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apples</i><br /> </p> <p> Precise match in quotes: "term1 term2"<br /> <i>"red apples"</i><br /> returns results matching exactly like:<br /> <i>Anthocyanin biosynthesis in <strong>red apples</strong></i><br /> </p> <p> Exclude a term with -: term1 -term2<br /> <i>apples -red</i><br /> returns results containing <i><strong>apples</strong></i> but not <i><strong>red</strong></i>:<br /> <i>Malic acid in green <strong>apples</strong></i><br /> </p> </div> </div> <div class="modal " id="templateSearchResultModal" role="dialog" aria-labelledby="Search results" aria-hidden="true"> <div class="modal-dialog modal-lg modal-dialog-centered"> <div class="modal-content"> <div class="modal-header modal-header--sticky shadow one-column d-block"> <div class="row no-gutters mx-1"> <div class="col mr-3"> <h1 class="" id="resultsSearchHeader"><span id="templateSearchResultNr"></span> hit<span id="templateSearchResultNrPlural">s</span> for <span id="templateSearchResultTerm"></span></h1> </div> <div class="col-auto"> <a id="scrolltopmodal" href="javascript:void(0)" onclick="scrollModalTop();" style="display: none;"><i class="co-home"></i></a> </div> <div class="col-auto"> <button data-dismiss="modal" aria-label="Close" class="btn btn-danger mt-1">Close</button> </div> </div> </div> <div class="modal-body one-column">  <div class="grid-container mx-n3"><div class="grid-85 tablet-grid-85"> <button aria-label="Refine" id="refineSearchModal" class="btn btn-primary float-left mt-4">Refine your search</button> <button aria-label="Refine" id="refineSearchModalHide" class="btn btn-danger float-left d-none mt-4">Hide refinement</button> </div></div> <div class="grid-container mx-n3"><div class="grid-100 tablet-grid-100"><div id="templateRefineSearch" class="d-none"></div></div></div> <div id="templateSearchResultContainer" class="searchResultsModal mx-n3"></div> <div class="grid-container mb-0"><div class="grid-100 tablet-grid-100"><div id="templateSearchResultContainerEmpty" class="co-notification d-none">There are no results for your search term.</div></div></div> </div> </div> </div> </div> </div>  <div class="modal " id="templateSearchErrorModal1" role="dialog" aria-labelledby="Search results" aria-hidden="true"> <div class="modal-dialog modal-lg modal-dialog-centered"> <div class="modal-content p-3"> <div class="modal-body text-left"> <h1 class="mt-0 pt-0">Network problems</h1> <div class="co-error">We are sorry, but your search could not be completed due to network problems. Please try again later.</div> </div> </div> </div> </div>  <div class="modal " id="templateSearchErrorModal2" role="dialog" aria-labelledby="Search results" aria-hidden="true"> <div class="modal-dialog modal-lg modal-dialog-centered"> <div class="modal-content p-3"> <div class="modal-body text-left"> <h1 class="mt-0 pt-0">Server timeout</h1> <div class="co-error">We are sorry, but your search could not be completed due to server timeouts. Please try again later.</div> </div> </div> </div> </div>  <div class="modal " id="templateSearchErrorModal3" role="dialog" aria-labelledby="Search results" aria-hidden="true"> <div class="modal-dialog modal-lg modal-dialog-centered"> <div class="modal-content p-3"> <div class="modal-body text-left"> <h1 class="mt-0 pt-0">Empty search term</h1> <div class="co-error">You have applied the search with an empty search term. Please revisit and try again.</div> </div> </div> </div> </div>  <div class="modal " id="templateSearchErrorModal4" role="dialog" aria-labelledby="Search results" aria-hidden="true"> <div class="modal-dialog modal-lg modal-dialog-centered"> <div class="modal-content p-3"> <div class="modal-body text-left"> <h1 class="mt-0 pt-0">Too many requests</h1> <div class="co-error">We are sorry, but we have received too many parallel search requests. Please try again later.</div> </div> </div> </div> </div>  <div class="modal " id="templateSearchLoadingModal" role="dialog" aria-labelledby="Search results" aria-hidden="true"> <div class="modal-dialog modal-sm modal-dialog-centered"> <div class="modal-content p-3 co_LoadingDotsContainer"> <div class="modal-body"> <div class="text">Searching</div> <div class="dots d-flex justify-content-center"><div class="dot"></div><div class="dot"></div><div class="dot"></div></div></div> </div> </div> </div> </div> <style> /*.modal {*/ /* background: rgba(255, 255, 255, 0.8);*/ /*}*/ .modal-header--sticky { position: sticky; top: 0; background-color: inherit; z-index: 1055; } .grid-container { margin-bottom: 1em; /*padding-left: 0;*/ /*padding-right: 0;*/ } #templateSearchInfo{ display: none; background-color: var(--background-color-primary); margin-top: 1px; z-index: 5; border: 1px solid var(--color-primary); opacity: .8; font-size: .7rem; border-radius: .25rem; } #templateSearchLoadingModal .co_LoadingDotsContainer { z-index: 1000; } #templateSearchLoadingModal .co_LoadingDotsContainer .text { text-align: center; font-weight: bold; padding-bottom: 1rem; } #templateSearchLoadingModal .co_LoadingDotsContainer .dot { background-color: #0072BC; border: 2px solid white; border-radius: 50%; float: left; height: 2rem; width: 2rem; margin: 0 5px; -webkit-transform: scale(0); transform: scale(0); -webkit-animation: animation_dots_breath 1000ms ease infinite 0ms; animation: animation_dots_breath 1000ms ease infinite 0ms; } #templateSearchLoadingModal .co_LoadingDotsContainer .dot:nth-child(2) { -webkit-animation: animation_dots_breath 1000ms ease infinite 300ms; animation: animation_dots_breath 1000ms ease infinite 300ms; } #templateSearchLoadingModal .co_LoadingDotsContainer .dot:nth-child(3) { -webkit-animation: animation_dots_breath 1000ms ease infinite 600ms; animation: animation_dots_breath 1000ms ease infinite 600ms; } #templateSearchResultModal [class*="grid-"] { padding-left: 10px !important; padding-right: 10px !important; } #templateSearchResultTerm { font-weight: bold; } #resultsSearchHeader { display: block !important; } #scrolltopmodal { font-size: 3.0em; margin-top: 0 !important; margin-right: 15px; } @-webkit-keyframes animation_dots_breath { 50% { -webkit-transform: scale(1); transform: scale(1); opacity: 1; } 100% { opacity: 0; } } @keyframes animation_dots_breath { 50% { -webkit-transform: scale(1); transform: scale(1); opacity: 1; } 100% { opacity: 0; } } @media (min-width: 768px) and (max-width: 991px) { #templateSearchResultModal .modal-dialog { max-width: 90%; } } </style> <script> if(document.querySelector('meta[name="global_moBaseURL"]').content == "https://meetingorganizer.copernicus.org/") FINDER_URL = document.querySelector('meta[name="global_moBaseURL"]').content.replace('meetingorganizer', 'finder-app')+"search/library.php"; else FINDER_URL = document.querySelector('meta[name="global_moBaseURL"]').content.replace('meetingorganizer', 'finder')+"search/library.php"; SEARCH_INPUT = document.getElementById('search_query_solr'); SEARCH_INPUT_MODAL = document.getElementById('search_query_modal'); searchRunning = false; offset = 20; INITIAL_OFFSET = 20; var MutationObserver = window.MutationObserver || window.WebKitMutationObserver || window.MozMutationObserver; const targetNodeSearchModal = document.getElementById("templateSearchResultModal"); const configSearchModal = { attributes: true, childList: true, subtree: true }; // Callback function to execute when mutations are observed const callbackSearchModal = (mutationList, observer) => { for (const mutation of mutationList) { if (mutation.type === "childList") { // console.log("A child node has been added or removed."); picturesGallery(); } else if (mutation.type === "attributes") { // console.log(`The ${mutation.attributeName} attribute was modified.`); } } }; // Create an observer instance linked to the callback function const observer = new MutationObserver(callbackSearchModal); // Start observing the target node for configured mutations observer.observe(targetNodeSearchModal, configSearchModal); function _addEventListener() { document.getElementById('search_query_solr').addEventListener('keypress', (e) => { if (e.key === 'Enter') _runSearch(); }); document.getElementById('start_site_search_solr').addEventListener('click', (e) => { _runSearch(); e.stopPropagation(); e.stopImmediatePropagation(); return false; }); $('#templateSearchResultModal').scroll(function() { if ($(this).scrollTop()) { $('#scrolltopmodal:hidden').stop(true, true).fadeIn().css("display","inline-block"); } else { $('#scrolltopmodal').stop(true, true).fadeOut(); } }); } function scrollModalTop() { $('#templateSearchResultModal').animate({ scrollTop: 0 }, 'slow'); // $('#templateSearchResultModal').scrollTop(0); } function picturesGallery() { $('body').off('click', '.paperlist-avatar img'); $('body').off('click', '#templateSearchResultContainer .paperlist-avatar img'); searchPaperListAvatar = []; searchPaperListAvatarThumb = []; search_pswpElement = document.querySelectorAll('.pswp')[0]; if (typeof search_gallery != "undefined") { search_gallery = null; } $('body').on('click', '#templateSearchResultContainer .paperlist-avatar img', function (e) { if(searchPaperListAvatarThumb.length === 0 && searchPaperListAvatar.length === 0) { $('#templateSearchResultContainer .paperlist-avatar img').each(function () { var webversion = $(this).attr('data-web'); var width = $(this).attr('data-width'); var height = $(this).attr('data-height'); var caption = $(this).attr('data-caption'); var figure = { src: webversion, w: width, h: height, title: caption }; searchPaperListAvatarThumb.push($(this)[0]); searchPaperListAvatar.push(figure); }); } var target = $(this); var index = $('#templateSearchResultContainer .paperlist-avatar img').index(target); var options = { showHideOpacity:false, bgOpacity:0.8, index:index, spacing:0.15, history: false, focus:false, getThumbBoundsFn: function(index) { var thumbnail = searchPaperListAvatarThumb[index]; var pageYScroll = window.pageYOffset || document.documentElement.scrollTop; var rect = thumbnail.getBoundingClientRect(); return {x:rect.left, y:rect.top + pageYScroll, w:rect.width}; } }; search_gallery = new PhotoSwipe( search_pswpElement, PhotoSwipeUI_Default,[searchPaperListAvatar[index]],options); search_gallery.init(); }); } function showError(code, msg) { console.error(code, msg); $("#templateSearchLoadingModal").modal("hide"); switch(code) { case -3: // http request fail case -2: // invalid MO response case 4: // CORS case 1: // project $("#templateSearchErrorModal1").modal({}); break; case -1: // timeout $("#templateSearchErrorModal2").modal({}); break; case 2: // empty term $("#templateSearchErrorModal3").modal({}); break; case 3: // DOS $("#templateSearchErrorModal4").modal({}); break; default: $("#templateSearchErrorModal1").modal({}); break; } } function clearForm() { var myFormElement = document.getElementById("library-filters") var elements = myFormElement.elements; $(".form-check-input").prop('checked', false).change().parent().removeClass('active'); for(i=0; i<elements.length; i++) { field_type = elements[i].type.toLowerCase(); switch(field_type) { case "text": case "password": case "textarea": case "hidden": elements[i].value = ""; break; case "radio": case "checkbox": if (elements[i].checked) { elements[i].checked = false; } break; case "select-one": case "select-multi": elements[i].selectedIndex = -1; break; default: break; } } } function generateShowMoreButton(offset, term) { var code = '<button aria-label="ShowMore" id="showMore" class="btn btn-success float-right mr-2" data-offset="' + offset + '">Show more</button>'; return code; } function hideModal(id) { $("#"+id).modal('hide'); } function showModal(id) { $("#"+id).modal({}); } function prepareForPhotoSwipe() { searchPaperListAvatar = []; searchPaperListAvatarThumb = []; search_pswpElement = document.querySelectorAll('.pswp')[0]; } function _sendAjax(projectID, term) { let httpRequest = new XMLHttpRequest(); if(searchRunning) { console.log("Search running"); return; } if (!httpRequest) { console.error("Giving up :( Cannot create an XMLHTTP instance"); showError(-1); return false; } // httpRequest.timeout = 20000; // time in milliseconds httpRequest.withCredentials = false; httpRequest.ontimeout = (e) => { showError(-1, "result timeout"); searchRunning = false; }; httpRequest.onreadystatechange = function() { if (httpRequest.readyState === XMLHttpRequest.DONE) { searchRunning = false; if (httpRequest.status === 200) { let rs = JSON.parse(httpRequest.responseText); if(rs) { if(rs.isError) { showError(rs.errorCode, rs.errorMessage); } else { let html = rs.resultHTMLs; $("#modal_search_query").val(rs.term); $("#templateSearchResultTerm").html(rs.term); $("#templateSearchResultNr").html(rs.resultsNr); $("#templateRefineSearch").html(rs.filter); if(rs.filter == false) { console.log('filter empty'); $("#refineSearchModal").removeClass('d-block').addClass('d-none'); } if(rs.resultsNr==1) $("#templateSearchResultNrPlural").hide(); else $("#templateSearchResultNrPlural").show(); if(rs.resultsNr==0) { hideModal('templateSearchLoadingModal'); $("#templateSearchResultContainer").html(""); $("#templateSearchResultContainerEmpty").removeClass("d-none"); showModal('templateSearchResultModal'); } else { if((rs.resultsNr - offset)>0) { html = html + generateShowMoreButton(offset, term); } $("#templateSearchResultContainerEmpty").addClass("d-none"); if( offset == INITIAL_OFFSET) { hideModal('templateSearchLoadingModal'); $("#templateSearchResultContainer").html(html); showModal('templateSearchResultModal'); } else { $('#showMore').remove(); startHtml = $("#templateSearchResultContainer").html(); $("#templateSearchResultContainer").html(startHtml + html); } // prepareForPhotoSwipe(); } } } else { showError(-2, "invalid result"); } } else { showError(-3, "There was a problem with the request."); } } }; if(offset == INITIAL_OFFSET) { hideModal('templateSearchResultModal'); showModal('templateSearchLoadingModal'); } httpRequest.open("GET", FINDER_URL+"?project="+projectID+"&term="+encodeURI(term)+((offset>INITIAL_OFFSET)?("&offset="+(offset-INITIAL_OFFSET)) : "")); httpRequest.send(); searchRunning = true; } function _runSearch() { var projectID = document.querySelector('meta[name="global_projectID"]').content; var term = _searchTrimInput(SEARCH_INPUT.value); if(term.length > 0) { _sendAjax(projectID, term); } else { showError(2, 'Empty search term') } } function _searchTrimInput(str) { return str.replace(/^\s+|\s+$/gm, ''); } function run() { _addEventListener(); $('#templateSearchInfoBtn, #modalSearchInfoBtn').popover({ sanitize: false, html: true, content: $("#templateSearchInfo").html(), placement: "bottom", template: '<div class="popover" role="tooltip"><div class="arrow"></div><button class="m-1 float-right btn btn-sm btn-danger" id="templateSearchInfoClose"><i class="fas fa-times-circle"></i></button><h3 class="popover-header"></h3><div class="popover-body"></div></div>', title: "Search tips", }); $(document).click(function (e) { let t = $(e.target); let a = t && t.attr("data-toggle")!=="popover" && t.parent().attr("data-toggle")!=="popover"; let b = t && $(".popover").has(t).length===0; if(a && b) { $('#templateSearchInfoBtn').popover('hide'); $('#modalSearchInfoBtn').popover('hide'); } }); $('#templateSearchInfoBtn').on('shown.bs.popover', function () { $("#templateSearchInfoClose").click(function(e){ $('#templateSearchInfoBtn').popover('hide'); e.stopPropagation(); e.stopImmediatePropagation(); return false; }); }) $('#templateSearchResultModal').on('hidden.bs.modal', function(e) { $('body').off('click', '#templateSearchResultContainer .paperlist-avatar img'); var pswpElement = document.querySelectorAll('.pswp')[0]; var gallery = null; var paperListAvatar = []; var paperListAvatarThumb = []; $('.paperlist-avatar img').each(function(){ var webversion = $(this).attr('data-web'); var width = $(this).attr('data-width'); var height = $(this).attr('data-height'); var caption =$(this).attr('data-caption'); var figure = { src:webversion, w:width, h:height, title:caption }; paperListAvatarThumb.push($(this)[0]); paperListAvatar.push(figure); }); $('body').on('click', '.paperlist-avatar img', function (e) { if(paperListAvatarThumb.length === 0 && paperListAvatar.length === 0){ $('.paperlist-avatar img').each(function(){ var webversion = $(this).attr('data-web'); var width = $(this).attr('data-width'); var height = $(this).attr('data-height'); var caption =$(this).attr('data-caption'); var figure = { src:webversion, w:width, h:height, title:caption }; paperListAvatarThumb.push($(this)[0]); paperListAvatar.push(figure); }); } var target = $(this); var index = $('.paperlist-avatar img').index(target); var options = { showHideOpacity:true, bgOpacity:0.8, index:index, spacing:0.15, getThumbBoundsFn: function(index) { var thumbnail = paperListAvatarThumb[index]; var pageYScroll = window.pageYOffset || document.documentElement.scrollTop; var rect = thumbnail.getBoundingClientRect(); return {x:rect.left, y:rect.top + pageYScroll, w:rect.width}; } }; gallery = new PhotoSwipe( pswpElement, PhotoSwipeUI_Default,[paperListAvatar[index]],options); gallery.init(); }); }); $('#templateSearchResultModal').on('hide.bs.modal', function(e) { $("#templateRefineSearch").removeClass('d-block').addClass('d-none'); $("#refineSearchModalHide").removeClass('d-block').addClass('d-none'); $("#refineSearchModal").removeClass('d-none').addClass('d-block'); offset = INITIAL_OFFSET; }) $(document).on("click", "#showMore", function(e){ offset+=INITIAL_OFFSET; runSearchModal() e.stopPropagation(); e.stopImmediatePropagation(); return false; }); $(document).ready(function() { $(document).on("click", "#refineSearchModal", function (e) { $("#templateRefineSearch").removeClass('d-none').addClass('d-block'); $(this).removeClass('d-block').addClass('d-none'); $("#refineSearchModalHide").removeClass('d-none').addClass('d-block'); }); $(document).on("click", "#refineSearchModalHide", function (e) { $("#templateRefineSearch").removeClass('d-block').addClass('d-none'); $(this).removeClass('d-block').addClass('d-none'); $("#refineSearchModal").removeClass('d-none').addClass('d-block'); }); $(document).on("click", "#modal_start_site_search", function (e) { runSearchModal(); e.stopPropagation(); e.stopImmediatePropagation(); return false; }); }); } function runSearchModal() { var projectID = document.querySelector('meta[name="global_projectID"]').content; var queryString = $('#library-filters').serialize(); var term = _searchTrimInput($('#modal_search_query').val()); term+='&'+queryString; if(term.length > 0) { _sendAjax(projectID, term); } else { showError(2, 'Empty search term') } } if(document.getElementById('search_query_solr')) { run(); } </script> </div></div>  </div> </div> </div> </div> </header>  <main class="one-column version-2023"> <div id="content" class="container"> <div id="page_content_container" class="CMSCONTAINER content-container">    <div id="landing_page" class="cmsbox j-intro-section j-section"><div class="row mt-1"> <div class="col-12 d-xl-none mt-1"> <div class="row service_icons mb-3"> <a href="https://www.ocean-sci.net/recent_papers.html" class="col-auto pr-0"> <img src="https://www.ocean-science.net/icon_open_access.svg" title="Open access" alt="Open access" /></a> <a href="https://www.ocean-science.net/peer_review/interactive_review_process.html" class="col-auto pr-0"> <img src="https://www.ocean-science.net/icon_public_peer_review.svg" title="Public peer review" alt="Public peer review" /></a> <a href="https://www.ocean-science.net/about/article_level_metrics.html" class="col-auto pr-0 d-none d-md-inline-block"> <img src="https://www.ocean-science.net/icon_article_level_metrics.svg" title="Article level metrics" alt="Article level metrics" /></a> <a href="https://www.ocean-science.net/about/article_processing_charges.html" class="col-auto pr-0 d-none d-xxl-inline-block"> <img src="https://www.ocean-science.net/icon_moderateAPCs.svg" title="Moderate APCs" alt="Moderate APCs" /></a> </div> </div> <div class="col-auto d-none d-lg-block img-responsive"> <img