803781]").text(description); $(".js-view-count[data-work-id=122803781]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 122803781; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='122803781']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=122803781]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":122803781,"title":"SUCCES3 cruise biogeochemical dataset (1): SuperSucker data, ammonium and nitrate+nitrite","translated_title":"","metadata":{"publication_date":{"day":14,"month":10,"year":2022,"errors":{}},"publication_name":"Zenodo (CERN European Organization for Nuclear Research)"},"translated_abstract":null,"internal_url":"https://www.academia.edu/122803781/SUCCES3_cruise_biogeochemical_dataset_1_SuperSucker_data_ammonium_and_nitrate_nitrite","translated_internal_url":"","created_at":"2024-08-12T06:13:10.198-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":39578631,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"SUCCES3_cruise_biogeochemical_dataset_1_SuperSucker_data_ammonium_and_nitrate_nitrite","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":null,"owner":{"id":39578631,"first_name":"B.","middle_initials":null,"last_name":"Hales","page_name":"HalesB","domain_name":"independent","created_at":"2015-12-01T15:04:35.113-08:00","display_name":"B. Hales","url":"https://independent.academia.edu/HalesB"},"attachments":[],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":122404,"name":"Nitrate","url":"https://www.academia.edu/Documents/in/Nitrate"},{"id":162978,"name":"Nitrite","url":"https://www.academia.edu/Documents/in/Nitrite"},{"id":545968,"name":"Cruise","url":"https://www.academia.edu/Documents/in/Cruise"},{"id":4023440,"name":"Biogeochemical Cycle","url":"https://www.academia.edu/Documents/in/Biogeochemical_Cycle"}],"urls":[{"id":43960702,"url":"https://zenodo.org/record/7198113"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-122803781-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="122803764"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/122803764/Feedbacks_Between_Estuarine_Metabolism_and_Anthropogenic_CO_sub_2_sub_Accelerate_Local_Rates_of_Ocean_Acidification_and_Hasten_Threshold_Exceedances"><img alt="Research paper thumbnail of Feedbacks Between Estuarine Metabolism and Anthropogenic CO<sub>2</sub> Accelerate Local Rates of Ocean Acidification and Hasten Threshold Exceedances" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title">Feedbacks Between Estuarine Metabolism and Anthropogenic CO<sub>2</sub> Accelerate Local Rates of Ocean Acidification and Hasten Threshold Exceedances</div><div class="wp-workCard_item"><span>Journal of geophysical research. Oceans</span><span>, Feb 27, 2024</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="122803764"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="122803764"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 122803764; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=122803764]").text(description); $(".js-view-count[data-work-id=122803764]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 122803764; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='122803764']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=122803764]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":122803764,"title":"Feedbacks Between Estuarine Metabolism and Anthropogenic CO\u003csub\u003e2\u003c/sub\u003e Accelerate Local Rates of Ocean Acidification and Hasten Threshold Exceedances","translated_title":"","metadata":{"publication_date":{"day":27,"month":2,"year":2024,"errors":{}},"publication_name":"Journal of geophysical research. Oceans"},"translated_abstract":null,"internal_url":"https://www.academia.edu/122803764/Feedbacks_Between_Estuarine_Metabolism_and_Anthropogenic_CO_sub_2_sub_Accelerate_Local_Rates_of_Ocean_Acidification_and_Hasten_Threshold_Exceedances","translated_internal_url":"","created_at":"2024-08-12T06:12:48.241-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":39578631,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Feedbacks_Between_Estuarine_Metabolism_and_Anthropogenic_CO_sub_2_sub_Accelerate_Local_Rates_of_Ocean_Acidification_and_Hasten_Threshold_Exceedances","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":null,"owner":{"id":39578631,"first_name":"B.","middle_initials":null,"last_name":"Hales","page_name":"HalesB","domain_name":"independent","created_at":"2015-12-01T15:04:35.113-08:00","display_name":"B. Hales","url":"https://independent.academia.edu/HalesB"},"attachments":[],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":68527,"name":"Ocean acidification","url":"https://www.academia.edu/Documents/in/Ocean_acidification"},{"id":379570,"name":"Estuary","url":"https://www.academia.edu/Documents/in/Estuary"}],"urls":[{"id":43960690,"url":"https://doi.org/10.1029/2023jc020313"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-122803764-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="113018629"><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/113018629/Seagrass_habitat_metabolism_increases_short_term_extremes_and_long_term_offset_of_CO_sub_2_sub_under_future_ocean_acidification"><img alt="Research paper thumbnail of Seagrass habitat metabolism increases short-term extremes and long-term offset of CO <sub>2</sub> under future ocean acidification" class="work-thumbnail" src="https://attachments.academia-assets.com/110091833/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/113018629/Seagrass_habitat_metabolism_increases_short_term_extremes_and_long_term_offset_of_CO_sub_2_sub_under_future_ocean_acidification">Seagrass habitat metabolism increases short-term extremes and long-term offset of CO <sub>2</sub> under future ocean acidification</a></div><div class="wp-workCard_item"><span>Proceedings of the National Academy of Sciences of the United States of America</span><span>, Apr 2, 2018</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="84f6c4091cb6276fafe4c741cbf03256" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":110091833,"asset_id":113018629,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/110091833/download_file?