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} #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 row"> <div class="col"> <div class="level2Toc"> <div class="grid-container"> <div class="grid-100"> <div class="tab co-angel-left hide-on-desktop"></div> <div class="tab co-angel-right hide-on-desktop"></div> <div class="mobile-citation"> <ul class="tab-navigation no-styling"> <li class="tab0.recent active"><nobr><a href="https://egusphere.copernicus.org/preprints/recent_papers.html">Recently posted</a></nobr></li><li class="tab5.byTopics hide-on-mobile"><nobr><a href="https://egusphere.copernicus.org/preprints/by_topics.html">By topics</a></nobr></li><li class="tab7.mostDownloaded"><nobr><a href="https://egusphere.copernicus.org/preprints/most_downloaded.html">Most downloaded</a></nobr></li><li class="tab8.mostCommented"><nobr><a href="https://egusphere.copernicus.org/preprints/most_commented.html">Most commented</a></nobr></li><li class="tab100.discussion"><nobr><a href="https://egusphere.copernicus.org/preprints/preprints.html">Preprint overview</a></nobr></li> </ul> </div> </div> </div> <div class="row no-gutters auto-fixed-top-forced"> <div class="col-12 mb-3 hide-on-fixed"> <div class="row no-gutters"> <div class="col-12"> The following lists the preprints posted within the last 10 days. </div> </div> </div> <div class="col-12 hide-on-fixed"> </div> <div class="col-12 pb-3 show-on-fixed recent-selection-wrapper" style="display:none;"> <button type="button" class="btn btn-primary">Filters</button> </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"> 27 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3377/">Multi-centennial climate change in a warming world beyond 2100</a> <div class="authors">Sun-Seon Lee, Sahil Sharma, Nan Rosenbloom, Keith B. Rodgers, Ji-Eun Kim, Eun Young Kwon, Christian L. E. Franzke, In-Won Kim, Mohanan Geethalekshmi Sreeush, and Karl Stein</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3377,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3377,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124498" data-show=".short_summary_124498" data-hide=".short_summary_button_124498" >Short summary</span> <div class="j-widget__max short_summary short_summary_124498" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This study presents a 10-member extension from 2101 to 2500 of the CESM2-LE, under a scenario aiming for zero fossil fuel emissions by 2250. Key findings include a 12 °C warming, a 23.5 % rise in precipitation, and diminished ENSO variability. Substantial carbon release from thawing permafrost will shift land from a carbon sink to a source. The ocean’s CO<sub>2</sub> absorption capacity will decline, emphasizing the extensive impacts of long-term climate change on ecosystems and human societies. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124498" data-show=".short_summary_button_124498">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"> 27 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3313/">Aquatic and Soil CO<sub>2</sub> Emissions from forested wetlands of Congo's Cuvette Centrale</a> <div class="authors">Antoine de Clippele, Astrid C. H. Jaeger, Simon Baumgartner, Marijn Bauters, Pascal Boeckx, Clement Botefa, Glenn Bush, Jessica Carilli, Travis W. Drake, Christian Ekamba, Gode Lompoko, Nivens Bey Mukwiele, Kristof Van Oost, Roland A. Werner, Joseph Zambo, Johan Six, and Matti Barthel</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3313,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3313,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124376" data-show=".short_summary_124376" data-hide=".short_summary_button_124376" >Short summary</span> <div class="j-widget__max short_summary short_summary_124376" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Tropical forest soils as a large terrestrial source of carbon dioxide (CO<sub>2</sub>) contribute to the GHG budgets. Despite this, carbon flux data from forested wetlands is scarce in tropical Africa. The study presents three years of semi-continuous measurements of surface CO<sub>2</sub> fluxes within the Congo Basin. Although no seasonal patterns were evident, our results showed a positive effect of soil temperature and soil moisture, while a quadratic relationship was observed with the water table level. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124376" data-show=".short_summary_button_124376">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"> 27 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3343/">Calcium is associated with specific soil organic carbon decomposition products</a> <div class="authors">Mike C. Rowley, Jasquelin Pena, Matthew A. Marcus, Rachel Porras, Elaine Pegoraro, Cyrill Zosso, Nicholas O. E. Ofiti, Guido L. B. Wiesenberg, Michael W. I. Schmidt, Margaret S. Torn, and Peter S. Nico</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3343,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3343,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124443" data-show=".short_summary_124443" data-hide=".short_summary_button_124443" >Short summary</span> <div class="j-widget__max short_summary short_summary_124443" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This study shows calcium helps to preserve soil organic carbon in acidic soils, challenging previous beliefs that their interactions were largely limited to alkaline soils. Using spectromicroscopy, we found calcium is co-located with aromatic and phenolic-rich carbon and that this association was disrupted when the calcium was removed, and only reformed during decomposition with added calcium. This suggests that calcium amendments could enhance soil organic carbon stability. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124443" data-show=".short_summary_button_124443">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"> 27 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-2888/">Improving the fine structure of intense rainfall forecast by a designed adversarial generation network</a> <div class="authors">Zuliang Fang, Qi Zhong, Haoming Chen, Xiuming Wang, Zhicha Zhang, and Hongli Liang</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-2888,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-2888,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123400" data-show=".short_summary_123400" data-hide=".short_summary_button_123400" >Short summary</span> <div class="j-widget__max short_summary short_summary_123400" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We developed a deep learning model based on Generative Adversarial Networks (GANs) to improve rainfall forecasts in northern China. Traditional models struggle with accuracy, especially for heavy rain. Our model merges data from multiple forecasts, capturing detailed rainfall patterns and offering more reliable short-term predictions. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123400" data-show=".short_summary_button_123400">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"> 27 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3592/">Topographic stresses affect stress changes caused by megathrust earthquakes and condition aftershock seismicity in forearcs: Insights from mechanical models and the Tohoku-Oki and Maule earthquakes</a> <div class="authors">Armin Dielforder, Gian Maria Bocchini, and Andrea Hampel</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3592,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3592,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_125151" data-show=".short_summary_125151" data-hide=".short_summary_button_125151" >Short summary</span> <div class="j-widget__max short_summary short_summary_125151" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Subduction zones feature a large elevation difference between the deep oceanic trench and the high mountains on land, which causes stresses in the upper plate. We investigate how these topographic stresses affect the aftershock seismicity of large subduction earthquakes using analytical and numerical stress models. We show that topographic stresses have a large influence on aftershock seismicity and promoted most of the seismicity after the Tohoku-Oki (Japan) and Maule (Chile) earthquakes. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_125151" data-show=".short_summary_button_125151">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"> 27 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3559/">Evaluating Weather and Chemical Transport Models at High Latitudes using MAGIC2021 Airborne Measurements</a> <div class="authors">Félix Langot, Cyril Crevoisier, Thomas Lauvaux, Charbel Abdallah, Jérôme Pernin, Xin Lin, Marielle Saunois, Axel Guedj, Thomas Ponthieu, Anke Roiger, Klaus-Dirk Gottschaldt, and Alina Fiehn</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3559,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3559,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_125090" data-show=".short_summary_125090" data-hide=".short_summary_button_125090" >Short summary</span> <div class="j-widget__max short_summary short_summary_125090" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Our study compares outputs from meteorological and atmospheric composition models to data from the MAGIC2021 campaign that took place in Sweden. Our results highlight performance differences among models, revealing strengths and weaknesses of different modelling techniques. We also found that wetland emission inventories overestimated emissions in regional simulations. This work helps refining methane emission predictions, essential for understanding climate change. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_125090" data-show=".short_summary_button_125090">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"> 27 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3093/">Regional transport of aerosols from Northern India and its impact on boundary layer dynamics and air quality over Chennai, a coastal megacity in Southern India</a> <div class="authors">Saleem Ali, Chandan Sarangi, and Sanjay Kumar Mehta</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3093,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3093,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123782" data-show=".short_summary_123782" data-hide=".short_summary_button_123782" >Short summary</span> <div class="j-widget__max short_summary short_summary_123782" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> The pollutants over Northern India are transported towards South India under the influence of the prevalent wind system, especially during winter. This long-range transport induces a widespread haziness over southern India, lasting for days. We evaluated the occurrence of such transport episodes over south India using observational methods and found that it suppresses the boundary layer height by ~38 % compared to the clear days while exacerbating the surface pollution by ~30–35 %. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123782" data-show=".short_summary_button_123782">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"> 27 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3382/">Brief communication: Storstrømmen glacier, Northeast Greenland, primed for end-of-decade surge</a> <div class="authors">Jonas Kvist Andersen, Rasmus Probst Meyer, Flora Salome Huiban, Mads Lykke Dømgaard, Romain Millan, and Anders Anker Bjørk</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3382,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3382,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124511" data-show=".short_summary_124511" data-hide=".short_summary_button_124511" >Short summary</span> <div class="j-widget__max short_summary short_summary_124511" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Storstrømmen Glacier in northeast Greenland goes through cycles of sudden flow speed-ups (known as surges) followed by long quiet phases. Currently in its quiet phase, recent measurements suggest it may be nearing conditions for a new surge, possibly between 2027 and 2040. We also observed several lake drainages that caused brief increases in glacier flow but did not trigger a surge. Continued monitoring is essential to understand how these processes influence glacier behavior. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124511" data-show=".short_summary_button_124511">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"> 26 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3490/">Defining Antarctic polynyas in satellite observations and climate model output to support ecological climate change research</a> <div class="authors">Laura L. Landrum, Alice K. DuVivier, Marika M. Holland, Kristen Krumhardt, and Zephyr Sylvester</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3490,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3490,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124836" data-show=".short_summary_124836" data-hide=".short_summary_button_124836" >Short summary</span> <div class="j-widget__max short_summary short_summary_124836" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Antarctic polynyas – areas of open water surrounded by sea ice or sea ice and land – are key players in Antarctic marine ecosystems. Changes in the physical characteristics of polynyas will influence how these ecosystems respond to a changing climate. This work explores how to best compare polynyas identified in satellite data and climate model data to verify that the model captures important features of Antarctic sea ice and marine ecosystems, and we show how polynyas may change. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124836" data-show=".short_summary_button_124836">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"> 26 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-2064/">Downward and upward revisions of Chinese emissions of black carbon and CO in bottom-up inventories are still required: an integrated analysis of WRF/CMAQ model and EMeRGe observations in East Asia in spring 2018</a> <div class="authors">Phuc Thi Minh Ha, Yugo Kanaya, Kazuyo Yamaji, Syuichi Itahashi, Satoru Chatani, Takashi Sekiya, Maria Dolores Andrés Hernández, John Philip Burrows, Hans Schlager, Michael Lichtenstern, Mira Poehlker, and Bruna Holanda</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-2064,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-2064,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_121694" data-show=".short_summary_121694" data-hide=".short_summary_button_121694" >Short summary</span> <div class="j-widget__max short_summary short_summary_121694" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Black carbon and CO are important to climate change. EMeRGe airborne observation can identify the suitability of emission inventories used in CMAQv5.0.2 model for Asian polluted regions. GFEDv4.1s is suitable for fire emissions. Anthropogenic BC and CO emissions from Philippines (REASv2.1) are insufficient. The estimated Chinese emissions in 2018 are 0.65±0.25 TgBC, 166±65 TgCO and 12.4±4.8 PgCO<sub>2</sub>, suggesting a reduction and increment for China's BC and CO emissions in the HTAPv2.2z inventory. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_121694" data-show=".short_summary_button_121694">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"> 26 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3552/">Multiple Equilibrium Configurations in River-Dominated Deltas</a> <div class="authors">Lorenzo Durante, Nicoletta Tambroni, and Michele Bolla Pittaluga</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3552,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3552,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_125065" data-show=".short_summary_125065" data-hide=".short_summary_button_125065" >Short summary</span> <div class="j-widget__max short_summary short_summary_125065" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> River deltas are dynamic areas where rivers meet the sea. This study examines delta configurations to guide balanced development and environmental health. Using the Po River Delta, we developed a model to understand how different delta parts interact and maintain balance. Our findings show that deltas can reach varied states of balance, with some areas more prone to shift. These insights support predictions of delta changes and better management strategies. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_125065" data-show=".short_summary_button_125065">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"> 26 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3517/">Coupling ocean currents and waves for seamless cross-scale modeling during Medicane Ianos</a> <div class="authors">Salvatore Causio, Seimur Shirinov, Ivan Federico, Giovanni De Cillis, Emanuela Clementi, Lorenzo Mentaschi, and Giovanni Coppini</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3517,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3517,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124955" data-show=".short_summary_124955" data-hide=".short_summary_button_124955" >Short summary</span> <div class="j-widget__max short_summary short_summary_124955" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This study examines how waves and ocean currents interact during severe weather, focusing on Medicane Ianos, one of the strongest storms in the Mediterranean. Using advanced modeling, we created a unique system to simulate these interactions, capturing effects like changes in water levels and wind impact on waves. We validated our approach with ideal tests and real data from the storm. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124955" data-show=".short_summary_button_124955">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"> 26 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3579/">Spatially separate production of hydrogen oxides and nitric oxide in lightning</a> <div class="authors">Jena M. Jenkins and William H. Brune</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3579,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3579,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_125128" data-show=".short_summary_125128" data-hide=".short_summary_button_125128" >Short summary</span> <div class="j-widget__max short_summary short_summary_125128" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Both the atmosphere’s primary cleaner, the hydroxyl radical, and nitric oxide are generated in extreme amounts by lightning, and laboratory and modelling experiments demonstrate that these molecules are generated in different places in lightning flashes. Thus the hydroxyl radical is not immediately consumed by the nitric oxide and instead is available to remove other pollutants in the atmosphere. Additionally, substantial nitrous acid is also likely generated by lightning. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_125128" data-show=".short_summary_button_125128">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"> 26 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3586/">Stratospheric Aerosol Intervention Experiment for the Chemistry-Climate Model Intercomparison Project</a> <div class="authors">Simone Tilmes, Ewa M. Bednarz, Andrin Jörimann, Daniele Visioni, Douglas E. Kinnison, Gabriel Chiodo, and David Plummer</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3586,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3586,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_125143" data-show=".short_summary_125143" data-hide=".short_summary_button_125143" >Short summary</span> <div class="j-widget__max short_summary short_summary_125143" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This paper describes the details of a new multi-model intercomparison experiment to assess the effects of Stratospheric Aerosol Injections on stratospheric chemistry and dynamics and, therefore, ozone. In this experiment, all models will use the same prescribed stratospheric aerosol distribution and fixed sea-surface temperatures and sea ice. We discuss the advantages and differences of this more constrained experiment compared to previous more interactive model experiments. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_125143" data-show=".short_summary_button_125143">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"> 26 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3612/">Temperature variability in southern Europe over the past 16,500 years constrained by speleothem fluid inclusion water isotopes</a> <div class="authors">Juan Luis Bernal-Wormull, Ana Moreno, Yuri Dublyansky, Christoph Spötl, Reyes Giménez, Carlos Pérez-Mejías, Miguel Bartolomé, Martin Arriolabengoa, Eneko Iriarte, Isabel Cacho, Richard Lawrence Edwards, and Hai Cheng</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3612,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3612,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_125192" data-show=".short_summary_125192" data-hide=".short_summary_button_125192" >Short summary</span> <div class="j-widget__max short_summary short_summary_125192" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We present in this manuscript a record of temperature changes during the last deglaciation and the Holocene using isotopes of fluid inclusions in stalagmites from the northeastern region of the Iberian Peninsula. This innovative climate proxy for this study region provides a quantitative understanding of the abrupt temperature changes in southern Europe of the last 16500 years before present. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_125192" data-show=".short_summary_button_125192">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"> 26 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3659/">Radiative and climate effects of aerosol scattering in long-wave radiation based on global climate modeling</a> <div class="authors">Thomas Drugé, Pierre Nabat, Martine Michou, and Marc Mallet</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3659,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3659,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_125267" data-show=".short_summary_125267" data-hide=".short_summary_button_125267" >Short summary</span> <div class="j-widget__max short_summary short_summary_125267" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Aerosol scattering in long-wave radiation is often neglected in climate models. In this study, we analyze its impact through a physical modeling of this process in the CNRM ARPEGE-Climat model. It mainly leads to surface LW radiation increases across Sahara, Sahel and Arabian Peninsula, resulting in daily minimum near-surface temperature rises. Other changes in atmospheric fields are also simulated. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_125267" data-show=".short_summary_button_125267">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"> 26 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3603/">A global summary of seafloor topography influenced by internal-wave induced turbulent water mixing</a> <div class="authors">Hans van Haren and Henk de Haas</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3603,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3603,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_125172" data-show=".short_summary_125172" data-hide=".short_summary_button_125172" >Short summary</span> <div class="j-widget__max short_summary short_summary_125172" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Turbulent water motions are important for the exchange of momentum, heat, nutrients, and suspended matter in the deep-sea. The shape of marine topography influences most water turbulence via breaking internal waves at ‘critically’ sloping seafloors. In this paper, the concept of critical slopes is revisited from a global internal wave-turbulence viewpoint using seafloor topography- and moored temperature sensor data. Potential robustness of the seafloor-internal wave interaction is discussed. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_125172" data-show=".short_summary_button_125172">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"> 26 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3305/">Assimilating Multi-site Eddy-Covariance Data to Calibrate the CH<sub>4</sub> Wetland Emission Module in a Terrestrial Ecosystem Model</a> <div class="authors">Jalisha Theanutti Kallingal, Marko Scholze, Paul Anthony Miller, Johan Lindström, Janne Rinne, Mika Aurela, Patrik Vestin, and Per Weslien</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3305,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3305,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124364" data-show=".short_summary_124364" data-hide=".short_summary_button_124364" >Short summary</span> <div class="j-widget__max short_summary short_summary_124364" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We explored the possibilities of a Bayesian-based data assimilation algorithm to improve the wetland CH<sub>4</sub> flux estimates by a dynamic vegetation model. By assimilating CH<sub>4</sub> observations from 14 wetland sites we calibrated model parameters and estimated large-scale annual emissions from northern wetlands. Our findings indicate that this approach leads to more reliable estimates of CH<sub>4</sub> dynamics, which will improve our understanding of the climate change feedback from wetland CH<sub>4</sub> emissions. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124364" data-show=".short_summary_button_124364">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"> 26 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3012/">A Time-Dependent Three-Dimensional Magnetopause Model Based on Quasi-elastodynamic Theory</a> <div class="authors">Yaxin Gu, Yi Wang, Fengsi Wei, Xueshang Feng, Andrey Samsonov, Xiaojian Song, Boyi Wang, Pingbing Zuo, Chaowei Jiang, Yalan Chen, Xiaojun Xu, and Zhilu Zhou</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3012,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3012,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123627" data-show=".short_summary_123627" data-hide=".short_summary_button_123627" >Short summary</span> <div class="j-widget__max short_summary short_summary_123627" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This study presents the POS model, the first time-dependent three-dimensional magnetopause model. The POS model captures the real-time movement and shape of the magnetopause with superior accuracy. Its concise formulation and fast computational speed make it suitable for future onboard satellite deployment, enhancing space weather forecasting capabilities and offering new methodologies for magnetopause modeling on other planets. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123627" data-show=".short_summary_button_123627">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"> 26 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3660/">Relating North Atlantic Deep Water transport to ocean bottom pressure variations as a target for satellite gravimetry missions</a> <div class="authors">Linus Shihora, Torge Martin, Anna Christina Hans, Rebecca Hummels, Michael Schindelegger, and Henryk Dobslaw</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3660,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3660,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_125269" data-show=".short_summary_125269" data-hide=".short_summary_button_125269" >Short summary</span> <div class="j-widget__max short_summary short_summary_125269" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> The Atlantic Meridional Overturning Circulation (AMOC) is a major part of the ocean circulation. Satellite gravimetry missions, like GRACE, which measure changes in Earth's mass distribution, could help monitor changes in the AMOC by detecting variations in ocean bottom pressure. To help asses if future satellite missions could detect these changes, we use ocean model simulation data to assess their connection. Additionally, we create a synthetic dataset future satellite mission simulations. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_125269" data-show=".short_summary_button_125269">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"> 26 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3387/">A Unified Framework for Surface Flux-Driven Cyclones Outside the Tropics</a> <div class="authors">Kerry Emanuel, Tommaso Alberti, Stella Bourdin, Suzana J. Camargo, Davide Faranda, Manos Flaounas, Juan Jesus Gonzalez-Aleman, Chia-Ying Lee, Mario Marcello Miglietta, Claudia Pasquero, Alice Portal, Hamish Ramsay, and Romualdo Romero</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3387,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3387,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124523" data-show=".short_summary_124523" data-hide=".short_summary_button_124523" >Short summary</span> <div class="j-widget__max short_summary short_summary_124523" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Storms strongly resembling hurricanes are sometime observed to form well outside the tropics, even in polar latitudes. They behave capriciously, developing very rapidly and then dying just as quickly. We show that strong dynamical processes in the atmosphere can sometimes cause it to become locally much colder than the underlying ocean, creating the conditions for hurricanes to form, but only over small areas and for short times. We call the resulting storms "cyclops". </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124523" data-show=".short_summary_button_124523">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3547/">Estimation of particulate organic carbon export to the ocean from lateral degradations of tropical peatland coasts</a> <div class="authors">Hiroki Kagawa, Koichi Yamamoto, Sigit Sutikno, Muhammad Haidar, Noerdin Basir, Atsushi Koyama, Ariyo Kanno, Yoshihisa Akamatsu, and Motoyuki Suzuki</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3547,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3547,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_125057" data-show=".short_summary_125057" data-hide=".short_summary_button_125057" >Short summary</span> <div class="j-widget__max short_summary short_summary_125057" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This study elucidated the carbon export that has never been highlighted before, such as coastal peat mass movements and coastal erosion in tropical peatlands. The flux of POC exported to the ocean in the northern part of Bengkalis Island, Indonesia was estimated to range from 2.06 to 7.60 tC m<sup>-1</sup> yr<sup>-1</sup> due to coastal erosion and from 1.43 to 5.41 tC m<sup>-1</sup> due to peat mass movement events. A significant amount of carbon is continuously released to the ocean. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_125057" data-show=".short_summary_button_125057">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3298/">Measurement report: size-resolved particle effective density measured by the AAC-SMPS and implications for chemical composition</a> <div class="authors">Yao Song, Jing Wei, Wenlong Zhao, Jinmei Ding, Xiangyu Pei, Fei Zhang, Zhengning Xu, Ruifang Shi, Ya Wei, Lu Zhang, Lingling Jin, and Zhibin Wang</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3298,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3298,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124354" data-show=".short_summary_124354" data-hide=".short_summary_button_124354" >Short summary</span> <div class="j-widget__max short_summary short_summary_124354" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This study investigates the size-resolved effective density (<em>ρ</em><sub>eff</sub>) of aerosol particles in Hangzhou using an AAC-SMPS. The <em>ρ</em><sub>eff</sub> values ranged from 1.47 to 1.63 g/cm<sup>3</sup>, increasing with particle diameter. Smaller particles showed significant diurnal density variations. The relationship between <em>ρ</em><sub>eff</sub> and particle diameter varies due to differences in the chemical composition of the particles. A new method to derive size-resolved chemical composition of particles from <em>ρ</em><sub>eff</sub> was proposed. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124354" data-show=".short_summary_button_124354">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-2776/">Technical note: Reconstructing surface missing aerosol elemental carbon data in long-term series with ensemble learning</a> <div class="authors">Qingxiao Meng, Yunjiang Zhang, Sheng Zhong, Jie Fang, Lili Tang, Yongcai Rao, Minfeng Zhou, Jian Qiu, Xiaofeng Xu, Jean-Eudes Petit, Olivier Favez, and Xinlei Ge</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-2776,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-2776,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123166" data-show=".short_summary_123166" data-hide=".short_summary_button_123166" >Short summary</span> <div class="j-widget__max short_summary short_summary_123166" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We developed a new method to reconstruct missing elemental carbon (EC) data in four Chinese cities from 2013 to 2023. Using machine learning, we accurately filled data gaps and introduced a new approach to analyze EC trends. Our findings reveal a significant decline in EC due to stricter pollution controls, though this slowed after 2020. This study provides a versatile framework for addressing data gaps and supports strategies to reduce urban air pollution and its climate impacts. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123166" data-show=".short_summary_button_123166">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-2972/">InSAR sensitivity to active layer ground ice content in Adventdalen, Svalbard</a> <div class="authors">Lotte Wendt, Line Rouyet, Hanne H. Christiansen, Tom Rune Lauknes, and Sebastian Westermann</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-2972,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-2972,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123559" data-show=".short_summary_123559" data-hide=".short_summary_button_123559" >Short summary</span> <div class="j-widget__max short_summary short_summary_123559" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> In permafrost environments, the ground surface moves due to the formation and melt of ice in the ground. This study compares ground surface displacements measured from satellite images against field data of ground ice contents. We find good agreement between the detected seasonal subsidence and observed ground ice melt. Our results show the potential of satellite remote sensing for mapping ground ice variability, but also indicate that ice in excess of the pore space must be considered. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123559" data-show=".short_summary_button_123559">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3075/">First Reported Detection of a Winter Continental Gamma-Ray Glow in Europe</a> <div class="authors">Jakub Šlegl, Zbyněk Sokol, Petr Pešice, Ronald Langer, Igor Strhárský, Jana Popová, Martin Kákona, Iva Ambrožová, and Ondřej Ploc</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3075,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3075,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123758" data-show=".short_summary_123758" data-hide=".short_summary_button_123758" >Short summary</span> <div class="j-widget__max short_summary short_summary_123758" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We observed the first-ever gamma-ray glow from a winter thunderstorm in Europe. Typically, these high-energy radiation events are linked to strong electric fields, but we found a surprisingly weak field at ground level. This suggests that the electric field higher up in the cloud plays a key role. Using advanced instruments, we gained new insights into how thunderstorms produce radiation, especially under rare winter conditions. This challenges existing theories. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123758" data-show=".short_summary_button_123758">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3201/">Significant influence of oxygenated volatile organic compounds on atmospheric chemistry analysis: A case study in a typical industrial city in China</a> <div class="authors">Jingwen Dai, Kun Zhang, Yanli Feng, Xin Yi, Rui Li, Jin Xue, Qing Li, Lishu Shi, Jiaqiang Liao, Yanan Yi, Fangting Wang, Liumei Yang, Hui Chen, Ling Huang, Jiani Tan, Yangjun Wang, and Li Li</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3201,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3201,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124006" data-show=".short_summary_124006" data-hide=".short_summary_button_124006" >Short summary</span> <div class="j-widget__max short_summary short_summary_124006" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Oxygenated volatile organic compounds (OVOCs) are important ozone (O<sub>3</sub>) precursors. However, most of O<sub>3</sub> formation analysis based on the box model (OBM) don't include OVOCs constraint To access the interference of OVOCs on O<sub>3</sub> simulation, this study conducted field campaign and OBM analysis. The results indicates that no OVOCs constraint in the OBM can lead to overestimate of OVOCs, free radicals, and O<sub>3</sub>. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124006" data-show=".short_summary_button_124006">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3322/">What advances monsoon onset over India?</a> <div class="authors">Bidyut Bikash Goswami and Caroline Muller</div> <div class="citation">External preprint server, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.21203/rs.3.rs-3743877/v2,</nobr><span class="hide-on-desktop">https://doi.org/10.21203/rs.3.rs-3743877/v2,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124399" data-show=".short_summary_124399" data-hide=".short_summary_button_124399" >Short summary</span> <div class="j-widget__max short_summary short_summary_124399" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> The Indian summer monsoon season runs from June to September. However, the exact onset date of monsoon varies from year to year. The onset marks the arrival of copious rainfall over India, and its accurate prediction has crucial societal implications. Comparing early versus late monsoon onsets, we note that warmer oceanic surface water in the Bay of Bengal advances monsoon onset over India. We validated our hypothesis by examining a climate model response to warm anomalies in the Bay of Bengal. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124399" data-show=".short_summary_button_124399">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3405/">Accretionary prism deformation and fluid migration caused by slow earthquakes in the Nankai subduction zone</a> <div class="authors">Takashi Tonegawa, Takeshi Akuhara, Yusuke Yamashita, Hiroko Sugioka, Masanao Shinohara, Shunsuke Takemura, and Takeshi Tsuji</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3405,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3405,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124555" data-show=".short_summary_124555" data-hide=".short_summary_button_124555" >Short summary</span> <div class="j-widget__max short_summary short_summary_124555" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This study demonstrates that for slow earthquakes in the shallow Nankai subduction zone, (1) the velocity reductions in the accretionary prism reflect the stress field changes due to the slow earthquakes, and (2) the temporal variations in the heterogeneous structure correspond to upward fluid migrations from the source region of the slow earthquakes. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124555" data-show=".short_summary_button_124555">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3385/">A shift in circadian stem increment patterns in a Pyrenean alpine treeline precedes spring growth after snow melting</a> <div class="authors">Helen Flynn, J. Julio Camarero, Alba Sanmiguel-Vallelado, Francisco Rojas Heredia, Pablo Domínguez Aguilar, Jesús Revuelto, and Juan Ignacio López-Moreno</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3385,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3385,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124520" data-show=".short_summary_124520" data-hide=".short_summary_button_124520" >Short summary</span> <div class="j-widget__max short_summary short_summary_124520" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> In the Spanish Pyrenees, changing snow seasons and warmer growing seasons could negatively impact tree growth in the montane evergreen forests. We used automatic sensors that measure tree growth to monitor and analyze the interactions between the climate, snow, and tree growth. We found a transition in the daily growth cycle that is triggered by the presence of snow. Additionally, warmer February and May temperatures enhanced tree growth. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124520" data-show=".short_summary_button_124520">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3471/">Rapid Increases of Ozone Concentrations over Tibetan Plateau Caused by Local and Non-Local Factors</a> <div class="authors">Chenghao Xu, Jintai Lin, Hao Kong, Junli Jin, Lulu Chen, and Xiaobin Xu</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3471,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3471,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124773" data-show=".short_summary_124773" data-hide=".short_summary_button_124773" >Short summary</span> <div class="j-widget__max short_summary short_summary_124773" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We observed a strong increase in deseasonalized ozone at urban stations on the Tibetan Plateau from 2015 to 2019, far exceeding the trend at the baseline station Waliguan and the Tibet Plateau average trend of four tropospheric ozone products. By combining multiple datasets and modeling approaches, we identified the main contributing factors as more frequent transport passing through the lower layers of high-emission regions and the rapid increase in anthropogenic nitrogen oxide emissions. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124773" data-show=".short_summary_button_124773">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-2996/">Tracking daily NO<sub><em>x</em></sub> emissions from an urban agglomeration based on TROPOMI NO<sub>2</sub> and a local ensemble transform Kalman filter</a> <div class="authors">Yawen Kong, Bo Zheng, and Yuxi Liu</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-2996,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-2996,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123597" data-show=".short_summary_123597" data-hide=".short_summary_button_123597" >Short summary</span> <div class="j-widget__max short_summary short_summary_123597" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Current high-resolution satellite remote sensing technologies provide a unique opportunity to derive timely, high-resolution emission data. We developed an emission inversion system to assimilate satellite NO<sub>2</sub> data to obtain daily, kilometer-scale NO<em><sub>x</sub></em> emission inventories. Our results enhance inventory accuracy, allowing us to capture the effects of pollution control policies on daily emissions (e.g., during COVID-19 lockdown) and improve fine-scale air quality modeling. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123597" data-show=".short_summary_button_123597">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3055/">Sensitivity of iceberg drift and deterioration simulations to input data from different ocean, sea ice and atmosphere models in the Barents Sea (Part II)</a> <div class="authors">Lia Herrmannsdörfer, Raed Khalil Lubbad, and Knut Vilhelm Høyland</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3055,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3055,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123721" data-show=".short_summary_123721" data-hide=".short_summary_button_123721" >Short summary</span> <div class="j-widget__max short_summary short_summary_123721" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Numerical simulations of iceberg drift and deterioration are a useful tool to bridge the gap of otherwise scarce iceberg observations in the Barents Sea. We forced iceberg simulations with different combinations of ocean, sea ice and atmosphere models to study their impact on the simulation results. We find that especially using different sea ice models Topaz and Barents-2.5 influences the iceberg drift, deterioration and occurrence in the domain. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123721" data-show=".short_summary_button_123721">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3477/">Technical note: Automatic retrieval of wind speed and direction from in situ wave observations of a small buoy</a> <div class="authors">Jan-Victor Björkqvist and Victor Alari</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3477,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3477,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 1 comment</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124789" data-show=".short_summary_124789" data-hide=".short_summary_button_124789" >Short summary</span> <div class="j-widget__max short_summary short_summary_124789" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Surface waves are generated by the wind and wave measurements can also be used to estimate the wind speed. This is beneficial in the open ocean where direct measurements of the wind are difficult. The wind speed deduced from wave measurements serve as a third estimate of the wind speed in addition to satellite measurements or numerical model results. We implemented such and algorithm to be used with wave data from a small buoy and validated it against direct wind measurements and model results. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124789" data-show=".short_summary_button_124789">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3496/">On the global geodynamic consequences of different phase boundary morphologies</a> <div class="authors">Gwynfor T. Morgan, J. Huw Davies, Robert Myhill, and James Panton</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3496,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3496,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124874" data-show=".short_summary_124874" data-hide=".short_summary_button_124874" >Short summary</span> <div class="j-widget__max short_summary short_summary_124874" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We simulate the effect of phase boundaries which are described by multiple Clapeyron slopes in P-T space on mantle geodynamics. We are motivated by two examples: the Rw-to-Brm+Pc reaction proceeding via Ak at cool temperatures, & a curving Gt-to-Brm boundary. Some have suggested these could change mantle dynamics. We find that this is unlikely for both reactions: the first due to the uniqueness of thermodynamic state, and the second due to the low value of Clapeyron slope and density change. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124874" data-show=".short_summary_button_124874">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3237/">Stress drops and earthquake nucleation in the simplest pressure-sensitive ideal elasto-plastic media</a> <div class="authors">Yury Alkhimenkov, Lyudmila Khakimova, and Yury Podladchikov</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3237,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3237,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124075" data-show=".short_summary_124075" data-hide=".short_summary_button_124075" >Short summary</span> <div class="j-widget__max short_summary short_summary_124075" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This study examines stress drops and earthquake nucleation in elasto-plastic media using 2D simulations, highlighting the importance of high temporal and spatial resolutions in capturing stress evolution and strain fields. Stress drops reflect fault rupture mechanics and emulate earthquake behavior. The non-Gaussian distribution of stress drop amplitudes resembles "solid turbulence." Elasto-plastic models simulate key earthquake processes and could improve seismic hazard assessment. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124075" data-show=".short_summary_button_124075">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"> 25 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3511/">Numerical Analysis of the Effect of Heterogeneity on CO<sub>2</sub> Dissolution Enhanced by Gravity Driven Convection</a> <div class="authors">Yufei Wang, Daniel Fernandez Garcia, and Maarten W. Saaltink</div> <div class="citation">External preprint server, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.22541/au.170709021.19680723/v1,</nobr><span class="hide-on-desktop">https://doi.org/10.22541/au.170709021.19680723/v1,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124932" data-show=".short_summary_124932" data-hide=".short_summary_button_124932" >Short summary</span> <div class="j-widget__max short_summary short_summary_124932" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> During geological carbon sequestration, the injected supercritical CO<sub>2</sub>, being less dense, floats above the brine. The dissolution of CO<sub>2</sub> into brine helps mitigate the risk of CO<sub>2</sub> leakage. As CO<sub>2</sub> dissolves into the brine, it increases the density of brine in the upper layer, initiating gravity-driven convection (GDC), which significantly enhances the rate of CO<sub>2</sub> dissolution. We derived two empirical formulas to predict the asymptotic dissolution rate driven by GDC in heterogeneous fields. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124932" data-show=".short_summary_button_124932">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"> 22 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3522/">Investigating Carbon and Nitrogen Conservation in Reported CMIP6 Earth System Model Data</a> <div class="authors">Gang Tang, Zebedee Nicholls, Chris Jones, Thomas Gasser, Alexander Norton, Tilo Ziehn, Alejandro Romero-Prieto, and Malte Meinshausen</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3522,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3522,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124964" data-show=".short_summary_124964" data-hide=".short_summary_button_124964" >Short summary</span> <div class="j-widget__max short_summary short_summary_124964" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We analyzed carbon and nitrogen mass conservation in data from CMIP6 Earth System Models. Our findings reveal significant discrepancies between flux and pool size data, particularly in nitrogen, where cumulative imbalances can reach hundreds of gigatons. These imbalances appear primarily due to missing or inconsistently reported fluxes – especially for land use and fire emissions. To enhance data quality, we recommend that future climate data protocols address this issue at the reporting stage. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124964" data-show=".short_summary_button_124964">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"> 22 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3550/">Kinetics of the reactions of OH with CO, NO, NO<sub>2</sub> and of HO<sub>2</sub> with NO<sub>2</sub> in air at 1 atm pressure, room temperature and tropospheric water vapour concentrations</a> <div class="authors">Michael Rolletter, Andreas Hofzumahaus, Anna Novelli, Andreas Wahner, and Hendrik Fuchs</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3550,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3550,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_125062" data-show=".short_summary_125062" data-hide=".short_summary_button_125062" >Short summary</span> <div class="j-widget__max short_summary short_summary_125062" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Highly accurate rate coefficients of termolecular reactions between OH and HO<sub>2</sub> radicals and reactive nitrogen oxides were measured for conditions in the lower troposphere, providing improved constraints on recommended values. No dependence on water vapour was found except for the HO<sub>2</sub>+NO<sub>2</sub> reaction, which can be explained by an enhanced rate coefficient of the NO<sub>2</sub> reaction with the water complex of the HO<sub>2</sub> radical. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_125062" data-show=".short_summary_button_125062">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"> 22 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-2827/">The role of surface-active macromolecules in the ice nucleating ability of lignin, Snomax, and agricultural soil extracts</a> <div class="authors">Kathleen A. Thompson, Paul Bieber, Anna J. Miller, Nicole Link, Benjamin J. Murray, and Nadine Borduas-Dedekind</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-2827,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-2827,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123279" data-show=".short_summary_123279" data-hide=".short_summary_button_123279" >Short summary</span> <div class="j-widget__max short_summary short_summary_123279" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Lignin and Snomax are surface-active macromolecules that show a relationship between increasing concentrations, decreasing surface tension, and increasing ice-nucleating ability. However, this relationship did not hold for agricultural soil extracts collected in the UK and Canada. Hydrophobic interfaces play an important role in the ice-nucleating activity of organic matter; as the complexity of the sample increases, the hydrophobic interfaces in the bulk compete with the air-water interface. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123279" data-show=".short_summary_button_123279">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"> 22 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3594/">Double dating in the Middle Pleistocene: assessing the consistency and performance of the carbonate U–Th and U–Pb dating methods</a> <div class="authors">Timothy J. Pollard, Jon D. Woodhead, Russell N. Drysdale, R. Lawrence Edwards, Xianglei Li, Ashlea N. Wainwright, Mathieu Pythoud, Hai Cheng, John C. Hellstrom, Ilaria Isola, Eleonora Regattieri, Giovanni Zanchetta, and Dylan S. Parmenter</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3594,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3594,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_125155" data-show=".short_summary_125155" data-hide=".short_summary_button_125155" >Short summary</span> <div class="j-widget__max short_summary short_summary_125155" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> The uranium-thorium and uranium-lead radiometric dating methods are both capable of dating carbonate samples ranging in age from about 400,000 to 650,000 years.  Here we test agreement between the two methods by 'double dating' speleothems (i.e. secondary cave mineral deposits) that grew within this age range. We demonstrate excellent agreement between the two dating methods and discuss their relative strengths and weaknesses. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_125155" data-show=".short_summary_button_125155">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"> 22 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3084/">Controls on fluvial grain sizes in post-glacial landscapes</a> <div class="authors">Anya H. Towers, Mikael Attal, Simon M. Mudd, and Fiona J. Clubb</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3084,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3084,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123771" data-show=".short_summary_123771" data-hide=".short_summary_button_123771" >Short summary</span> <div class="j-widget__max short_summary short_summary_123771" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We explore controls on channel sediment characteristics in post-glacial landscapes. In contrast to other studies that have focused on landscapes with little glacial influence, we find no apparent controls. We propose that Scotland's post-glacial legacy drives the lack of sedimentological trends, and that changes in landscape morphology and sediment sources caused by glacial processes lead to a complete decoupling between fluvial sediment grain size and environmental variables. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123771" data-show=".short_summary_button_123771">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"> 22 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3503/">Technical note: a Weighing Forest Floor Grid-Lysimeter</a> <div class="authors">Heinke Paulsen and Markus Weiler</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3503,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3503,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 1 comment</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124889" data-show=".short_summary_124889" data-hide=".short_summary_button_124889" >Short summary</span> <div class="j-widget__max short_summary short_summary_124889" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This technical note describes the development of the weighing Forest Floor Grid-Lysimeter. The device is needed to investigate the dynamics of the water balance components of the organic layer in forests. Quantifying precipitation, drainage, evaporation and storage. We designed a setup that can be easily rebuild and is cost-effective, which allows for customized applications. Performance metrics from laboratory results and initial field data are presented. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124889" data-show=".short_summary_button_124889">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"> 22 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3341/">Complex interplay of forcings drives Indian vegetation and summer monsoon variability during MIS 11</a> <div class="authors">Dulce Oliveira, Stéphanie Desprat, Qiuzhen Yin, Coralie Zorzi, Zhipeng Wu, Krishnamurthy Anupama, Srinivasan Prasad, Montserrat Alonso-García, and Philippe Martinez</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3341,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3341,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124441" data-show=".short_summary_124441" data-hide=".short_summary_button_124441" >Short summary</span> <div class="j-widget__max short_summary short_summary_124441" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We present an unprecedented record of Indian summer monsoon (ISM)-induced vegetation changes for MIS 11, a key interglacial. Site U1446 pollen data and models show that ISM-vegetation shifts stem from an interplay of dominant forcings based on boundary conditions. Insolation is the main driver during MIS 11c interglacial conditions, akin to future scenarios, while ice volume and CO₂ prevail in the glacial inception. Superimposed changes are marked by prominent forest contractions and expansions. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124441" data-show=".short_summary_button_124441">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"> 22 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3170/">Benchmarking historical performance and future projections from a global hydrologic model with a basin-scale model</a> <div class="authors">Rajesh R. Shrestha, Alex J. Cannon, Sydney Hoffman, Marie Whibley, and Aranildo Lima</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3170,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3170,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123951" data-show=".short_summary_123951" data-hide=".short_summary_button_123951" >Short summary</span> <div class="j-widget__max short_summary short_summary_123951" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We evaluate the historical performance and future projections from a global hydrologic model, the Community Water Model, against a watershed hydrologic model, the Variable Infiltration Capacity for the Liard River basin in Canada. Results from the two models are generally consistent at annual and monthly time scales, suggesting that a calibrated global hydrologic model can provide robust projections. We explain the differences in projections in terms of model uncertainties. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123951" data-show=".short_summary_button_123951">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"> 21 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3031/">Terrestrial and marine plastic pollution outlook in the Mediterranean region: a box-model approach based on OECD policy scenarios</a> <div class="authors">Théo Segur and Jeroen E. Sonke</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3031,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3031,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123670" data-show=".short_summary_123670" data-hide=".short_summary_button_123670" >Short summary</span> <div class="j-widget__max short_summary short_summary_123670" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Our paper provides a quantification of plastic pollution in the Mediterranean region, and several policy scenario projections based on OECD data toward 2100. We estimate a 4-fold increase of Mediterranean marine plastic stock by 2060 and that the implementation of terrestrial plastic cleanup can significantly help to reduce plastic pollution transfer from land to sea. Our results provide insight for policy makers, which is needed at the regional scale in a context of the UNEP plastic treaty. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123670" data-show=".short_summary_button_123670">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"> 21 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3051/">Variation in shortwave water vapour continuum and impact on clear-sky shortwave radiative feedback</a> <div class="authors">Kaah P. Menang, Stefan A. Buehler, Lukas Kluft, Robin J. Hogan, and Florian E. Roemer</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3051,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3051,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123717" data-show=".short_summary_123717" data-hide=".short_summary_button_123717" >Short summary</span> <div class="j-widget__max short_summary short_summary_123717" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We investigated how the uncertainty in representing water vapour continuum absorption in the shortwave affects clear-sky shortwave radiative feedback. For current surface temperature, the impact is modest (<2 %). In a warmer world, continuum induced error in estimated shortwave feedback is up to ~5 %. Using the MT_CKD model in radiative transfer calculations may lead to an underestimation of the shortwave feedback. Constraining shortwave continuum will contribute to reducing these discrepancies. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123717" data-show=".short_summary_button_123717">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"> 21 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3101/">Portable X-Ray Fluorescence as a Tool for Urban Soil Contamination Analysis: Accuracy, Precision, and Practicality</a> <div class="authors">Eriell Jenkins, John Galbraith, and Anna Paltseva</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3101,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3101,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123801" data-show=".short_summary_123801" data-hide=".short_summary_button_123801" >Short summary</span> <div class="j-widget__max short_summary short_summary_123801" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This review examines the use of portable X-ray fluorescence (PXRF) technology to detect harmful metals in urban soils. PXRF provides a fast, cost-effective method for analyzing contaminated soils, essential for safe urban agriculture. The review highlights PXRF's accuracy and limitations, stressing the need for proper calibration and sample preparation. These findings will help inform future efforts to enhance soil health and environmental safety in urban areas. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123801" data-show=".short_summary_button_123801">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"> 21 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3238/">Thermodynamically admissible derivation of Biot's poroelastic equations and Gassmann's equations from conservation laws</a> <div class="authors">Yury Alkhimenkov and Yury Y. Podladchikov</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3238,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3238,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124077" data-show=".short_summary_124077" data-hide=".short_summary_button_124077" >Short summary</span> <div class="j-widget__max short_summary short_summary_124077" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This paper presents a rigorous derivation of Gassmann's equations, grounded in thermodynamic principles and conservation laws, addressing gaps and potential inconsistencies in the original formulation. It also explores Biot's poroelastic equations, demonstrating that Gassmann's equations are a specific case within Biot’s framework. The study affirms the robustness of Gassmann's equations when assumptions are met, and symbolic Maple routines are provided to ensure reproducibility of the results. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124077" data-show=".short_summary_button_124077">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"> 21 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3310/">Evaluating spatiotemporal variations and exposure risk of ground-level ozone concentrations across China from 2000 to 2020 using satellite-derived high-resolution data</a> <div class="authors">Qingqing He, Jingru Cao, Pablo E. Saide, Tong Ye, and Weihang Wang</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3310,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3310,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124373" data-show=".short_summary_124373" data-hide=".short_summary_button_124373" >Short summary</span> <div class="j-widget__max short_summary short_summary_124373" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We explored variations in ground ozone and exposure risk hotspots across China (2000–2020) at multiple spatiotemporal scales using a high-resolution dataset derived from satellite LST via a machine-learning hindcast framework. The dataset was validated using cross-validation and external measurements. A non-monotonous trend emerged, with turning points around 2007 and 2015, showing regional variation. Ozone levels >100 μg/m<sup>3</sup> shifted from June to May, while levels >160 μg/m<sup>3</sup> expanded in the NCP. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124373" data-show=".short_summary_button_124373">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"> 21 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3415/">Short Communications: Multiscale topographic complexity analysis with pyTopoComplexity</a> <div class="authors">Larry Syu-Heng Lai, Adam M. Booth, Alison R. Duvall, and Erich Herzig</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3415,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3415,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124586" data-show=".short_summary_124586" data-hide=".short_summary_button_124586" >Short summary</span> <div class="j-widget__max short_summary short_summary_124586" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> pyTopoComplexity is an open-source tool that quantifies land surface complexity using advanced methods. Applied to a landslide-affected area in Washington, USA, it accurately analyzed landform features at various scales, enhancing our understanding of landform recovery after disturbances. By integrating with Landlab’s landscape evolution simulations, the software allows researchers to explore how different processes drive the evolution of surface complexity in response to natural forces. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124586" data-show=".short_summary_button_124586">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"> 21 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-2503/">Sources and trends of Black Carbon Aerosol in a Megacity of Nanjing, East China After the China Clean Action Plan and Three-Year Action Plan</a> <div class="authors">Abudurexiati Abulimiti, Yanlin Zhang, Mingyuan Yu, Yihang Hong, Yu-Chi Lin, Chaman Gul, and Fang Cao</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-2503,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-2503,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_122468" data-show=".short_summary_122468" data-hide=".short_summary_button_122468" >Short summary</span> <div class="j-widget__max short_summary short_summary_122468" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> To improve air quality, the Chinese government implemented strict clean air actions. We explored how black carbon (BC) responded to these actions and found that the reduction in liquid fuel use was the main factor driving the decrease in BC levels. Additionally, meteorological factors also played a significant role in the long-term trends of BC. These factors should be considered in future emission reduction policies to further enhance air quality improvements. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_122468" data-show=".short_summary_button_122468">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"> 21 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3492/">Pelagic coccolithophore production and dissolution and their impacts on particulate inorganic carbon cycling in the western North Pacific</a> <div class="authors">Yuye Han, Zvi Steiner, Zhimian Cao, Di Fan, Junhui Chen, Jimin Yu, and Minhan Dai</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3492,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3492,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124858" data-show=".short_summary_124858" data-hide=".short_summary_button_124858" >Short summary</span> <div class="j-widget__max short_summary short_summary_124858" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Coccolithophore calcite accounts for a major fraction of particulate inorganic carbon (PIC) standing stocks in the western North Pacific, with a markedly higher contribution in the oligotrophic subtropical gyre than in the Kuroshio-Oyashio transition region, which highlights the importance of coccolithophores for PIC production in the pelagic ocean. We also found extensive dissolution of coccolithophore calcite in the oversaturated shallow waters primarily driven by microbial metabolic activity. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124858" data-show=".short_summary_button_124858">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-2024-3159/">Investigating the link between mineral dust hematite content and intensive optical properties by means of lidar measurements and aerosol modelling</a> <div class="authors">Sofía Gómez Maqueo Anaya, Dietrich Althausen, Julian Hofer, Moritz Haarig, Ulla Wandinger, Bernd Heinold, Ina Tegen, Matthias Faust, Holger Baars, Albert Ansmann, Ronny Engelmann, Annett Skupin, Birgit Heese, and Kerstin Schepanski</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3159,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3159,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123929" data-show=".short_summary_123929" data-hide=".short_summary_button_123929" >Short summary</span> <div class="j-widget__max short_summary short_summary_123929" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This study investigates how hematite (an iron oxide mineral) in the Saharan Desert dust affects how dust particles interact with radiation. Using lidar data from Cabo Verde (2021–2022) and hematite content from atmospheric model simulations, the results show that higher hematite fraction leads to stronger particle backscattering at specific wavelengths. These findings can improve the representaiton of mineral dust in climate models, particularly regarding their radiative effect. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123929" data-show=".short_summary_button_123929">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-2024-3222/">Measurement Report: Influence of particle density on secondary ice production by graupel and ice pellet collisions</a> <div class="authors">Sudha Yadav, Lilly Metten, Pierre Grzegorczyk, Alexander Theis, Subir Kumar Mitra, and Miklós Szakáll</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3222,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3222,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124045" data-show=".short_summary_124045" data-hide=".short_summary_button_124045" >Short summary</span> <div class="j-widget__max short_summary short_summary_124045" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We conducted laboratory studies on the fragmentation of ice particles by collision. Graupels were created by riming at -7 and -15 °C simulating also rotation and tumbling. Ice pellets were generated by freezing water in 3D-printed spherical molds. The number of fragments generated by collision was between 1 and 20, and strongly dependent on the density of the graupel. We also showed that the number of fragments becomes zero when the particle suffers more than three collisions in a row. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124045" data-show=".short_summary_button_124045">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-2024-2930/">High-resolution air quality maps for Bucharest using Mixed-Effects Modeling Framework</a> <div class="authors">Camelia Talianu, Jeni Vasilescu, Doina Nicolae, Alexandru Ilie, Andrei Dandocsi, Anca Nemuc, and Livio Belegante</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-2930,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-2930,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123481" data-show=".short_summary_123481" data-hide=".short_summary_button_123481" >Short summary</span> <div class="j-widget__max short_summary short_summary_123481" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Bucharest, Romania's capital, has successfully used mobile measurements and mixed-effects LUR models to derive seasonal maps of near-surface PM<sub>10</sub>, NO<sub>2</sub>, and UFP. The data was collected during two intensive campaigns, covering high-traffic streets, residential, industrial, and commercial districts. The model's performance was evaluated, demonstrating its potential for high-resolution mapping in other cities with well-characterized urban structures and diverse in situ monitoring stations. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123481" data-show=".short_summary_button_123481">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-2024-3560/">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"><strong>Discussion: open, 0 comments</strong></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-2024-3309/">An assessment of the disequilibrium of Alaskan glaciers</a> <div class="authors">Daniel R. Otto, Gerard H. Roe, and John Erich Christian</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3309,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3309,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124370" data-show=".short_summary_124370" data-hide=".short_summary_button_124370" >Short summary</span> <div class="j-widget__max short_summary short_summary_124370" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Glaciers respond slowly to changes in climate, meaning that they are not yet adjusted to the present-day level of warming. Using a simple model, we find that the median Alaskan glacier has undergone only 27 % of the retreat necessary to equilibrate to the current climate. Our findings hold even when accounting for large uncertainties, suggesting that substantial retreat is inevitable even if future warming slows or stabilizes. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124370" data-show=".short_summary_button_124370">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-2024-3108/">Data-Driven Scaling Methods for Soil Moisture Cosmic Ray Neutron Sensors</a> <div class="authors">Roland Baatz, Patrick Davies, Paolo Nasta, and Heye Bogena</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3108,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3108,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123814" data-show=".short_summary_123814" data-hide=".short_summary_button_123814" >Short summary</span> <div class="j-widget__max short_summary short_summary_123814" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This study develops a new method to improve soil moisture measurements from cosmic ray neutron sensors. Using advanced modeling, we account for changes in atmospheric pressure, air humidity, and cosmic ray intensity based on site and sensor characteristics. The results show that precise adjustments are needed to better measure soil moisture, supporting improved decisions in farming, water management, and climate monitoring. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123814" data-show=".short_summary_button_123814">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-2024-3263/">A Novel Framework for Analyzing Rainy Season Dynamics in semi-arid environments: A case study in the Peruvian Rio Santa Basin</a> <div class="authors">Lorenz Hänchen, Emily Potter, Cornelia Klein, Pierluigi Calanca, Fabien Maussion, Wolfgang Gurgiser, and Georg Wohlfahrt</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3263,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3263,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124166" data-show=".short_summary_124166" data-hide=".short_summary_button_124166" >Short summary</span> <div class="j-widget__max short_summary short_summary_124166" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> In semi-arid regions, the timing and duration of the rainy season are crucial for agriculture. This study introduces a new framework for improving estimations of start and end of the rainy season by testing how well they fit local vegetation data. We improve the performance of existing methods and present a new one with higher performance. Our findings can help to make informed decisions about water usage, and the framework can be applied to other regions as well. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124166" data-show=".short_summary_button_124166">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-2024-3448/">Multiphysics property prediction from hyperspectral drill core data</a> <div class="authors">Akshay Kamath, Samuel Thiele, Moritz Kirsch, and Richard Gloaguen</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3448,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3448,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124713" data-show=".short_summary_124713" data-hide=".short_summary_button_124713" >Short summary</span> <div class="j-widget__max short_summary short_summary_124713" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We developed a deep learning model that uses hyperspectral imaging data to predict key physical rock properties, specifically density, slowness, and gamma-ray values. Our model successfully learned to translate hyperspectral information into predicted physical properties. Tests on independent data gave accurate results, demonstrating the potential of hyperspectral data for mapping physical rock properties. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124713" data-show=".short_summary_button_124713">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-2024-3449/">Variable organic matter stoichiometry enhances the biological drawdown of CO<sub>2</sub> in the Northwest European shelf seas</a> <div class="authors">Kubilay Timur Demir, Moritz Mathis, Jan Kossack, Feifei Liu, Ute Daewel, Christoph Stegert, Helmuth Thomas, and Corinna Schrum</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3449,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3449,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124714" data-show=".short_summary_124714" data-hide=".short_summary_button_124714" >Short summary</span> <div class="j-widget__max short_summary short_summary_124714" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This study examines how variations in the ratios of carbon, nitrogen and phosphorus in organic matter affect carbon cycling in the Northwest European shelf seas. Traditional models with fixed ratios tend to underestimate biological carbon uptake. By integrating variable ratios into a regional model, we find that carbon dioxide uptake increases by 10–33 %. These results highlight the need to include variable ratios for accurate assessments of regional and global carbon cycles. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124714" data-show=".short_summary_button_124714">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-2024-3501/">Cold pools mediate mesoscale adjustments of trade-cumulus fields to changes in cloud-droplet number concentration</a> <div class="authors">Pouriya Alinaghi, Fredrik Jansson, Daniel A. Blázquez, and Franziska Glassmeier</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3501,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3501,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124882" data-show=".short_summary_124882" data-hide=".short_summary_button_124882" >Short summary</span> <div class="j-widget__max short_summary short_summary_124882" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Shallow clouds in the trades are a major source of uncertainty in climate projections. These clouds organize into striking mesoscale patterns that are exactly what climate models lack. This study explores the origin of such patterns and investigates how variations in microscale properties control them. The importance of microscale effects is compared to that of large-scale forcing on the mesoscale organization of trade-cumulus fields. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124882" data-show=".short_summary_button_124882">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"><strong>Discussion: open, 0 comments</strong></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 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-2024-3554/">Ionospheric Chaos in Solar quiet Current due to Sudden Stratospheric Warming Events Across Europe-Africa Sector</a> <div class="authors">Irewola Aaron Oludehinwa, Andrei Velichko, Olasunkanmi Isaac Olusola, Olawale Segun Bolaji, Norbert Marwan, Babaola O. Ogunsua, Abdullahi Ndzi Njah, and Timothy O. Ologun</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3554,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3554,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_125073" data-show=".short_summary_125073" data-hide=".short_summary_button_125073" >Short summary</span> <div class="j-widget__max short_summary short_summary_125073" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> The contributing influence of SSW to regional ionosphere through chaos theory is examined. We found that ionospheric chaos is more pronounced in the European sector compared to Africa sector during SSW. Evidence of orderliness behavior in regional ionosphere of African sector was observed. Finally, we noticed that after the peak phase of SSW, ionospheric chaos is found to be more pronounced. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_125073" data-show=".short_summary_button_125073">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-2024-3456/">Promoted phosphorus transformation by increasing soil microbial diversity and network complexity – A case of long-term mixed-species plantations of <em>Eucalyptus</em> with N-fixing tree species</a> <div class="authors">Jiyin Li, Yeming You, Wen Zhang, Yi Wang, Yuying Liang, Haimei Huang, Hailun Ma, Qinxia He, Angang Ming, and Xueman Huang</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3456,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3456,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124725" data-show=".short_summary_124725" data-hide=".short_summary_button_124725" >Short summary</span> <div class="j-widget__max short_summary short_summary_124725" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Monoculture of Eucalyptus can lead to soil degradation. In this study, we introduced nitrogen-fixing species in Eucalyptus plantations and investigated the effect of the introduction of nitrogen-fixing species on soil phosphorus transformation by soil microorganisms and their nitrogen-phosphorus cycling functional genes, which may be a promising forest management strategy to improve ecosystem phosphorus benefits. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124725" data-show=".short_summary_button_124725">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-2024-3462/">Measurement Report: A survey of meteorological and cloud properties during ACTIVATE's postfrontal flights and their suitability for Lagrangian case studies</a> <div class="authors">Florian Tornow, Ann Fridlind, George Tselioudis, Brian Cairns, Andrew Ackerman, Seethala Chellappan, David Painemal, Paquita Zuidema, Christiane Voigt, Simon Kirschler, and Armin Sorooshian</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3462,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3462,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124742" data-show=".short_summary_124742" data-hide=".short_summary_button_124742" >Short summary</span> <div class="j-widget__max short_summary short_summary_124742" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> The recent NASA campaign ACTIVATE (Aerosol Cloud meTeorology Interactions oVer the western ATlantic Experiment) performed 71 tandem flights in mid-latitude marine cold-air outbreaks off the US Eastern seaboard. We provide meteorological and cloud transition stage context, allowing us to identify days that are most suitable for Lagrangian modeling and analysis. Surveyed cloud properties show signatures of cloud microphysical processes, such as cloud-top entrainment and secondary ice formation. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124742" data-show=".short_summary_button_124742">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"> 19 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3386/">Assessing evapotranspiration dynamics across central Europe in the context of land-atmosphere drivers</a> <div class="authors">Anke Fluhrer, Martin Baur, María Piles, Bagher Bayat, Mehdi Rahmati, David Chaparro, Clémence Dubois, Florian Hellwig, Carsten Montzka, Angelika Kübert, Marlin Mueller, Isabel Augscheller, Francois Jonard, Konstantin Schellenberg, and Thomas Jagdhuber</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3386,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3386,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124521" data-show=".short_summary_124521" data-hide=".short_summary_button_124521" >Short summary</span> <div class="j-widget__max short_summary short_summary_124521" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This study compares established evapotranspiration products in Central Europe and evaluates their multi-seasonal performance during wet & drought phases between 2017–2020 together with important soil-plant-atmosphere drivers. Results show that SEVIRI, ERA5-land & GLEAM perform best compared to ICOS measurements. During moisture limited drought years, ET is decreasing due to decreasing soil moisture and increasing vapor pressure deficit, while in other years ET is mainly controlled by VPD. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124521" data-show=".short_summary_button_124521">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"> 19 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3473/">Intensity and dynamics of extreme cold spells of the 21st century in France from CMIP6 data</a> <div class="authors">Camille Cadiou and Pascal Yiou</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3473,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3473,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124779" data-show=".short_summary_124779" data-hide=".short_summary_button_124779" >Short summary</span> <div class="j-widget__max short_summary short_summary_124779" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Cold extremes significantly affect healthcare and energy systems. Global warming is expected to reduce these extremes. Our study indeed shows that very intense cold spells will become nearly impossible in France by the end of the 21st century for high levels of warming. However, we demonstrate that events as intense as the 1985 cold spell in France may still occur in the near future. These events are linked to specific atmospheric patterns that bring cold air from high latitudes into Europe. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124779" data-show=".short_summary_button_124779">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"> 19 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-2727/">Optical Properties of North Atlantic Aerosols Through a compact dual-wavelength depolarization Lidar Observations</a> <div class="authors">Yenny González, María F. Sánchez-Barrero, Ioana Popovici, África Barreto, Stephane Victori, Ellsworth J. Welton, Rosa D. García, Pablo G. Sicilia, Fernando A. Almansa, Carlos Torres, and Philippe Goloub</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-2727,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-2727,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_122925" data-show=".short_summary_122925" data-hide=".short_summary_button_122925" >Short summary</span> <div class="j-widget__max short_summary short_summary_122925" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We characterize the optical properties of various aerosols using a compact dual-wavelength depolarization lidar (CIMEL CE376) at 532 and 808 nm. Through a modified two-wavelength Klett inversion method, we assess the vertical distribution and temporal evolution of Saharan dust, volcanic aerosols, and wildfire smoke in the subtropical North Atlantic from August 2021 to August 2023. The study confirms the CE376 lidar's effectiveness in monitoring and characterizing atmospheric aerosols over time. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_122925" data-show=".short_summary_button_122925">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"> 19 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3097/">What do the arc magmatism trace element patterns and Sr-Nd-Pb isotopic data reflect: Insight from the Urumieh-Dokhtar magmatic arc of Iran</a> <div class="authors">Mohammad Reza Ghorbani, Meysam Akbari, Ian T. Graham, Mathieu Benoit, and Fatemeh Sepidbar</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3097,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3097,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123791" data-show=".short_summary_123791" data-hide=".short_summary_button_123791" >Short summary</span> <div class="j-widget__max short_summary short_summary_123791" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Original geochemical data for the vast Cenozoic arc magmatism of Iran introduce three distinct rock series rooted in the mantle wedge. The LILE-rich and LILE-poor series show wet-slab melt metasomatism and dry-slab melt metasomatism signatures respectively. The third series rich in incompatible elements, ITE-rich, indicate the input of asthenosphere as well. Eocene-Early Miocene ages for the three series imply that the metasomatic events predate Eocene and the three series occur intermittently. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123791" data-show=".short_summary_button_123791">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"> 19 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-2929/">Impacts of Barrier-Island Breaching on Mainland Flooding During Storm Events applied to Moriches, NY</a> <div class="authors">Catherine Renae Jeffries, Robert Weiss, Jennifer L. Irish, and Kyle Mandli</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-2929,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-2929,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123478" data-show=".short_summary_123478" data-hide=".short_summary_button_123478" >Short summary</span> <div class="j-widget__max short_summary short_summary_123478" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Barrier islands are important to their adjacent mainland coastline. Breaching of barrier islands creates a channel of water between the ocean and bay and increases the storm surge along the mainland coast. To examine how breaching impacts the coast we simulated a hurricane and varied the number, locations, and sizes of different breaches. We learned that total breach area directly impacts coastal flooding, and breach locations are an important predictor of flooding. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123478" data-show=".short_summary_button_123478">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"> 19 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3389/">Improved modelling of mountain snowpacks with spatially distributed precipitation bias correction derived from historical reanalysis</a> <div class="authors">Manon von Kaenel and Steve Margulis</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3389,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3389,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124525" data-show=".short_summary_124525" data-hide=".short_summary_button_124525" >Short summary</span> <div class="j-widget__max short_summary short_summary_124525" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Accurate snow water equivalent (SWE) estimates are crucial for water management in snowmelt-dependent regions, but bias and uncertainty in precipitation data make this challenging. Here, we leverage insights from a historical SWE data product to correct these biases and yield more accurate SWE estimates and streamflow predictions. Incorporating snow depth observations further boosts accuracy. This study demonstrates an effective method to downscale and bias-correct global mountain precipitation. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124525" data-show=".short_summary_button_124525">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"> 19 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3443/">Estimating breakpoints between climate states in the Cenozoic Era</a> <div class="authors">Mikkel Bennedsen, Eric Hillebrand, Siem Jan Koopman, and Kathrine By Larsen</div> <div class="citation">External preprint server, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/https://doi.org/10.48550/arXiv.2404.08336,</nobr><span class="hide-on-desktop">https://doi.org/https://doi.org/10.48550/arXiv.2404.08336,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124707" data-show=".short_summary_124707" data-hide=".short_summary_button_124707" >Short summary</span> <div class="j-widget__max short_summary short_summary_124707" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Our study presents a statistical approach for identifying transitions between climate states in the Cenozoic Era. We analyze a temperature proxy record covering the period from 67.1 million years ago to present time. Our analysis corroborates the transitions previously identified in the literature and provides statistical justification for additional transitions. Our approach allows for constructing confidence intervals, offering measures of uncertainty. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124707" data-show=".short_summary_button_124707">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"> 19 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3526/">Effects of Warming and Stratospheric Aerosol Injection on Tropical Cyclone Distribution and Frequency in a High-Resolution Global Circulation Model</a> <div class="authors">Andrew Feder, David Randall, and Donald Dazlich</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3526,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3526,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124992" data-show=".short_summary_124992" data-hide=".short_summary_button_124992" >Short summary</span> <div class="j-widget__max short_summary short_summary_124992" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We studied the effect of solar geoengineering on the intensity and distribution of tropical cyclones in global climate models, as compared to a historical baseline and a comparable, non-engineered warming scenario. We find that, while the given geoengineering approach does not completely bring cyclones back to their typical historical behavior, it restores important elements of cyclone behavior to baseline with some important regional deviations. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124992" data-show=".short_summary_button_124992">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"> 19 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3534/">Evaluating the consistency of forest disturbance datasets in continental USA</a> <div class="authors">Laura Eifler, Franziska Müller, and Ana Bastos</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3534,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3534,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_125018" data-show=".short_summary_125018" data-hide=".short_summary_button_125018" >Short summary</span> <div class="j-widget__max short_summary short_summary_125018" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Forests provide ecosystem services and biodiversity, but they are increasingly affected by disturbances. Consistent global data on forest disturbances are lacking, impeding effective assessment. We compare four forest disturbance datasets for the continental USA, finding moderate agreement overall, with ground-based inventories more consistent than satellite data. This emphasizes the need for enhanced data quality assessment, integration, and accuracy to better understand forest disturbances. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_125018" data-show=".short_summary_button_125018">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"> 19 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3484/">Towards a Global Spatial Machine Learning Model for Seasonal Groundwater Level Predictions in Germany</a> <div class="authors">Stefan Kunz, Alexander Schulz, Maria Wetzel, Maximilian Nölscher, Teodor Chiaburu, Felix Biessmann, and Stefan Broda</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3484,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3484,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124810" data-show=".short_summary_124810" data-hide=".short_summary_button_124810" >Short summary</span> <div class="j-widget__max short_summary short_summary_124810" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Accurate groundwater level predictions are essential for a sustainable groundwater management. This study applies two machine learning (ML) models—N-HiTS and TFT—to seasonally predict groundwater levels for 5,288 monitoring wells across Germany. Both approaches provided good predictions across diverse hydrogeological conditions, whereby N-HiTS outperformed the TFT. Both models showed better perforance in areas with high data density, in lowlands, and when distinct seasonal dynamics occurred. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124810" data-show=".short_summary_button_124810">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"> 19 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3401/">Atmospheric moisture tracking with WAM2layers v3</a> <div class="authors">Peter Kalverla, Imme Benedict, Chris Weijenborg, and Ruud J. van der Ent</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3401,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3401,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124546" data-show=".short_summary_124546" data-hide=".short_summary_button_124546" >Short summary</span> <div class="j-widget__max short_summary short_summary_124546" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We introduce a new version of WAM2layers, a computer program that tracks how the weather brings water from one place to another. It uses data from weather and climate models, whose resolution is steadily increasing. Processing the latest data became a challenge, and the updates presented here ensure that WAM2layers runs smoothly again. We also made it easier to use the program and to understand its source code. This makes it more transparent and reliable, and easier to maintain. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124546" data-show=".short_summary_button_124546">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"> 18 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3148/">The influence of lateral flow on land surface fluxes in southeast Australia varies with model resolution</a> <div class="authors">Anjana Devanand, Jason Evans, Andy Pitman, Sujan Pal, David Gochis, and Kevin Sampson</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3148,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3148,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123906" data-show=".short_summary_123906" data-hide=".short_summary_button_123906" >Short summary</span> <div class="j-widget__max short_summary short_summary_123906" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Including lateral flow increases evapotranspiration near major river channels in high-resolution land surface simulations in southeast Australia, consistent with observations. The 1-km resolution model shows a widespread pattern of dry ridges that does not exist at coarser resolutions. Our results have implications for improved simulations of droughts and future water availability. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123906" data-show=".short_summary_button_123906">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"> 18 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3260/">Understanding Boreal Summer UTLS Water Vapor Variations in Monsoon Regions: A Lagrangian Perspective</a> <div class="authors">Hongyue Wang, Mijeong Park, Mengchu Tao, Cristina Peña-Ortiz, Nuria Pilar Plaza, Felix Ploeger, and Paul Konopka</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3260,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3260,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124148" data-show=".short_summary_124148" data-hide=".short_summary_button_124148" >Short summary</span> <div class="j-widget__max short_summary short_summary_124148" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> We investigated how stratospheric water vapor behaves over the Asian and North American monsoons. Using a method that tracks air movement, we recreated the moisture patterns. Our results show that the moisture in monsoon regions is primarily controlled by largescale air temperatures, while the North American monsoon is influenced by distant transport. These findings enhance our understanding of summertime stratospheric water vapor changes and offer insights into climate feedback mechanisms. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124148" data-show=".short_summary_button_124148">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"> 18 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3154/">Geo-Informatics Data Acquisition Instrument for Assessment of Avalanche Risk and Trafficability: STMET</a> <div class="authors">Ganesh Kumar and Zorawar Singh</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3154,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3154,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123921" data-show=".short_summary_123921" data-hide=".short_summary_button_123921" >Short summary</span> <div class="j-widget__max short_summary short_summary_123921" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> The paper introduces the design and data acquisition system of the instrument named Snow Terrain and Mobility Evaluation Tool (STMET). As a multipurpose instrument, STMET will purge the hauling of separate equipment during the movement in the difficult snow-bound regions helping in easy mobility and collection of crucial parameters for avalanche defence. The instrument presented in this paper can replace traditional instruments like Cone Penetrometers, Ramsonde and even SnowMicropen. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123921" data-show=".short_summary_button_123921">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"> 18 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3129/">Non-biting midges (<em>Chironomidae</em>) as a proxy for summer temperatures during the post-Holsteinian (MIS 11b) – a central European perspective</a> <div class="authors">Tomasz Polkowski, Agnieszka Gruszczyńska, Bartosz Kotrys, Artur Górecki, Anna Hrynowiecka, Marcin Żarski, Mirosław Błaszkiewicz, Jerzy Nitychoruk, Monika Czajkowska, Stefan Lauterbach, and Michał Słowiński</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3129,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3129,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_123859" data-show=".short_summary_123859" data-hide=".short_summary_button_123859" >Short summary</span> <div class="j-widget__max short_summary short_summary_123859" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> In our study, we investigate what changes in environment and climate occured during post-Holsteinian period in Krępa palaeolake in Eastern Poland. In order to achieve this goal we reconstructed summer temperature at that time with the use of Chironomidae larvae head capsules. This is first research from Central Europe in which we use chironomids to trace climate change through pre-Holocenian period. We hope to encourage scientific community to carry out further research in the region. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_123859" data-show=".short_summary_button_123859">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"> 18 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3399/">Dry and warm conditions in Australia exacerbated by aerosol reduction in China</a> <div class="authors">Jiyuan Gao, Yang Yang, Hailong Wang, Pinya Wang, and Hong Liao</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3399,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3399,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124542" data-show=".short_summary_124542" data-hide=".short_summary_button_124542" >Short summary</span> <div class="j-widget__max short_summary short_summary_124542" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> The decline in aerosols in China altered temperature and pressure gradients between the two hemispheres, which intensified the Southern Trade Winds and caused a moisture divergence in Australia, resulting in less rainfall. Reduced surface moisture led to more energy being converted into sensible heat instead of evaporating as latent heat, which raised near-surface temperatures. Our findings offer insights for managing drought and wildfire risks in Australia. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124542" data-show=".short_summary_button_124542">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"> 18 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3412/">Hunga Tonga-Hunga Ha’apai Volcano Impact Model Observation Comparison (HTHH-MOC) Project: Experiment Protocol and Model Descriptions</a> <div class="authors">Yunqian Zhu, Hideharu Akiyoshi, Valentina Aquila, Elisabeth Asher, Ewa M. Bednarz, Slimane Bekki, Christoph Brühl, Amy H. Butler, Parker Case, Simon Chabrillat, Gabriel Chiodo, Margot Clyne, Lola Falletti, Peter R. Colarco, Eric Fleming, Andrin Jörimann, Mahesh Kovilakam, Gerbrand Koren, Ales Kuchar, Nicolas Lebas, Qing Liang, Cheng-Cheng Liu, Graham Mann, Michael Manyin, Marion Marchand, Olaf Morgenstern, Paul Newman, Luke D. Oman, Freja F. Østerstrøm, Yifeng Peng, David Plummer, Ilaria Quaglia, William Randel, Samuel Rémy, Takashi Sekiya, Stephen Steenrod, Timofei Sukhodolov, Simone Tilmes, Kostas Tsigaridis, Rei Ueyama, Daniele Visioni, Xinyue Wang, Shingo Watanabe, Yousuke Yamashita, Pengfei Yu, Wandi Yu, Jun Zhang, and Zhihong Zhuo</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3412,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3412,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124574" data-show=".short_summary_124574" data-hide=".short_summary_button_124574" >Short summary</span> <div class="j-widget__max short_summary short_summary_124574" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> To understand the climate impact of the 2022 Hunga volcanic eruption, we developed a climate model-observation comparison project. The paper describes the protocols and models that participate in the experiments. We designed several experiments to achieve our goal of this activity: 1. evaluate the climate model performance; 2. understand the Earth system responses to this eruption. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124574" data-show=".short_summary_button_124574">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"> 18 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3340/">The 3D <em>Q</em><sub>p</sub> Model of the China Seismic Experiment Site (CSES-<em>Q</em>1.0) and Its Tectonic Implications</a> <div class="authors">Mengqiao Duan, Lianqing Zhou, Ying Fu, Yanru An, Jingqiong Yang, and Xiaodong Zhang</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3340,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3340,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 0 comments</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124437" data-show=".short_summary_124437" data-hide=".short_summary_button_124437" >Short summary</span> <div class="j-widget__max short_summary short_summary_124437" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> Local seismic tomography yields the highest-resolution 3D <em>Q</em><sub>p</sub> model in CSES. Low <em>Q</em><sub>p</sub> anomalies along faults and basins indicate high medium fragmentation, thick sediments, or fluid richness. Tengchong volcano's westward dipping high attenuation suggests magma flow. Most M6+ earthquakes occur in low attenuation zones or anomaly boundaries. The 2008 Wenchuan <em>M</em><sub>S</sub> 8.0 and 2013 Lushan <em>M</em><sub>S</sub> 7.0 epicenters were separated by a low attenuation area, indicating future major earthquake risks. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124437" data-show=".short_summary_button_124437">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"> 18 Nov 2024</div> <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3353/">Enhancing physically based and distributed hydrological model calibration through internal state variable constraints</a> <div class="authors">Frédéric Talbot, Jean-Daniel Sylvain, Guillaume Drolet, Annie Poulin, and Richard Arsenault</div> <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2024-3353,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2024-3353,</span> 2024</div> <div class="statusMessage"><strong>Discussion: open, 1 comment</strong></div> <span class="show-hide journal-contentLinkColor triangle short_summary_button_124459" data-show=".short_summary_124459" data-hide=".short_summary_button_124459" >Short summary</span> <div class="j-widget__max short_summary short_summary_124459" style="display: none"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content"> This research explores different modelling approaches within a distributed and physically based hydrological model, emphasizing configurations that integrate groundwater recharge and dynamics. The study demonstrates that precise adjustments in model calibration can enhance the accuracy and representation of hydrological variables, which are crucial for effective water management and climate change adaptation strategies. </div> <div><a href="#" class="show-hide triangle" data-hide=".short_summary_124459" data-show=".short_summary_button_124459">Hide</a></div> </div> </div> </div> <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> </div> </div>  <div class="pswp" tabindex="-1" role="dialog" aria-hidden="true" >  <div class="pswp__bg"></div>  <div class="pswp__scroll-wrap">  <div class="pswp__container"> <div class="pswp__item"></div> <div class="pswp__item"></div> <div class="pswp__item"></div> </div>  <div class="pswp__ui pswp__ui--hidden"> <div class="pswp__top-bar">  <div class="pswp__counter"></div> <button class="pswp__button pswp__button--close" title="Close (Esc)"></button> <button class="pswp__button pswp__button--fs" title="Toggle fullscreen"></button>   <div class="pswp__preloader"> <div class="pswp__preloader__icn"> <div class="pswp__preloader__cut"> <div class="pswp__preloader__donut"></div> </div> </div> </div> </div> <div class="pswp__share-modal pswp__share-modal--hidden pswp__single-tap"> <div class="pswp__share-tooltip"></div> </div> <button class="pswp__button pswp__button--arrow--left" title="Previous (arrow left)"> </button> <button class="pswp__button pswp__button--arrow--right" title="Next (arrow right)"> </button> <div class="pswp__caption "> <div class="pswp__caption__center"></div> </div> </div> </div> </div> <script> $(function (){ $('.recent-selection-wrapper button').click((event) => { event.preventDefault(); event.stopPropagation(); event.stopImmediatePropagation(); let currentElement = event.currentTarget; $("html, body").animate({ scrollTop: $('.breadcrumb').offset().top }, "slow"); return false; }); }); </script>  <a rel="license" style="display: none" href="https://creativecommons.org/licenses/by/4.0/">CC BY 4.0</a> </div> </div>  </div> </div> </main>  <footer class="d-print-none version-2023"> <div class="footer"> <div class="container"> <div class="row align-items-center mb-3"> <div class="col-12 col-lg-auto text-center text-md-left title-wrapper"> <div id="j-header-footer" class="text-center text-md-left"> <div class="h1 text-center text-md-left"> EGUsphere </div> <p>The preprint repository of the EGU</p> </div> </div> <div class="col-12 col-lg-auto text-center text-md-left pt-lg-2"> <div class="row align-items-center"> <div class="col-12 col-sm col-md-auto text-center text-md-left mb-3 mb-sm-0"> <span class="egu-logo"><a href="http://www.egu.eu/" target="_blank"><img src="https://contentmanager.copernicus.org/319373/778/ssl" alt="" style="width: 410px; height: 325px;" /></a></span> </div> <div class="col-12 col-sm text-center text-md-left"> <span class="copernicus-logo"><a href="https://publications.copernicus.org/" target="_blank"><img src="https://contentmanager.copernicus.org/319376/778/ssl" alt="" style="width: 1784px; height: 330px;" /></a></span> </div> </div> </div> </div> </div> </div> <div class="links pb-4 pt-4"> <div class="container"> <div class="row align-items-center"> <div class="col-12 col-xl-auto mt-3"> <div class="row align-items-start align-items-lg-center"> <div class="col-12 mb-3 mb-md-0 pl-md-0 text-center text-md-left"><a href="https://creativecommons.org/licenses/by/4.0/" target="_blank"><i class="fab fa-creative-commons fa-lg mr-1"></i><i class="fab fa-creative-commons-by fa-lg"></i></a> All site content, except where otherwise noted, is licensed under the <a href="https://creativecommons.org/licenses/by/4.0/" target="_blank">Creative Commons Attribution 4.0 License</a>.</div> </div> </div> <div class="col-12 text-center text-md-left col-lg-auto mt-3"> <div class="row align-items-center"> <div class="col d-md-none px-0"></div> <div class="col-auto pr-1"><a href="https://www.egusphere.net/about/contact.html">Contact</a></div> <div class="col-auto px-1">|</div> <div class="col-auto px-1"><a href="https://www.egusphere.net/imprint.html">Imprint</a></div> <div class="col-auto px-1">|</div> <div class="col-auto px-1"><a href="https://www.copernicus.org/data_protection.html" target="_blank">Data protection</a></div> <div class="col-auto pl-2"><a class="twitter-follow-button" target="_blank" href="https://twitter.com/egusphere"><i class="fab fa-square-x-twitter fa-2x"></i></a></div> <div class="col d-md-none px-0"></div> </div> </div> </div> </div> </div> </footer> </body> </html> <style>#egusphere-search{display:block!important;}</style>

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