id="open_pop_up" src="https://www.ocean-science.net/os_journal_cover_homepage.jpg" cofileid="12264" alt="OS cover" title="OS cover" data-toggle="modal" data-target="#coverModal" class="hover-cursor-pointer" /> </div> <div class="col pl-lg-0 mt-1"> <div class="row service_icons mb-3 d-none d-xl-block"> <a href="https://www.ocean-sci.net/recent_papers.html" class="col-auto pr-0"> <img src="https://www.ocean-science.net/icon_open_access.svg" title="Open access" alt="Open access" /></a> <a href="https://www.ocean-science.net/peer_review/interactive_review_process.html" class="col-auto pr-0"> <img src="https://www.ocean-science.net/icon_public_peer_review.svg" title="Public peer review" alt="Public peer review" /></a> <a href="https://www.ocean-science.net/about/article_level_metrics.html" class="col-auto pr-0 d-none d-md-inline-block"> <img src="https://www.ocean-science.net/icon_article_level_metrics.svg" title="Article level metrics" alt="Article level metrics" /></a> <a href="https://www.ocean-science.net/about/article_processing_charges.html" class="col-auto pr-0 d-none d-xxl-inline-block"> <img src="https://www.ocean-science.net/icon_moderateAPCs.svg" title="Moderate APCs" alt="Moderate APCs" /></a> <a href="https://www.ocean-science.net/about/financial_support.html" class="col-auto pr-0 d-none d-xxl-inline-block"> <img src="https://www.ocean-science.net/icon_financial_support.svg" title="Financial support" alt="Financial support" /></a> </div> <div class="row"> <div class="col-12 font-weight-bold">Co-editors-in-chief: Karen J. Heywood, Mario Hoppema, Bernadette Sloyan & Anne Marie Treguier</div> </div> <div class="row mb-3"> <div class="col-12"> eISSN: OS <span class="" id="cmsvar_111">1812-0792</span>, OSD <span class="" id="cmsvar_115">1812-0822</span> </div> </div> <div class="row"> <div class="col-12"> <p class="font-weight-normal">Ocean Science (OS) is a not-for-profit international scientific journal dedicated to the publication and public discussion of studies investigating the ocean's physical, biogeochemical and biological and ecosystem properties and processes. Ocean Science publishes studies with important implications for our understanding of the state and behaviour of the ocean, its impacts on and responses to climate, including coupling at the ocean–atmosphere, ocean–sea ice–ice sheet and ocean–coast (land) interfaces.</p> </div> </div> </div> </div> <div id="coverModal" class="modal fade" tabindex="-1" role="dialog" aria-hidden="true"> <div class="modal-dialog"> <div class="modal-content"> <div class="modal-header"> <button type="button" class="close" data-dismiss="modal" aria-label="Close"> <span aria-hidden="true">×</span> </button> </div> <div class="container-fluid"> <div class="row"> <div class="col-12 p-3"> <img class="img-fluid" alt="OS cover enlarged" cofileid="20464" src="https://www.ocean-science.net/graphic_OS_cover_huge.jpg" /> </div> </div> </div> </div> </div> </div></div><div id="cmsbox_124258" class="cmsbox mobile-metrics landscape mt-3"> <div class="journal-metrics-wrapper landscape"> <div class="row journal-metrics-item-wrapper align-items-center"> <div class="col-6 col-md mt-3 mt-md-0 "> <div class="row mb-3 mb-md-0 journal-metrics-item align-items-center"> <div class="col-12 col-lg-auto img-responsive"> <img src="https://contentmanager.copernicus.org/390807/ssl" alt="JIF" class=""> </div> <div class="col-12 col-lg pl-lg-0 journal-metrics-item-label mt-2 mt-lg-0"> <span class="pr-1">JIF</span>4.1 </div> </div> </div> <div class="col-6 col-md mt-3 mt-md-0 "> <div class="row mb-3 mb-md-0 journal-metrics-item align-items-center"> <div class="col-12 col-lg-auto img-responsive"> <img src="https://contentmanager.copernicus.org/390807/ssl" alt="JIF 5-year" class=""> </div> <div class="col-12 col-lg pl-lg-0 journal-metrics-item-label mt-2 mt-lg-0"> <span class="pr-1">JIF 5-year</span>4 </div> </div> </div> <div class="col-6 col-md mt-3 mt-md-0 "> <div class="row mb-3 mb-md-0 journal-metrics-item align-items-center"> <div class="col-12 col-lg-auto img-responsive"> <img src="https://contentmanager.copernicus.org/390808/ssl" alt="CiteScore" class=""> </div> <div class="col-12 col-lg pl-lg-0 journal-metrics-item-label mt-2 mt-lg-0"> <span class="pr-1">CiteScore</span>5.9 </div> </div> </div> <div class="col-6 col-md mt-3 mt-md-0 "> <div class="row mb-3 mb-md-0 journal-metrics-item align-items-center"> <div class="col-12 col-lg-auto img-responsive"> <img src="https://contentmanager.copernicus.org/390811/ssl" alt="Google h5-index" class=""> </div> <div class="col-12 col-lg pl-lg-0 journal-metrics-item-label mt-2 mt-lg-0"> <span class="pr-1">Google h5-index</span>33 </div> </div> </div> </div> </div> </div><div id="news_container" class="cmsbox "> <h2>News</h2> <div class="grid-container paperlist-object"> <div class="hide-on-desktop hide-on-tablet mobile-grid-100"> <a class="no-border paperlist-avatar-unclickable" target="_blank" href="https://www.egu.eu/webinars/229/how-to-write-a-research-paper/"><img alt="" cofileid="454898" src="https://www.ocean-science.net/graphic-logo-egu-80px.png" width="80px"/></a> </div> <div class="hide-on-desktop hide-on-tablet mobile-grid-100"> <span class="published-date">13 Sep 2024</span> <a target="_blank" href="https://www.egu.eu/webinars/229/how-to-write-a-research-paper/" class="article-title">EGU webinar: how to write a research paper</a> <p class="citation">You have worked hard to get your results, analyse the data, and draw conclusions from your research topic. Now it is time to write up! Please find information on EGU's webinar "How to write a research paper" <a target="_blank" href="https://www.egu.eu/webinars/229/how-to-write-a-research-paper/">here</a>. <a target="_blank" href="https://www.egu.eu/webinars/229/how-to-write-a-research-paper/"><img cofileid="17978" alt="" src="https://www.ocean-science.net/graphic_grey_right_symbol.png"></a></p> </div> <div class="grid-85 tablet-grid-85 hide-on-mobile"> <span class="published-date">13 Sep 2024</span> <a target="_blank" href="https://www.egu.eu/webinars/229/how-to-write-a-research-paper/" class="article-title">EGU webinar: how to write a research paper</a> <p class="citation">You have worked hard to get your results, analyse the data, and draw conclusions from your research topic. Now it is time to write up! Please find information on EGU's webinar "How to write a research paper" <a target="_blank" href="https://www.egu.eu/webinars/229/how-to-write-a-research-paper/">here</a>. <a target="_blank" href="https://www.egu.eu/webinars/229/how-to-write-a-research-paper/"><img cofileid="17978" alt="" src="https://www.ocean-science.net/graphic_grey_right_symbol.png"></a></p> </div> <div class="grid-15 tablet-grid-15 hide-on-mobile text-right"> <a class="no-border paperlist-avatar-unclickable" target="_blank" href="https://www.egu.eu/webinars/229/how-to-write-a-research-paper/"><img alt="" cofileid="454898" src="https://www.ocean-science.net/graphic-logo-egu-80px.png" width="80px"/></a> </div> <div class="hide-on-desktop hide-on-tablet mobile-grid-100"> <img class=" paperlist-avatar-unclickable" alt="" cofileid="2543936" src="https://www.ocean-science.net/logo-researchgate-short-bw.svg" width="80px"/> </div> <div class="hide-on-desktop hide-on-tablet mobile-grid-100"> <span class="published-date">12 Sep 2024</span> <span class="article-title">OS now at ResearchGate</span> <p class="citation">Copernicus is pleased to announce a new collaboration with ResearchGate in the framework of ResearchGate's Journal Home programme. Please read Copernicus' <a target="blank" href="https://publications.copernicus.org/news_and_press/2024-09-12_new-collaboration-between-copernicus-publications-and-researchgate.html">official announcement</a> and have a look at <a target="blank" href="https://www.researchgate.net/journal/Ocean-Science-1812-0792">OS' profile page</a> for more details. </p> </div> <div class="grid-85 tablet-grid-85 hide-on-mobile"> <span class="published-date">12 Sep 2024</span> <span class="article-title">OS now at ResearchGate</span> <p class="citation">Copernicus is pleased to announce a new collaboration with ResearchGate in the framework of ResearchGate's Journal Home programme. Please read Copernicus' <a target="blank" href="https://publications.copernicus.org/news_and_press/2024-09-12_new-collaboration-between-copernicus-publications-and-researchgate.html">official announcement</a> and have a look at <a target="blank" href="https://www.researchgate.net/journal/Ocean-Science-1812-0792">OS' profile page</a> for more details. </p> </div> <div class="grid-15 tablet-grid-15 hide-on-mobile text-right"> <img class=" paperlist-avatar-unclickable" alt="" cofileid="2543936" src="https://www.ocean-science.net/logo-researchgate-short-bw.svg" width="80px"/> </div> <div class="j-news-archive-link grid-100 tablet-grid-100 mobile-grid-100"> <a class="btn btn-primary" href="https://www.ocean-science.net/about/news_and_press.html">News archive</a> </div> </div> </div><div id="highlight-articles" class="cmsbox landing-page mt-4"><div id="highlight-paper-content"> <div id="highlight-articles-header"> <h2>Highlight articles</h2> </div> <div class="grid-container paperlist-object in-range paperList-final" data-diff="0"> <div class="grid-100 hide-on-desktop hide-on-tablet"> <a class="paperlist-avatar" target="_blank" href="https://os.copernicus.org/articles/20/661/2024/os-20-661-2024-avatar-web.png"> <img class="img-responsive" src="https://os.copernicus.org/articles/20/661/2024/os-20-661-2024-avatar-thumb80.png" data-caption="Copyright waived. This work has been dedicated to the public domain (Creative Commons Public Domain Dedication)." data-web="https://os.copernicus.org/articles/20/661/2024/os-20-661-2024-avatar-web.png" data-width="517" data-height="600" width="80" height="80"> </a> </div> <div class="grid-85 tablet-grid-85"> <div class="published-date"> 24 May 2024</div> <a class="article-title" target="_parent" href="https://os.copernicus.org/articles/20/661/2024/">Impact of Hurricane Irma on coral reef sediment redistribution at Looe Key Reef, Florida, USA</a> <div class="authors">Kimberly K. Yates, Zachery Fehr, Selena Johnson, and David Zawada</div> <div class="citation">Ocean Sci., 20, 661–688, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/os-20-661-2024,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/os-20-661-2024,</span> 2024</div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_116862" data-show=".short_summary_116862" data-hide=".short_summary_button_116862" >Short summary</span> <span class="show-hide journal-contentLinkColor triangle ce_comment_button_116862 ml-2" data-show=".ce_comment_116862" data-hide=".ce_comment_button_116862">Co-editor-in-chief</span> <div class="j-widget__max short_summary short_summary_116862" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Global understanding of storm-driven sediment transport along coral reefs and its impact on species and habitats is limited. Measurement of seafloor elevation and volume change due to a category 4 hurricane showed rapid burial of coral reef habitats and migration of large seafloor features due to the storm. Post-storm erosion rates were 2 orders of magnitude greater than historical rates, indicating areas of seafloor instability that could be less suitable for restoration of benthic species. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_116862" data-show=".short_summary_button_116862">Hide</a></div> </div> </div> <div class="j-widget__max ce_comment ce_comment_116862 mt-3" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Co-editor-in-chief</div> <div class="content"> This paper, using pre-storm, immediate post-storm and recovery data, quantifies seafloor elevation and volume change within the Looe Key Reef system of the Florida Keys Reef Tract over a 2.5-year period from 2016–2019 and to examine impacts from category-4 Hurricane Irma and post-storm re-equilibration of seafloor sediments. The study highlights the need to data collected over seasonal and annual time periods to improve characterization and understanding of short-term (event-driven, seasonal, interannual) and long-term (decadal to multi-decadal) rates and processes of seafloor change and help guide benthic habitat post-storm recovery and restoration efforts in topographically complex coral reef systems. </div> <div><a href="#" class="show-hide triangle" data-hide=".ce_comment_116862" data-show=".ce_comment_button_116862">Hide</a></div> </div> </div> </div> <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> <a class="paperlist-avatar" target="_blank" href="https://os.copernicus.org/articles/20/661/2024/os-20-661-2024-avatar-web.png"> <img class="img-responsive" src="https://os.copernicus.org/articles/20/661/2024/os-20-661-2024-avatar-thumb80.png" data-web="https://os.copernicus.org/articles/20/661/2024/os-20-661-2024-avatar-web.png" data-width="517" data-caption="Copyright waived. This work has been dedicated to the public domain (Creative Commons Public Domain Dedication)." data-height="600" width="80" height="80"> </a> </div> </div> <div class="grid-container paperlist-object in-range paperList-final" data-diff="0"> <div class="grid-100 hide-on-desktop hide-on-tablet"> <a class="paperlist-avatar" target="_blank" href="https://os.copernicus.org/articles/20/569/2024/os-20-569-2024-avatar-web.png"> <img class="img-responsive" src="https://os.copernicus.org/articles/20/569/2024/os-20-569-2024-avatar-thumb80.png" data-caption="© D. van Oevelen for the photo (bottom right). All rights reserved. © Authors for the rest of the figure. Distributed under the Creative Commons Attribution 4.0 License." data-web="https://os.copernicus.org/articles/20/569/2024/os-20-569-2024-avatar-web.png" data-width="600" data-height="399" width="80" height="80"> </a> </div> <div class="grid-85 tablet-grid-85"> <div class="published-date"> 15 Apr 2024</div> <a class="article-title" target="_parent" href="https://os.copernicus.org/articles/20/569/2024/">Resemblance of the global depth distribution of internal-tide generation and cold-water coral occurrences</a> <div class="authors">Anna-Selma van der Kaaden, Dick van Oevelen, Christian Mohn, Karline Soetaert, Max Rietkerk, Johan van de Koppel, and Theo Gerkema</div> <div class="citation">Ocean Sci., 20, 569–587, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/os-20-569-2024,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/os-20-569-2024,</span> 2024</div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_111365" data-show=".short_summary_111365" data-hide=".short_summary_button_111365" >Short summary</span> <span class="show-hide journal-contentLinkColor triangle ce_comment_button_111365 ml-2" data-show=".ce_comment_111365" data-hide=".ce_comment_button_111365">Co-editor-in-chief</span> <div class="j-widget__max short_summary short_summary_111365" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Cold-water corals (CWCs) and tidal waves in the interior of the ocean have been connected in case studies. We demonstrate this connection globally using hydrodynamic simulations and a CWC database. Internal-tide generation shows a similar depth pattern with slope steepness and latitude as CWCs. Our results suggest that internal-tide generation can be a useful predictor of CWC habitat and that current CWC habitats might change following climate-change-related shoaling of internal-tide generation. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_111365" data-show=".short_summary_button_111365">Hide</a></div> </div> </div> <div class="j-widget__max ce_comment ce_comment_111365 mt-3" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Co-editor-in-chief</div> <div class="content"> There have been various recent papers linking internal waves/tides with cold water coral distribution and abundance. This is the first one, to the best of our knowledge, that approaches the question from a global context. The focus on biophysical interaction means that it may be of particular interest to the broad geoscience community. </div> <div><a href="#" class="show-hide triangle" data-hide=".ce_comment_111365" data-show=".ce_comment_button_111365">Hide</a></div> </div> </div> </div> <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> <a class="paperlist-avatar" target="_blank" href="https://os.copernicus.org/articles/20/569/2024/os-20-569-2024-avatar-web.png"> <img class="img-responsive" src="https://os.copernicus.org/articles/20/569/2024/os-20-569-2024-avatar-thumb80.png" data-web="https://os.copernicus.org/articles/20/569/2024/os-20-569-2024-avatar-web.png" data-width="600" data-caption="© D. van Oevelen for the photo (bottom right). All rights reserved. © Authors for the rest of the figure. Distributed under the Creative Commons Attribution 4.0 License." data-height="399" width="80" height="80"> </a> </div> </div> <div class="grid-container paperlist-object in-range paperList-final" data-diff="0"> <div class="grid-100 hide-on-desktop hide-on-tablet"> <a class="paperlist-avatar" target="_blank" href="https://os.copernicus.org/articles/19/1669/2023/os-19-1669-2023-avatar-web.png"> <img class="img-responsive" src="https://os.copernicus.org/articles/19/1669/2023/os-19-1669-2023-avatar-thumb80.png" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-web="https://os.copernicus.org/articles/19/1669/2023/os-19-1669-2023-avatar-web.png" data-width="600" data-height="322" width="80" height="80"> </a> </div> <div class="grid-85 tablet-grid-85"> <div class="published-date"> 30 Nov 2023</div> <a class="article-title" target="_parent" href="https://os.copernicus.org/articles/19/1669/2023/">Constraining an eddy energy dissipation rate due to relative wind stress for use in energy budget-based eddy parameterisations</a> <div class="authors">Thomas Wilder, Xiaoming Zhai, David Munday, and Manoj Joshi</div> <div class="citation">Ocean Sci., 19, 1669–1686, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/os-19-1669-2023,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/os-19-1669-2023,</span> 2023</div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_112317" data-show=".short_summary_112317" data-hide=".short_summary_button_112317" >Short summary</span> <span class="show-hide journal-contentLinkColor triangle ce_comment_button_112317 ml-2" data-show=".ce_comment_112317" data-hide=".ce_comment_button_112317">Co-editor-in-chief</span> <div class="j-widget__max short_summary short_summary_112317" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> The dissipation rate of eddy energy in current energy budget-based eddy parameterisations is still relatively unconstrained, leading to uncertainties in ocean transport and ocean heat uptake. Here, we derive a dissipation rate due to the interaction of surface winds and eddy currents, a process known to significantly damp ocean eddies. The dissipation rate is quantified using seasonal climatology and displays wide spatial variability, with some of the largest values found in the Southern Ocean. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_112317" data-show=".short_summary_button_112317">Hide</a></div> </div> </div> <div class="j-widget__max ce_comment ce_comment_112317 mt-3" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Co-editor-in-chief</div> <div class="content"> This analytical study investigates the eddy energy dissipation rate for relative wind stress. The derived dissipation rate draws on our fundamental understanding of relative wind stress damping, vertical eddy structure, and eddy energy. The study suggests a method to parameterise the damping of total eddy energy in coarse resolution global climate models, and may have implications for a wide range of climate processes. </div> <div><a href="#" class="show-hide triangle" data-hide=".ce_comment_112317" data-show=".ce_comment_button_112317">Hide</a></div> </div> </div> </div> <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> <a class="paperlist-avatar" target="_blank" href="https://os.copernicus.org/articles/19/1669/2023/os-19-1669-2023-avatar-web.png"> <img class="img-responsive" src="https://os.copernicus.org/articles/19/1669/2023/os-19-1669-2023-avatar-thumb80.png" data-web="https://os.copernicus.org/articles/19/1669/2023/os-19-1669-2023-avatar-web.png" data-width="600" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-height="322" width="80" height="80"> </a> </div> </div> <div class="grid-container paperlist-object in-range paperList-final" data-diff="0"> <div class="grid-100 hide-on-desktop hide-on-tablet"> <a class="paperlist-avatar" target="_blank" href="https://os.copernicus.org/articles/19/1595/2023/os-19-1595-2023-avatar-web.png"> <img class="img-responsive" src="https://os.copernicus.org/articles/19/1595/2023/os-19-1595-2023-avatar-thumb80.png" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-web="https://os.copernicus.org/articles/19/1595/2023/os-19-1595-2023-avatar-web.png" data-width="600" data-height="391" width="80" height="80"> </a> </div> <div class="grid-85 tablet-grid-85"> <div class="published-date"> 22 Nov 2023</div> <a class="article-title" target="_parent" href="https://os.copernicus.org/articles/19/1595/2023/">Southern Ocean warming and Antarctic ice shelf melting in conditions plausible by late 23rd century in a high-end scenario</a> <div class="authors">Pierre Mathiot and Nicolas C. Jourdain</div> <div class="citation">Ocean Sci., 19, 1595–1615, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/os-19-1595-2023,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/os-19-1595-2023,</span> 2023</div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_113215" data-show=".short_summary_113215" data-hide=".short_summary_button_113215" >Short summary</span> <span class="show-hide journal-contentLinkColor triangle ce_comment_button_113215 ml-2" data-show=".ce_comment_113215" data-hide=".ce_comment_button_113215">Co-editor-in-chief</span> <div class="j-widget__max short_summary short_summary_113215" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> How much the Antarctic ice shelf basal melt rate can increase in response to global warming remains an open question. To achieve this, we compared an ocean simulation under present-day atmospheric condition to a one under late 23rd century atmospheric conditions. The ocean response to the perturbation includes a decrease in the production of cold dense water and an increased intrusion of warmer water onto the continental shelves. This induces a substantial increase in ice shelf basal melt rates. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_113215" data-show=".short_summary_button_113215">Hide</a></div> </div> </div> <div class="j-widget__max ce_comment ce_comment_113215 mt-3" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Co-editor-in-chief</div> <div class="content"> Future climate of the Antarctic is a topic of concern to scientists and to the general public, and has implications for global sea level rise. This paper uses an ocean model driven by high-end atmospheric conditions plausible by late 23rd century to highlight what might happen to the Antarctic ice and its surrounding ocean if our emissions of CO2 continue to rise in an extreme way. The model suggests that the future Antarctic continental shelf would be more like the present day Amundsen Sea – warmer and fresher. This would lead to substantial increases in ice shelf melt rates. </div> <div><a href="#" class="show-hide triangle" data-hide=".ce_comment_113215" data-show=".ce_comment_button_113215">Hide</a></div> </div> </div> </div> <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> <a class="paperlist-avatar" target="_blank" href="https://os.copernicus.org/articles/19/1595/2023/os-19-1595-2023-avatar-web.png"> <img class="img-responsive" src="https://os.copernicus.org/articles/19/1595/2023/os-19-1595-2023-avatar-thumb80.png" data-web="https://os.copernicus.org/articles/19/1595/2023/os-19-1595-2023-avatar-web.png" data-width="600" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-height="391" width="80" height="80"> </a> </div> </div> <div class="grid-container paperlist-object in-range paperList-final" data-diff="0"> <div class="grid-100 hide-on-desktop hide-on-tablet"> <a class="paperlist-avatar" target="_blank" href="https://os.copernicus.org/articles/19/941/2023/os-19-941-2023-avatar-web.png"> <img class="img-responsive" src="https://os.copernicus.org/articles/19/941/2023/os-19-941-2023-avatar-thumb80.png" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-web="https://os.copernicus.org/articles/19/941/2023/os-19-941-2023-avatar-web.png" data-width="600" data-height="313" width="80" height="80"> </a> </div> <div class="grid-85 tablet-grid-85"> <div class="published-date"> 28 Jun 2023</div> <a class="article-title" target="_parent" href="https://os.copernicus.org/articles/19/941/2023/">Dense water formation in the eastern Mediterranean under a global warming scenario</a> <div class="authors">Iván M. Parras-Berrocal, Rubén Vázquez, William Cabos, Dimitry V. Sein, Oscar Álvarez, Miguel Bruno, and Alfredo Izquierdo</div> <div class="citation">Ocean Sci., 19, 941–952, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/os-19-941-2023,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/os-19-941-2023,</span> 2023</div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_109351" data-show=".short_summary_109351" data-hide=".short_summary_button_109351" >Short summary</span> <span class="show-hide journal-contentLinkColor triangle ce_comment_button_109351 ml-2" data-show=".ce_comment_109351" data-hide=".ce_comment_button_109351">Co-editor-in-chief</span> <div class="j-widget__max short_summary short_summary_109351" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Global warming may strongly affect dense water formation in the eastern Mediterranean, potentially impacting basin circulation and water properties. We find that at the end of the century dense water formation is reduced by 75 % for the Adriatic, 84 % for the Aegean, and 83 % for the Levantine Sea. This reduction is caused by changes in the temperature and salinity of surface and intermediate waters, which strengthen the vertical stratification, hampering deep convection. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_109351" data-show=".short_summary_button_109351">Hide</a></div> </div> </div> <div class="j-widget__max ce_comment ce_comment_109351 mt-3" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Co-editor-in-chief</div> <div class="content"> This research predicts the potential future of the Eastern Mediterranean's circulation under the RCP8.5 emission scenario, using a coupled regional climate system model and a global oceanic model. The study predicts a significant decrease in dense water formation, a key process in Mediterranean overturning circulation, by up to 84% in the Adriatic, Aegean, and Levantine seas by the end of the century. This study forecasts a shift in the main source of Eastern Mediterranean Deep Water from the Adriatic Sea to the Aegean Sea. These changes, related to increased vertical stratification that hinders vertical mixing and convection, fill a crucial gap in our understanding of how climate change could reshape the Mediterranean Sea's dynamics. </div> <div><a href="#" class="show-hide triangle" data-hide=".ce_comment_109351" data-show=".ce_comment_button_109351">Hide</a></div> </div> </div> </div> <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> <a class="paperlist-avatar" target="_blank" href="https://os.copernicus.org/articles/19/941/2023/os-19-941-2023-avatar-web.png"> <img class="img-responsive" src="https://os.copernicus.org/articles/19/941/2023/os-19-941-2023-avatar-thumb80.png" data-web="https://os.copernicus.org/articles/19/941/2023/os-19-941-2023-avatar-web.png" data-width="600" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-height="313" width="80" height="80"> </a> </div> </div> <p class="j-news-archive-link grid-container grid-parent"> <strong> <a class="grid-30 tablet-grid-30 mobile-grid-100" href="https://www.ocean-science.net/articles_and_preprints/highlight_articles.html">More highlight articles <img cofileid="17978" alt="" src="https://www.ocean-science.net/graphic_grey_right_symbol.png"></a> <a class="grid-30 tablet-grid-30 mobile-grid-100 a-margin__left-2" target="_blank" href="https://www.egu.eu/news/highlight-articles/">All EGU highlight articles <img cofileid="17978" alt="" src="https://www.ocean-science.net/graphic_grey_right_symbol.png"></a> </strong> </p> </div>    </div><div id="special-issues-scheduled-content" class="cmsbox "> <div id="special-issues-header"><h2>Scheduled special issues</h2></div> <div class="grid-container grid-parent"> <div class="grid-100 tablet-grid-100 mobile-grid-100 grid-parent" id="chronologically"> <div class="grid-container grid-parent special-issue triangle_special_issues"> <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> <a href="javascript:void(0);" class="show-hide" data-toggle="#info-chronologically-content-1325,#info-chronologically-link-1325" data-duration="300"> Biogeochemical processes and Air–sea exchange in the Sea-Surface microlayer </a> (BG/OS inter-journal SI) </div> <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 01 Oct 2024–31 Jul 2025 | Sanja Frka (Rudjer Boskovic Institute, Croatia), Peter S. Liss (University of East Anglia, United Kingdom), Klaus Jürgens (Leibniz Institute for Baltic Sea Research, Germany), and Xinping Hu (Texas A&M University – Corpus Christi, United States) | <a href="javascript:void(0);" class="info-link show-hide" id="info-chronologically-link-1325" data-show="#info-chronologically-content-1325" data-hide="#info-chronologically-link-1325">Information</a> </div> <div class="j-widget__max short_summary" id="info-chronologically-content-1325" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Information</div> <div class="content" id="1325"> Over the last 2 decades, studies have shown that the sea-surface microlayer covers large areas of the global ocean and, under certain conditions, can