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="113018629"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="113018629"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 113018629; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=113018629]").text(description); $(".js-view-count[data-work-id=113018629]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 113018629; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='113018629']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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); 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However, during bloom and post鈥恇loom conditions large ammonium concentrations and uptake rates have been described. High鈥恌requency on board nitrate聽+聽nitrite and ammonium analysis synchronized with continuous data from a towed profiling vehicle (equipped with in situ temperature, salinity, dissolved oxygen, and beam attenuation sensors), allowed us to describe coupled high鈥恟esolution physico鈥恈hemical dynamics of inorganic nitrogen in seven cross鈥恠helf transects, over several days, during an active phytoplankton bloom following cessation of upwelling favorable winds. We present first鈥恛f鈥恡heir鈥恔ind high鈥恟esolution cross鈥恠ections showing a build鈥恥p, both within a thin plume of onshore鈥恛riginated water, and in mid鈥恡o鈥恇ottom on鈥恠hore water columns, from undetectable values to up to 8聽碌M of ammonium. The plume ext...</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="108397013"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397013"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397013; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108397013]").text(description); $(".js-view-count[data-work-id=108397013]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108397013; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108397013']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=108397013]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108397013,"title":"Short Time鈥怱cale Variability of Ammonium, Nitrate, and Nitrogen Loss Dynamics During an Upwelling鈥怚nduced Bloom at the Oregon Shelf","translated_title":"","metadata":{"abstract":"Ammonium, a key intermediate nutrient, is typically low to undetectable on the Oregon coast, particularly as active upwelling delivers high onshore flow of ammonium鈥恜oor waters. However, during bloom and post鈥恇loom conditions large ammonium concentrations and uptake rates have been described. High鈥恌requency on board nitrate聽+聽nitrite and ammonium analysis synchronized with continuous data from a towed profiling vehicle (equipped with in situ temperature, salinity, dissolved oxygen, and beam attenuation sensors), allowed us to describe coupled high鈥恟esolution physico鈥恈hemical dynamics of inorganic nitrogen in seven cross鈥恠helf transects, over several days, during an active phytoplankton bloom following cessation of upwelling favorable winds. We present first鈥恛f鈥恡heir鈥恔ind high鈥恟esolution cross鈥恠ections showing a build鈥恥p, both within a thin plume of onshore鈥恛riginated water, and in mid鈥恡o鈥恇ottom on鈥恠hore water columns, from undetectable values to up to 8聽碌M of ammonium. The plume ext...","publisher":"American Geophysical Union (AGU)","publication_name":"Journal of Geophysical Research: Oceans"},"translated_abstract":"Ammonium, a key intermediate nutrient, is typically low to undetectable on the Oregon coast, particularly as active upwelling delivers high onshore flow of ammonium鈥恜oor waters. However, during bloom and post鈥恇loom conditions large ammonium concentrations and uptake rates have been described. High鈥恌requency on board nitrate聽+聽nitrite and ammonium analysis synchronized with continuous data from a towed profiling vehicle (equipped with in situ temperature, salinity, dissolved oxygen, and beam attenuation sensors), allowed us to describe coupled high鈥恟esolution physico鈥恈hemical dynamics of inorganic nitrogen in seven cross鈥恠helf transects, over several days, during an active phytoplankton bloom following cessation of upwelling favorable winds. We present first鈥恛f鈥恡heir鈥恔ind high鈥恟esolution cross鈥恠ections showing a build鈥恥p, both within a thin plume of onshore鈥恛riginated water, and in mid鈥恡o鈥恇ottom on鈥恠hore water columns, from undetectable values to up to 8聽碌M of ammonium. The plume ext...","internal_url":"https://www.academia.edu/108397013/Short_Time_Scale_Variability_of_Ammonium_Nitrate_and_Nitrogen_Loss_Dynamics_During_an_Upwelling_Induced_Bloom_at_the_Oregon_Shelf","translated_internal_url":"","created_at":"2023-10-20T13:10:04.849-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":39578631,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Short_Time_Scale_Variability_of_Ammonium_Nitrate_and_Nitrogen_Loss_Dynamics_During_an_Upwelling_Induced_Bloom_at_the_Oregon_Shelf","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Ammonium, a key intermediate nutrient, is typically low to undetectable on the Oregon coast, particularly as active upwelling delivers high onshore flow of ammonium鈥恜oor waters. However, during bloom and post鈥恇loom conditions large ammonium concentrations and uptake rates have been described. High鈥恌requency on board nitrate聽+聽nitrite and ammonium analysis synchronized with continuous data from a towed profiling vehicle (equipped with in situ temperature, salinity, dissolved oxygen, and beam attenuation sensors), allowed us to describe coupled high鈥恟esolution physico鈥恈hemical dynamics of inorganic nitrogen in seven cross鈥恠helf transects, over several days, during an active phytoplankton bloom following cessation of upwelling favorable winds. We present first鈥恛f鈥恡heir鈥恔ind high鈥恟esolution cross鈥恠ections showing a build鈥恥p, both within a thin plume of onshore鈥恛riginated water, and in mid鈥恡o鈥恇ottom on鈥恠hore water columns, from undetectable values to up to 8聽碌M of ammonium. The plume ext...","owner":{"id":39578631,"first_name":"B.","middle_initials":null,"last_name":"Hales","page_name":"HalesB","domain_name":"independent","created_at":"2015-12-01T15:04:35.113-08:00","display_name":"B. 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As such, they are an initiation point for both planning and implementation activities. However, existing water quality criteria, which were created four decades ago, are not scientifically appropriate for assessing OA conditions. Even when existing water quality criteria for seawater pH are met, a wide range of severe biological impacts of OA are observed. New criteria are needed. The Panel further recommends that OA water quality criteria be expanded to include other acidification parameters, as pH is only one of several possible parameters for describing the carbonate system. One such alternative, aragonite saturation state, has been found to be biologically relevant to a number of calcifying organisms. Appendix G provides additional insight about the need for revised water quality criteria.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="52ffe52a7e10a42f2957427d939f4072" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":106792226,"asset_id":108397012,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/106792226/download_file?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="108397012"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397012"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397012; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108397012]").text(description); $(".js-view-count[data-work-id=108397012]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108397012; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108397012']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "52ffe52a7e10a42f2957427d939f4072" } } $('.js-work-strip[data-work-id=108397012]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108397012,"title":"The West Coast Ocean Acidification and Hypoxia Science Panel: Major Findings, Recommendations and Actions","translated_title":"","metadata":{"ai_title_tag":"Revamping Water Quality Criteria for Ocean Acidification","grobid_abstract":"Water quality criteria serve as the foundation for many management activities, providing managers with thresholds to objectively determine the condition of a water body and to set targets for clean-up efforts. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-108397008-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="108397007"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/108397007/Air_water_CO2_Fluxes_and_Inorganic_Carbon_Dynamics_in_a_Microtidal_Eutrophic_Estuary"><img alt="Research paper thumbnail of Air-water CO2 Fluxes and Inorganic Carbon Dynamics in a Microtidal, Eutrophic Estuary" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title">Air-water CO2 Fluxes and Inorganic Carbon Dynamics in a Microtidal, Eutrophic Estuary</div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">ABSTRACT</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="108397007"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397007"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397007; 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However, in the past these measurements have been somewhat restricted due to the time-intensive nature of the sample collection and manual filtration procedures. To increase temporal and spatial coverage of POC distributions, we designed and built a semi-automated filtration</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="108397006"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397006"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397006; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108397006]").text(description); $(".js-view-count[data-work-id=108397006]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108397006; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108397006']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=108397006]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108397006,"title":"Distribution and Composition of Particulate Organic Carbon along Oregon's Upwelling Zone","translated_title":"","metadata":{"abstract":"Direct measurements of particulate organic carbon (POC) concentrations are needed to quantitatively understand the carbon cycle in Eastern Boundary ocean margins. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-108397006-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="108397005"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/108397005/An_update_to_the_Surface_Ocean_CO2_Atlas_SOCAT_"><img alt="Research paper thumbnail of An update to the Surface Ocean CO2 Atlas (SOCAT)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title">An update to the Surface Ocean CO2 Atlas (SOCAT)</div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="108397005"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397005"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397005; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108397005]").text(description); $(".js-view-count[data-work-id=108397005]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108397005; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108397005']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=108397005]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108397005,"title":"An update to the Surface Ocean CO2 Atlas (SOCAT)","translated_title":"","metadata":{},"translated_abstract":null,"internal_url":"https://www.academia.edu/108397005/An_update_to_the_Surface_Ocean_CO2_Atlas_SOCAT_","translated_internal_url":"","created_at":"2023-10-20T13:10:02.655-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":39578631,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"An_update_to_the_Surface_Ocean_CO2_Atlas_SOCAT_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":null,"owner":{"id":39578631,"first_name":"B.","middle_initials":null,"last_name":"Hales","page_name":"HalesB","domain_name":"independent","created_at":"2015-12-01T15:04:35.113-08:00","display_name":"B. 