even form biofilm-like (and thus unique) habitats between the ocean and the atmosphere. Due to its recurrent biofilm-like features and unique position at the atmosphere–ocean interface, the microlayer is central to a range of global biogeochemical and climate-related processes, including marine carbon cycling, air–sea gas exchange, physical surface processes, and aerosol production. Despite the fact that processes occurring in and across the microlayer have received increasing attention during recent years, our knowledge about the microlayer remains rudimentary. New approaches and technologies have been developed to understand the formation and function of the microlayer on a mechanistic level. For example, the BASS (Biogeochemical processes and Air–sea exchange in the Sea-Surface microlayer; <a href="https://uol.de/en/bass"target="_blank">https://uol.de/en/bass</a>) group has been funded to explore the significance of the microlayer as a bio- and photochemical reactor in an unprecedented comprehensive and interdisciplinary approach, and BASS findings will contribute to this special issue (SI). The purpose of the SI is twofold: (1) to present outcomes of a BASS mesocosm study and (2) to present further contributions on the microlayer from the wider research community based on field, mesocosm, modelling, and laboratory studies. This SI will bring together the latest scientific studies to describe the microlayer as an interface between the ocean and atmosphere across different disciplines. </div> <div class="row"> <div class="col-auto"> <a href="#" class="show-hide triangle" data-hide="#info-chronologically-content-1325" data-show="#info-chronologically-link-1325">Hide</a> </div> <div class="col text-right"> <a class="si-mobile-native-share" href="#" data-title="Biogeochemical processes and Air–sea exchange in the Sea-Surface microlayer" data-url="" data-id="1325" style="display: none;"> <i class="fas fa-lg fa-share-alt"></i> </a> <a class="desktop-share" href="#" data-title="Biogeochemical processes and Air–sea exchange in the Sea-Surface microlayer" data-url="" data-id="1325" title="Copy to clipboard"> <i class="fas fa-lg fa-share-alt"></i> </a> </div> </div> </div> </div> </div> <div class="grid-container grid-parent special-issue triangle_special_issues"> <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> <a href="javascript:void(0);" class="show-hide" data-toggle="#info-chronologically-content-1345,#info-chronologically-link-1345" data-duration="300"> Special issue on ocean extremes (55th International Liége Colloquium) </a> </div> <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 15 Sep 2024–15 Sep 2025 | Matjaz Licer, Mélanie Juza, Thomas Froelicher, Serena Zunino, Antonio Ricchi, Yonggang Liu, Aida Alvera-Azcárate, Andrea Piñones, and OS editors | <a href="javascript:void(0);" class="info-link show-hide" id="info-chronologically-link-1345" data-show="#info-chronologically-content-1345" data-hide="#info-chronologically-link-1345">Information</a> </div> <div class="j-widget__max short_summary" id="info-chronologically-content-1345" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Information</div> <div class="content" id="1345"> <p>Marine extreme events, encompassing phenomena such as storm surges, marine heatwaves, biogeochemical extremes, harmful algal blooms, jellyfish blooms, extreme storms, and even unique occurrences like medicanes (Mediterranean hurricanes), are becoming more common. These events have profound consequences for marine ecosystems, coastal communities, and global economies. Extreme sea level events, driven by intense storms and rising sea levels, can inundate coastlines, leading to devastating flooding and erosion. Marine heatwaves, fuelled by climate change, can trigger mass coral bleaching events, disrupting delicate marine ecosystems and jeopardizing the biodiversity that they support. Harmful algal blooms and jellyfish blooms, exacerbated by nutrient pollution and warmer waters, can lead to oxygen depletion, cause mass mortality events in various species, and pose risks to human health. The concurrence of oceanic and atmospheric extremes, marine and atmospheric heat waves, wind and wave extremes, harmful algal blooms, hypoxic conditions, and high-acidity events may lead to a nonlinear increase in environmental stress.</p> <p>Addressing the impacts of these events requires a comprehensive approach, involving measures to mitigate climate change, improve coastal resilience, and promote sustainable marine management practices. A crucial aspect of addressing and mitigating the impacts of marine extreme events lies in deepening our scientific understanding of these phenomena and in establishing solid methodologies for defining climatological baselines and for extreme analyses in a changing climate. Scientific research plays a pivotal role in unravelling the intricate mechanisms behind these events, predicting their occurrence, and formulating effective strategies to manage and adapt to their consequences. By exploring the underlying causes, interactions, and feedback loops, scientists can provide invaluable insights that guide policymakers, communities, and industries in making informed decisions.</p> </div> <div class="row"> <div class="col-auto"> <a href="#" class="show-hide triangle" data-hide="#info-chronologically-content-1345" data-show="#info-chronologically-link-1345">Hide</a> </div> <div class="col text-right"> <a class="si-mobile-native-share" href="#" data-title="Special issue on ocean extremes (55th International Liége Colloquium)" data-url="" data-id="1345" style="display: none;"> <i class="fas fa-lg fa-share-alt"></i> </a> <a class="desktop-share" href="#" data-title="Special issue on ocean extremes (55th International Liége Colloquium)" data-url="" data-id="1345" title="Copy to clipboard"> <i class="fas fa-lg fa-share-alt"></i> </a> </div> </div> </div> </div> </div> <div class="grid-container grid-parent special-issue triangle_special_issues"> <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> <a href="https://os.copernicus.org/articles/special_issue1334.html">Advances in ocean science from underwater gliders</a> </div> <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 14 Aug 2024–31 Dec 2025 | Charitha Pattiaratchi (University of Western Australia, Australia), Annunziata Pirro (National Institute of Oceanography and Applied Geophysics, Italy), Filipa Carvalho (National Oceanography Centre, United Kingdom), Ilker Fer (University of Bergen, Norway), Luc Rainville (University of Washington, United States), and OS editors | <a href="javascript:void(0);" class="info-link show-hide" id="info-chronologically-link-1334" data-show="#info-chronologically-content-1334" data-hide="#info-chronologically-link-1334">Information</a> </div> <div class="j-widget__max short_summary" id="info-chronologically-content-1334" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Information</div> <div class="content" id="1334"> <p>Over the past 25 years autonomous underwater gliders have progressed from experimental vehicles through scientific instruments to operational tools. Observations from gliders are now enhancing our understanding of physical, biogeochemical, and biological oceanographic processes. They represent a mature technology and complement traditional ocean sampling capabilities, especially for sustained real-time oceanographic measurements. They are now used as standard research tools in sustainable ocean observations and process studies, collecting measurements of physical, chemical, and bio-optical ocean variables. Underwater gliders have unique capacities to connect open-ocean and coastal processes and to sample the ocean at regional scales during multi-month missions. Gliders have been routinely deployed to monitor the ocean, for example monitoring continental shelves, boundary currents, and polar regions including in under-ice operations. More recently gliders have contributed to environmental hazard detection such as in the detection of marine heat waves and hurricane prediction.</p> <p>This special issue has been stimulated by the International Underwater Glider Conference (IUGC) that was held in Gothenburg in June 2024, but submissions are open to everyone regardless of participation in the conference.</p> <p>We invite papers advancing knowledge on the ocean's physical, biogeochemical, and ecosystem properties and processes by using underwater gliders and/or by their combined use with other observing platforms or numerical models. Contributions on technological aspects such as the development of glider sensors are welcome provided they include some ocean science advance.</p> </div> <div class="row"> <div class="col-auto"> <a href="#" class="show-hide triangle" data-hide="#info-chronologically-content-1334" data-show="#info-chronologically-link-1334">Hide</a> </div> <div class="col text-right"> <a class="si-mobile-native-share" href="#" data-title="Advances in ocean science from underwater gliders" data-url="https://os.copernicus.org/articles/special_issue1334.html" data-id="1334" style="display: none;"> <i class="fas fa-lg fa-share-alt"></i> </a> <a class="desktop-share" href="#" data-title="Advances in ocean science from underwater gliders" data-url="https://os.copernicus.org/articles/special_issue1334.html" data-id="1334" title="Copy to clipboard"> <i class="fas fa-lg fa-share-alt"></i> </a> </div> </div> </div> </div> </div> <div class="grid-container grid-parent special-issue triangle_special_issues"> <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> <a href="https://os.copernicus.org/articles/special_issue1276.html">Ocean Science Jubilee: reviews and perspectives</a> </div> <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 01 Aug 2023–30 Jun 2025 | OS editors | Coordinator: Karen J. Heywood | <a href="javascript:void(0);" class="info-link show-hide" id="info-chronologically-link-1276" data-show="#info-chronologically-content-1276" data-hide="#info-chronologically-link-1276">Information</a> </div> <div class="j-widget__max short_summary" id="info-chronologically-content-1276" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Information</div> <div class="content" id="1276"> In 2024–2025 Ocean Science will be 20 years old, during which time it has been internationally at the forefront of high-quality, open-access, and open-peer-review publishing in our field of science. To celebrate this jubilee, we are publishing a special collection of “reviews and perspectives” papers, looking back at how ocean sciences have advanced over the last 20 years and looking forward to how they might advance over the next 20 years. The Ocean Science Jubilee special issue will be a compilation of influential papers across the broad range of ocean science topics covered by the journal. Accepted reviews and perspectives papers may also be included in the <a href="https://encyclopedia-of-geosciences.net/"target="_blank">https://encyclopedia-of-geosciences.net/</a>. <br /><br /> Submission of reviews and perspectives papers is open to everyone. We welcome the perspectives of early-career scientists. You do not have to be invited to submit a paper to the special issue. Reviews and perspectives papers are welcome on any topic and discipline within ocean sciences, as with any paper in Ocean Science. Manuscripts will undergo the usual rigorous and open peer review. </div> <div class="row"> <div class="col-auto"> <a href="#" class="show-hide triangle" data-hide="#info-chronologically-content-1276" data-show="#info-chronologically-link-1276">Hide</a> </div> <div class="col text-right"> <a class="si-mobile-native-share" href="#" data-title="Ocean Science Jubilee: reviews and perspectives" data-url="https://os.copernicus.org/articles/special_issue1276.html" data-id="1276" style="display: none;"> <i class="fas fa-lg fa-share-alt"></i> </a> <a class="desktop-share" href="#" data-title="Ocean Science Jubilee: reviews and perspectives" data-url="https://os.copernicus.org/articles/special_issue1276.html" data-id="1276" title="Copy to clipboard"> <i class="fas fa-lg fa-share-alt"></i> </a> </div> </div> </div> </div> </div> <div class="grid-container grid-parent special-issue triangle_special_issues"> <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> <a href="https://os.copernicus.org/articles/special_issue365_1241.html">Development and deployment of regional ocean configurations for Modular Ocean Model 6 (MOM6)</a> (GMD/OS inter-journal SI) </div> <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 01 Jan 2023–indefinite | OS editors | Coordinator: Charles Stock | <a href="javascript:void(0);" class="info-link show-hide" id="info-chronologically-link-1241" data-show="#info-chronologically-content-1241" data-hide="#info-chronologically-link-1241">Information</a> </div> <div class="j-widget__max short_summary" id="info-chronologically-content-1241" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Information</div> <div class="content" id="1241"> This special issue describes efforts establishing high-resolution regional ocean and biogeochemical modelling capabilities for Modular Ocean Model 6 (MOM6) and selected initial applications. MOM is amongst the most widely used ocean models for global climate and earth system applications, with a lineage of scientific contributions exceeding 50 years. MOM6 represents an ambitious evolution of previous MOM formulations, embracing numerous recent modelling advances and an open development approach. MOM6 and its associated biogeochemical components have been successfully deployed for the Sixth Coupled Model Intercomparison Project (CMIP6) and other international global climate and ocean prediction efforts. The resolution and regional optimality of global simulations, however, are inevitably limited by the computational, forcing, and parameterization demands of global climate-scale simulations. Ocean modelling frameworks capable of simulating and connecting physical, biogeochemical, and ecosystem processes from ocean basins to coasts and estuaries are needed to understand the role of oceans in global change and to anticipate global change impacts on marine ecosystems and coastal communities. Development of robust regional modelling capabilities for MOM6 (i.e. <q>regional MOM6</q>) creates such a framework, but the extension of MOM6 to high-resolution regional applications presents many challenges. <br /><br /> The papers in this collection present the overall design and implementation of regional MOM6, describe new parameterizations intended for regional applications, present a first generation of regional MOM6 configurations from across the global ocean, and offer select initial applications in ocean science. Advances in horizontal grid generation and boundary condition formulation are highlighted, including those enabling a more seamless transmission of physical and biogeochemical information from global to regional scales and those required to handle flexible Lagrangian vertical coordinates. The robustness of physical and biogeochemical configurations and parameterizations – many of which were developed for global applications – is explored in higher-resolution implementations spanning environments from the Arctic to equatorial waters. Analysis of tradeoffs between model skill and computational cost highlights algorithmic improvements critical for producing decision-relevant ensembles that span a range of ocean futures. The collected works provide a foundation for the expanded application of regional MOM6 to understand and predict ocean conditions across scales. <br /><br /> This is a <q>traditional style</q> special issue open to all papers within the topic. We anticipate that contributions will be primarily to GMD initially but that there will be a growing number of applications suitable for OS once the core development papers have been published. The indefinite ending date will allow for a greater number of initial applications to be published in OS and enable eventual documentation of <q>generational updates</q> planned for some configurations. </div> <div class="row"> <div class="col-auto"> <a href="#" class="show-hide triangle" data-hide="#info-chronologically-content-1241" data-show="#info-chronologically-link-1241">Hide</a> </div> <div class="col text-right"> <a class="si-mobile-native-share" href="#" data-title="Development and deployment of regional ocean configurations for Modular Ocean Model 6 (MOM6)" data-url="https://os.copernicus.org/articles/special_issue365_1241.html" data-id="1241" style="display: none;"> <i class="fas fa-lg fa-share-alt"></i> </a> <a class="desktop-share" href="#" data-title="Development and deployment of regional ocean configurations for Modular Ocean Model 6 (MOM6)" data-url="https://os.copernicus.org/articles/special_issue365_1241.html" data-id="1241" title="Copy to clipboard"> <i class="fas fa-lg fa-share-alt"></i> </a> </div> </div> </div> </div> </div> </div> </div> <script> $(function (){ if(!navigator.share){ $('.si-mobile-native-share').hide(); $('.desktop-share').show(); } else { $('.si-mobile-native-share').show(); $('.desktop-share').hide(); } $('.si-mobile-native-share').click((event) => { event.stopPropagation(); event.preventDefault(); event.stopImmediatePropagation(); let element = event.currentTarget; if (navigator.share) { let url = window.getUrl(element); navigator.share({ title: $(element).attr('data-title'), text: '', url: url, }).then(() => { console.log('Successful share'); return false; }) .catch((error) => { console.log('Error sharing', error); return false; }); } return false; }); $('.desktop-share').click((event) => { event.stopPropagation(); event.preventDefault(); event.stopImmediatePropagation(); let element = event.currentTarget; let url = window.getUrl(element); window.updateClipboard(url); return false; }); }); /** * Method for copy something to clipboard * @param newClip */ window.updateClipboard = function (newClip) { if (navigator.clipboard) { navigator.clipboard.writeText(newClip).then(function () { }, function (err) { console.warn('Error during copying to clipboard: ', err.toString()); }); } return false; }; window.getUrl = function (element){ let dataUrl = $(element).attr('data-url'); if(typeof dataUrl !== 'undefined' && dataUrl.length > 0) { return dataUrl } else { let id = $(element).attr('data-id'); return window.location.href + '#' + id; } } </script> </div><div id="recent_paper" class="cmsbox j-article j-article-section"><div id="recent-paper-content"> <div id="recent_paper_header"> <h2>Recent papers</h2> </div> <div class="grid-container paperlist-object type-0 in-range paperList-discussion" data-diff="0"> <div class="grid-100 hide-on-desktop hide-on-tablet"> </div> <div class="grid-85 tablet-grid-85"> <div class="published-date"> 20 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3560/">On the response of the Equatorial Atmosphere and Ocean to changes in Sea Surface Temperature along the Path of the North Equatorial Counter Current</a> <div class="authors">David John Webb</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3560,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3560,</span> 2024</div> <div class="statusMessage"><span>Preprint under review for OS</span> <nobr>(discussion: open, 0 comments)</nobr></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_125093" data-show=".short_summary_125093" data-hide=".short_summary_button_125093" >Short summary</span> <div class="j-widget__max short_summary short_summary_125093" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> A modern climate model is used to test the hypothesis that changes observed during El Niños are, in part, forced by changes in the temperature of the North Equatorial Counter Current. This is a warm current that flows eastwards across the Pacific, a few degrees north of the Equator, close to the Inter-Tropical Convection Zone, a major region of deep atmospheric convection. The tests generate a significant El Niño type response in the ocean, giving confidence that the hypothesis is correct. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_125093" data-show=".short_summary_button_125093">Hide</a></div> </div> </div> </div> <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> </div> </div> <div class="grid-container paperlist-object type-0 in-range paperList-discussion" data-diff="0"> <div class="grid-100 hide-on-desktop hide-on-tablet"> </div> <div class="grid-85 tablet-grid-85"> <div class="published-date"> 20 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3403/">Coastal circulation and eddies generation in the Southwest Mexican Pacific</a> <div class="authors">Federico Angel Velázquez-Muñoz, Raúl Candelario Cruz-Gómez, and Cesar Monzon</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3403,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3403,</span> 2024</div> <div class="statusMessage"><span>Preprint under review for OS</span> <nobr>(discussion: open, 0 comments)</nobr></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124551" data-show=".short_summary_124551" data-hide=".short_summary_button_124551" >Short summary</span> <div class="j-widget__max short_summary short_summary_124551" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We identify the Mexican Coastal Current interaction with coastline using sea level anomaly and derived geostrophic velocities, finding that an average width of 95 km and an average speed of 0.3 m/s width seasonal variability. Numerical modeling proves that interaction of coastal current with the coastline generates ocean eddies in some places that form a wide concavity. These eddies are formed while the current is present getting intense and detaching from the coast until the current weakens. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124551" data-show=".short_summary_button_124551">Hide</a></div> </div> </div> </div> <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> </div> </div> <div class="grid-container paperlist-object in-range paperList-final" data-diff="0"> <div class="grid-100 hide-on-desktop hide-on-tablet"> <a class="paperlist-avatar" target="_blank" href="https://os.copernicus.org/articles/20/1479/2024/os-20-1479-2024-avatar-web.png"> <img class="img-responsive" src="https://os.copernicus.org/articles/20/1479/2024/os-20-1479-2024-avatar-thumb80.png" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-web="https://os.copernicus.org/articles/20/1479/2024/os-20-1479-2024-avatar-web.png" data-width="516" data-height="600" width="80" height="80"> </a> </div> <div class="grid-85 tablet-grid-85"> <div class="published-date"> 18 Nov 2024</div> <a class="article-title" target="_parent" href="https://os.copernicus.org/articles/20/1479/2024/">Turbulent features of nearshore wave–current flow</a> <div class="authors">Massimiliano Marino, Carla Faraci, Bjarne Jensen, and Rosaria Ester Musumeci</div> <div class="citation">Ocean Sci., 20, 1479–1493, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/os-20-1479-2024,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/os-20-1479-2024,</span> 2024</div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_120897" data-show=".short_summary_120897" data-hide=".short_summary_button_120897" >Short summary</span> <div class="j-widget__max short_summary short_summary_120897" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Understanding how waves and currents interact helps us comprehend physical processes occurring in a coastal environment. In the present work, waves and currents were reproduced in the laboratory and flow velocities were measured. Results showed that the superposition of waves induces a cyclic enhancement or suppression of near-bed turbulence, and, depending on current velocity, wave orbital velocity, and bed roughness, waves can alter the current velocity, following highly nonlinear patterns. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_120897" data-show=".short_summary_button_120897">Hide</a></div> </div> </div> </div> <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> <a class="paperlist-avatar" target="_blank" href="https://os.copernicus.org/articles/20/1479/2024/os-20-1479-2024-avatar-web.png"> <img class="img-responsive" src="https://os.copernicus.org/articles/20/1479/2024/os-20-1479-2024-avatar-thumb80.png" data-web="https://os.copernicus.org/articles/20/1479/2024/os-20-1479-2024-avatar-web.png" data-width="516" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-height="600" width="80" height="80"> </a> </div> </div> <div class="grid-container paperlist-object type-0 in-range paperList-discussion" data-diff="0"> <div class="grid-100 hide-on-desktop hide-on-tablet"> </div> <div class="grid-85 tablet-grid-85"> <div class="published-date"> 14 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3436/">Effect of double diffusion processes in the deep ocean on the distribution and dynamics of particulate and dissolved matter: a case study in Tyrrhenian Sea</a> <div class="authors">Xavier Durrieu de Madron, Paul Blin, Mireille Pujo-Pay, Vincent Taillandier, and Pascal Conan</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3436,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3436,</span> 2024</div> <div class="statusMessage"><span>Preprint under review for OS</span> <nobr>(discussion: open, 0 comments)</nobr></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124675" data-show=".short_summary_124675" data-hide=".short_summary_button_124675" >Short summary</span> <div class="j-widget__max short_summary short_summary_124675" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This study investigated the effects of salt fingering on particle and solute distribution in the Tyrrhenian Sea. Density interfaces associated with thermohaline staircases slow the settling of suspended particles and promote aggregation. This affects particle size distribution and creates nutrient and oxygen gradients, affecting microbial activity and nutrient cycling. The research highlights the potential role of salt fingers in deep ocean biogeochemical processes. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124675" data-show=".short_summary_button_124675">Hide</a></div> </div> </div> </div> <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> </div> </div> <div class="grid-container paperlist-object type-0 in-range paperList-discussion" data-diff="0"> <div class="grid-100 hide-on-desktop hide-on-tablet"> </div> <div class="grid-85 tablet-grid-85"> <div class="published-date"> 13 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3380/">Application of quality-controlled sea level height observation at the central East China Sea: Assessment of sea level rise</a> <div class="authors">Taek-Bum Jeong, Yong Sun Kim, Hyeonsoo Cha, Kwang-Young Jeong, Mi-Jin Jang, Jin-Yong Jeong, and Jae-Ho Lee</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3380,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3380,</span> 2024</div> <div class="statusMessage"><span>Preprint under review for OS</span> <nobr>(discussion: open, 0 comments)</nobr></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124507" data-show=".short_summary_124507" data-hide=".short_summary_button_124507" >Short summary</span> <div class="j-widget__max short_summary short_summary_124507" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This study presents a new method to improve the accuracy of sea level height from the Ieodo Ocean Research Station in the East China Sea. The method helps identify data errors, such as repeated or unusual values, and flags extreme weather events. The analysis found that sea level rise are mostly due to ocean mass changes, with local ground subsidence also playing a role. This high-quality data supports research on short-term and long-term events, helping coastal monitoring and planning efforts. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124507" data-show=".short_summary_button_124507">Hide</a></div> </div> </div> </div> <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> </div> </div> </div>    </div><div id="cmsbox_285981" class="cmsbox "><h2>Notice on the current situation in Ukraine</h2> <div class="co-notification"><p>To show our support for Ukraine, all fees for papers from authors (first or corresponding authors) affiliated to <strong>Ukrainian institutions</strong> are automatically waived, regardless if these papers are co-authored by scientists affiliated to Russian and/or Belarusian institutions. The only exception will be if the corresponding author or first contact (contractual partner of Copernicus) are from a Russian and/or Belarusian institution, in that case the APCs are not waived.</p> <p>In accordance with current European restrictions, Copernicus Publications does not step into business relations with and issue APC-invoices (articles processing charges) to <strong>Russian and Belarusian institutions</strong>. The peer-review process and scientific exchange of our journals including preprint posting is not affected. However, these restrictions require that the first contact (contractual partner of Copernicus) has an affiliation and invoice address outside Russia or Belarus.</p> </div></div><div id="essentential-logos-carousel" class="cmsbox "><ul class="essentential-logos no-styling"> <li class="essentential-logo"> <a href="https://www.ocean-science.net/policies/licence_and_copyright.html" title="CC BY 4.0" alt="CC BY 4.0" target="_self" class="essential-logo__link"><img src="https://www.ocean-science.net/ejl_CC-BY-40.svg" alt="CC BY 4.0" cofileid="19671" class="essential-logo__media"/></a> <a href="http://creativecommons.org/licenses/by/3.0/" title="license CC BY 4.0 " alt="license CC BY 4.0 " target="_blank" class="essential-logo__link-hidden" rel="license">CC BY 4.0</a> </li> <li class="essentential-logo"> <a href="https://publications.copernicus.org/services/journal_metrics.html" title="Clarivate Analytics" alt="Clarivate Analytics" target="_blank" class="essential-logo__link"><img 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