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This system has proved to be a sink of CO2 to deep waters via POC export during the relaxation of the alongshore winds (Hales et al., 2006). On May 2009, during one of those upwelling events, we performed a deliberate tracer injection experiment at the bottom boundary layer (BBL, sigma-t &amp;gt; 26.5) off the Oregon coast. The tracer consisted in a dye/SF6 mixture. After the injection of the tracer the nutrients, carbonate and dissolved oxygen chemistry, as well as in situ hydrography (S, T, bio-optics), of the BBL was measured using a high-frequency profiling system. The tracer was followed for 5 days, during which the water moved towards the coast, according to an upwelling process. SF6 sensitivity allowed us to definitively identify waters that were out of the patch. The main modifications in the chemical properties of the water traced were found nearshore, showing signs of respiration, while there was an apparent decoupling of nitrate from these signals.</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="108397004"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397004"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397004; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108397004]").text(description); $(".js-view-count[data-work-id=108397004]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108397004; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108397004']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=108397004]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108397004,"title":"Changes in the Chemical Composition of the Bottom Boundary Layer during AN Upwelling Event at the Oregon Coast","translated_title":"","metadata":{"abstract":"ABSTRACT On the Oregon coast shelf, prevailing summer winds blow alongshore, mainly favoring the upwelling of nutrient-rich dense offshore water, which triggers a phytoplankton bloom. 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The tracer was followed for 5 days, during which the water moved towards the coast, according to an upwelling process. SF6 sensitivity allowed us to definitively identify waters that were out of the patch. The main modifications in the chemical properties of the water traced were found nearshore, showing signs of respiration, while there was an apparent decoupling of nitrate from these signals.","internal_url":"https://www.academia.edu/108397004/Changes_in_the_Chemical_Composition_of_the_Bottom_Boundary_Layer_during_AN_Upwelling_Event_at_the_Oregon_Coast","translated_internal_url":"","created_at":"2023-10-20T13:10:02.530-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":39578631,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Changes_in_the_Chemical_Composition_of_the_Bottom_Boundary_Layer_during_AN_Upwelling_Event_at_the_Oregon_Coast","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"ABSTRACT On the Oregon coast shelf, prevailing summer winds blow alongshore, mainly favoring the upwelling of nutrient-rich dense offshore water, which triggers a phytoplankton bloom. 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In particular, the change in saturation state (Omega) of calcium carbonate minerals calcite and aragonite may be energetically unfavorable for shell formation while favoring shell dissolution. Eastern boundary upwelling systems may provide</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="108397003"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397003"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397003; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108397003]").text(description); $(".js-view-count[data-work-id=108397003]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108397003; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108397003']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=108397003]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108397003,"title":"Inorganic carbon dynamics in the upwelling system off the Oregon coast and implications for commercial shellfish hatcheries","translated_title":"","metadata":{"abstract":"The increasing absorption of anthropogenic CO2 by the global ocean and concomitant decrease in pH will alter seawater carbonate chemistry in ways that may negatively impact calcifying organisms. 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The western Canadian shelf is no exception to this, and it is thought to be part of an important high latitude sink region for atmospheric CO2, balancing lower latitude source regions</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="108397002"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397002"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397002; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108397002]").text(description); $(".js-view-count[data-work-id=108397002]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108397002; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108397002']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=108397002]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108397002,"title":"pCO2 Dynamics on the Western Canadian Coastal Margin","translated_title":"","metadata":{"abstract":"There is large uncertainty in sea-air CO2 fluxes from coastal margins due to sparse data sets that inadequately resolve the extreme temporal and spatial variability inherent in these regions. 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The western Canadian shelf is no exception to this, and it is thought to be part of an important high latitude sink region for atmospheric CO2, balancing lower latitude source regions","internal_url":"https://www.academia.edu/108397002/pCO2_Dynamics_on_the_Western_Canadian_Coastal_Margin","translated_internal_url":"","created_at":"2023-10-20T13:10:02.088-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":39578631,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"pCO2_Dynamics_on_the_Western_Canadian_Coastal_Margin","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"There is large uncertainty in sea-air CO2 fluxes from coastal margins due to sparse data sets that inadequately resolve the extreme temporal and spatial variability inherent in these regions. 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Once CO2 dissolves in water, it forms carbonic acid and increases hydrogen ions, thus decreasing seawater pH. In coastal upwelling zones high CO2, low pH water upwells from depth on to the continental shelf. This ``acidified&#x27;&#x27; water reduces the saturation states of calcite and aragonite, adversely affecting calcifying organisms. To study the pH dynamics in a coastal upwelling system Submersible Autonomous Moored Instruments for measuring the partial pressure of CO2 (pCO2) (SAMI-CO2) and pH (SAMI-pH) were moored in surface waters off the coast of Oregon at 44掳 37.93&#x27; N, 124掳 18.19&#x27;W in spring of 2009 and from autumn 2009 through summer 2010. In addition, a SAMI-CO2 and a SAMI-pH were moored at a depth of 123 m on the shelf break just west of the surface mooring. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-108397001-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="108396987"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/108396987/Retention_controls_on_shelf_hypoxia_in_coastal_upwelling_systems"><img alt="Research paper thumbnail of Retention controls on-shelf hypoxia in coastal upwelling systems" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title">Retention controls on-shelf hypoxia in coastal upwelling systems</div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="108396987"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108396987"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108396987; 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Here near bottom oxygen drawdown is controlled by the balance between flushing with offshore source waters and the degree to which surface particulate organic carbon production and its subsequent sinking and remineralization are retained over the shelf and focused on the bottom. In the model, particle production is controlled by wind-driven upwelling of a generic nutrient to the surface, balanced by respiration and sinking. The degree to which this production occurs over shelf is a balance between the net particle growth rate 畏 , and the upwelling driven shelf flushing rate 位 , equivalent to the Ekman upwelling index scaled by the shelf width and surface layer depth. Initial oxygen drawdown follows this exponential rate of surface particle accumula...","owner":{"id":39578631,"first_name":"B.","middle_initials":null,"last_name":"Hales","page_name":"HalesB","domain_name":"independent","created_at":"2015-12-01T15:04:35.113-08:00","display_name":"B. 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Oceans</span><span>, Feb 27, 2024</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="122803764"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="122803764"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 122803764; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=122803764]").text(description); $(".js-view-count[data-work-id=122803764]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 122803764; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='122803764']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=122803764]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":122803764,"title":"Feedbacks Between Estuarine Metabolism and Anthropogenic CO\u003csub\u003e2\u003c/sub\u003e Accelerate Local Rates of Ocean Acidification and Hasten Threshold Exceedances","translated_title":"","metadata":{"publication_date":{"day":27,"month":2,"year":2024,"errors":{}},"publication_name":"Journal of geophysical research. 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However, during bloom and post鈥恇loom conditions large ammonium concentrations and uptake rates have been described. High鈥恌requency on board nitrate聽+聽nitrite and ammonium analysis synchronized with continuous data from a towed profiling vehicle (equipped with in situ temperature, salinity, dissolved oxygen, and beam attenuation sensors), allowed us to describe coupled high鈥恟esolution physico鈥恈hemical dynamics of inorganic nitrogen in seven cross鈥恠helf transects, over several days, during an active phytoplankton bloom following cessation of upwelling favorable winds. We present first鈥恛f鈥恡heir鈥恔ind high鈥恟esolution cross鈥恠ections showing a build鈥恥p, both within a thin plume of onshore鈥恛riginated water, and in mid鈥恡o鈥恇ottom on鈥恠hore water columns, from undetectable values to up to 8聽碌M of ammonium. The plume ext...</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="108397013"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397013"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397013; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108397013]").text(description); $(".js-view-count[data-work-id=108397013]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108397013; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108397013']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=108397013]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108397013,"title":"Short Time鈥怱cale Variability of Ammonium, Nitrate, and Nitrogen Loss Dynamics During an Upwelling鈥怚nduced Bloom at the Oregon Shelf","translated_title":"","metadata":{"abstract":"Ammonium, a key intermediate nutrient, is typically low to undetectable on the Oregon coast, particularly as active upwelling delivers high onshore flow of ammonium鈥恜oor waters. However, during bloom and post鈥恇loom conditions large ammonium concentrations and uptake rates have been described. High鈥恌requency on board nitrate聽+聽nitrite and ammonium analysis synchronized with continuous data from a towed profiling vehicle (equipped with in situ temperature, salinity, dissolved oxygen, and beam attenuation sensors), allowed us to describe coupled high鈥恟esolution physico鈥恈hemical dynamics of inorganic nitrogen in seven cross鈥恠helf transects, over several days, during an active phytoplankton bloom following cessation of upwelling favorable winds. We present first鈥恛f鈥恡heir鈥恔ind high鈥恟esolution cross鈥恠ections showing a build鈥恥p, both within a thin plume of onshore鈥恛riginated water, and in mid鈥恡o鈥恇ottom on鈥恠hore water columns, from undetectable values to up to 8聽碌M of ammonium. The plume ext...","publisher":"American Geophysical Union (AGU)","publication_name":"Journal of Geophysical Research: Oceans"},"translated_abstract":"Ammonium, a key intermediate nutrient, is typically low to undetectable on the Oregon coast, particularly as active upwelling delivers high onshore flow of ammonium鈥恜oor waters. However, during bloom and post鈥恇loom conditions large ammonium concentrations and uptake rates have been described. High鈥恌requency on board nitrate聽+聽nitrite and ammonium analysis synchronized with continuous data from a towed profiling vehicle (equipped with in situ temperature, salinity, dissolved oxygen, and beam attenuation sensors), allowed us to describe coupled high鈥恟esolution physico鈥恈hemical dynamics of inorganic nitrogen in seven cross鈥恠helf transects, over several days, during an active phytoplankton bloom following cessation of upwelling favorable winds. We present first鈥恛f鈥恡heir鈥恔ind high鈥恟esolution cross鈥恠ections showing a build鈥恥p, both within a thin plume of onshore鈥恛riginated water, and in mid鈥恡o鈥恇ottom on鈥恠hore water columns, from undetectable values to up to 8聽碌M of ammonium. The plume ext...","internal_url":"https://www.academia.edu/108397013/Short_Time_Scale_Variability_of_Ammonium_Nitrate_and_Nitrogen_Loss_Dynamics_During_an_Upwelling_Induced_Bloom_at_the_Oregon_Shelf","translated_internal_url":"","created_at":"2023-10-20T13:10:04.849-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":39578631,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Short_Time_Scale_Variability_of_Ammonium_Nitrate_and_Nitrogen_Loss_Dynamics_During_an_Upwelling_Induced_Bloom_at_the_Oregon_Shelf","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Ammonium, a key intermediate nutrient, is typically low to undetectable on the Oregon coast, particularly as active upwelling delivers high onshore flow of ammonium鈥恜oor waters. However, during bloom and post鈥恇loom conditions large ammonium concentrations and uptake rates have been described. High鈥恌requency on board nitrate聽+聽nitrite and ammonium analysis synchronized with continuous data from a towed profiling vehicle (equipped with in situ temperature, salinity, dissolved oxygen, and beam attenuation sensors), allowed us to describe coupled high鈥恟esolution physico鈥恈hemical dynamics of inorganic nitrogen in seven cross鈥恠helf transects, over several days, during an active phytoplankton bloom following cessation of upwelling favorable winds. We present first鈥恛f鈥恡heir鈥恔ind high鈥恟esolution cross鈥恠ections showing a build鈥恥p, both within a thin plume of onshore鈥恛riginated water, and in mid鈥恡o鈥恇ottom on鈥恠hore water columns, from undetectable values to up to 8聽碌M of ammonium. The plume ext...","owner":{"id":39578631,"first_name":"B.","middle_initials":null,"last_name":"Hales","page_name":"HalesB","domain_name":"independent","created_at":"2015-12-01T15:04:35.113-08:00","display_name":"B. 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As such, they are an initiation point for both planning and implementation activities. However, existing water quality criteria, which were created four decades ago, are not scientifically appropriate for assessing OA conditions. Even when existing water quality criteria for seawater pH are met, a wide range of severe biological impacts of OA are observed. New criteria are needed. The Panel further recommends that OA water quality criteria be expanded to include other acidification parameters, as pH is only one of several possible parameters for describing the carbonate system. One such alternative, aragonite saturation state, has been found to be biologically relevant to a number of calcifying organisms. Appendix G provides additional insight about the need for revised water quality criteria.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="52ffe52a7e10a42f2957427d939f4072" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":106792226,"asset_id":108397012,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/106792226/download_file?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="108397012"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397012"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397012; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108397012]").text(description); $(".js-view-count[data-work-id=108397012]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108397012; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108397012']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "52ffe52a7e10a42f2957427d939f4072" } } $('.js-work-strip[data-work-id=108397012]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108397012,"title":"The West Coast Ocean Acidification and Hypoxia Science Panel: Major Findings, Recommendations and Actions","translated_title":"","metadata":{"ai_title_tag":"Revamping Water Quality Criteria for Ocean Acidification","grobid_abstract":"Water quality criteria serve as the foundation for many management activities, providing managers with thresholds to objectively determine the condition of a water body and to set targets for clean-up efforts. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-108397008-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="108397007"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/108397007/Air_water_CO2_Fluxes_and_Inorganic_Carbon_Dynamics_in_a_Microtidal_Eutrophic_Estuary"><img alt="Research paper thumbnail of Air-water CO2 Fluxes and Inorganic Carbon Dynamics in a Microtidal, Eutrophic Estuary" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title">Air-water CO2 Fluxes and Inorganic Carbon Dynamics in a Microtidal, Eutrophic Estuary</div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">ABSTRACT</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="108397007"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397007"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397007; 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However, in the past these measurements have been somewhat restricted due to the time-intensive nature of the sample collection and manual filtration procedures. To increase temporal and spatial coverage of POC distributions, we designed and built a semi-automated filtration</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="108397006"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397006"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397006; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108397006]").text(description); $(".js-view-count[data-work-id=108397006]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108397006; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108397006']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=108397006]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108397006,"title":"Distribution and Composition of Particulate Organic Carbon along Oregon's Upwelling Zone","translated_title":"","metadata":{"abstract":"Direct measurements of particulate organic carbon (POC) concentrations are needed to quantitatively understand the carbon cycle in Eastern Boundary ocean margins. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-108397006-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="108397005"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/108397005/An_update_to_the_Surface_Ocean_CO2_Atlas_SOCAT_"><img alt="Research paper thumbnail of An update to the Surface Ocean CO2 Atlas (SOCAT)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title">An update to the Surface Ocean CO2 Atlas (SOCAT)</div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="108397005"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397005"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397005; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108397005]").text(description); $(".js-view-count[data-work-id=108397005]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108397005; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108397005']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=108397005]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108397005,"title":"An update to the Surface Ocean CO2 Atlas (SOCAT)","translated_title":"","metadata":{},"translated_abstract":null,"internal_url":"https://www.academia.edu/108397005/An_update_to_the_Surface_Ocean_CO2_Atlas_SOCAT_","translated_internal_url":"","created_at":"2023-10-20T13:10:02.655-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":39578631,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"An_update_to_the_Surface_Ocean_CO2_Atlas_SOCAT_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":null,"owner":{"id":39578631,"first_name":"B.","middle_initials":null,"last_name":"Hales","page_name":"HalesB","domain_name":"independent","created_at":"2015-12-01T15:04:35.113-08:00","display_name":"B. 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This system has proved to be a sink of CO2 to deep waters via POC export during the relaxation of the alongshore winds (Hales et al., 2006). On May 2009, during one of those upwelling events, we performed a deliberate tracer injection experiment at the bottom boundary layer (BBL, sigma-t &amp;gt; 26.5) off the Oregon coast. The tracer consisted in a dye/SF6 mixture. After the injection of the tracer the nutrients, carbonate and dissolved oxygen chemistry, as well as in situ hydrography (S, T, bio-optics), of the BBL was measured using a high-frequency profiling system. The tracer was followed for 5 days, during which the water moved towards the coast, according to an upwelling process. SF6 sensitivity allowed us to definitively identify waters that were out of the patch. The main modifications in the chemical properties of the water traced were found nearshore, showing signs of respiration, while there was an apparent decoupling of nitrate from these signals.</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="108397004"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397004"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397004; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108397004]").text(description); $(".js-view-count[data-work-id=108397004]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108397004; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108397004']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=108397004]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108397004,"title":"Changes in the Chemical Composition of the Bottom Boundary Layer during AN Upwelling Event at the Oregon Coast","translated_title":"","metadata":{"abstract":"ABSTRACT On the Oregon coast shelf, prevailing summer winds blow alongshore, mainly favoring the upwelling of nutrient-rich dense offshore water, which triggers a phytoplankton bloom. 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The tracer was followed for 5 days, during which the water moved towards the coast, according to an upwelling process. SF6 sensitivity allowed us to definitively identify waters that were out of the patch. The main modifications in the chemical properties of the water traced were found nearshore, showing signs of respiration, while there was an apparent decoupling of nitrate from these signals.","internal_url":"https://www.academia.edu/108397004/Changes_in_the_Chemical_Composition_of_the_Bottom_Boundary_Layer_during_AN_Upwelling_Event_at_the_Oregon_Coast","translated_internal_url":"","created_at":"2023-10-20T13:10:02.530-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":39578631,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Changes_in_the_Chemical_Composition_of_the_Bottom_Boundary_Layer_during_AN_Upwelling_Event_at_the_Oregon_Coast","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"ABSTRACT On the Oregon coast shelf, prevailing summer winds blow alongshore, mainly favoring the upwelling of nutrient-rich dense offshore water, which triggers a phytoplankton bloom. 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In particular, the change in saturation state (Omega) of calcium carbonate minerals calcite and aragonite may be energetically unfavorable for shell formation while favoring shell dissolution. Eastern boundary upwelling systems may provide</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="108397003"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397003"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397003; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108397003]").text(description); $(".js-view-count[data-work-id=108397003]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108397003; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108397003']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=108397003]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108397003,"title":"Inorganic carbon dynamics in the upwelling system off the Oregon coast and implications for commercial shellfish hatcheries","translated_title":"","metadata":{"abstract":"The increasing absorption of anthropogenic CO2 by the global ocean and concomitant decrease in pH will alter seawater carbonate chemistry in ways that may negatively impact calcifying organisms. 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The western Canadian shelf is no exception to this, and it is thought to be part of an important high latitude sink region for atmospheric CO2, balancing lower latitude source regions</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="108397002"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108397002"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108397002; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108397002]").text(description); $(".js-view-count[data-work-id=108397002]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108397002; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108397002']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=108397002]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108397002,"title":"pCO2 Dynamics on the Western Canadian Coastal Margin","translated_title":"","metadata":{"abstract":"There is large uncertainty in sea-air CO2 fluxes from coastal margins due to sparse data sets that inadequately resolve the extreme temporal and spatial variability inherent in these regions. 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The western Canadian shelf is no exception to this, and it is thought to be part of an important high latitude sink region for atmospheric CO2, balancing lower latitude source regions","internal_url":"https://www.academia.edu/108397002/pCO2_Dynamics_on_the_Western_Canadian_Coastal_Margin","translated_internal_url":"","created_at":"2023-10-20T13:10:02.088-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":39578631,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"pCO2_Dynamics_on_the_Western_Canadian_Coastal_Margin","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"There is large uncertainty in sea-air CO2 fluxes from coastal margins due to sparse data sets that inadequately resolve the extreme temporal and spatial variability inherent in these regions. 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Once CO2 dissolves in water, it forms carbonic acid and increases hydrogen ions, thus decreasing seawater pH. In coastal upwelling zones high CO2, low pH water upwells from depth on to the continental shelf. This ``acidified&#x27;&#x27; water reduces the saturation states of calcite and aragonite, adversely affecting calcifying organisms. To study the pH dynamics in a coastal upwelling system Submersible Autonomous Moored Instruments for measuring the partial pressure of CO2 (pCO2) (SAMI-CO2) and pH (SAMI-pH) were moored in surface waters off the coast of Oregon at 44掳 37.93&#x27; N, 124掳 18.19&#x27;W in spring of 2009 and from autumn 2009 through summer 2010. In addition, a SAMI-CO2 and a SAMI-pH were moored at a depth of 123 m on the shelf break just west of the surface mooring. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-108397001-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="108396987"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/108396987/Retention_controls_on_shelf_hypoxia_in_coastal_upwelling_systems"><img alt="Research paper thumbnail of Retention controls on-shelf hypoxia in coastal upwelling systems" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title">Retention controls on-shelf hypoxia in coastal upwelling systems</div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="108396987"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108396987"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108396987; 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The degree to which this production occurs over shelf is a balance between the net particle growth rate 畏 , and the upwelling driven shelf flushing rate 位 , equivalent to the Ekman upwelling index scaled by the shelf width and surface layer depth. Initial oxygen drawdown follows this exponential rate of surface particle accumula...","internal_url":"https://www.academia.edu/97235778/Potential_and_timescale_for_on_shelf_hypoxia_in_upwelling_systems_and_idealized_model_analysis","translated_internal_url":"","created_at":"2023-02-20T10:43:03.674-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":39578631,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Potential_and_timescale_for_on_shelf_hypoxia_in_upwelling_systems_and_idealized_model_analysis","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"A maximally simple, coupled physical-biogeochemical box model is used to examine interactions controlling the potential and timescale for hypoxic levels of oxygen depletion over the shelf in an idealized eastern boundary upwelling system. Here near bottom oxygen drawdown is controlled by the balance between flushing with offshore source waters and the degree to which surface particulate organic carbon production and its subsequent sinking and remineralization are retained over the shelf and focused on the bottom. In the model, particle production is controlled by wind-driven upwelling of a generic nutrient to the surface, balanced by respiration and sinking. The degree to which this production occurs over shelf is a balance between the net particle growth rate 畏 , and the upwelling driven shelf flushing rate 位 , equivalent to the Ekman upwelling index scaled by the shelf width and surface layer depth. Initial oxygen drawdown follows this exponential rate of surface particle accumula...","owner":{"id":39578631,"first_name":"B.","middle_initials":null,"last_name":"Hales","page_name":"HalesB","domain_name":"independent","created_at":"2015-12-01T15:04:35.113-08:00","display_name":"B. 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