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804 picturesGallery(); 805 } else if (mutation.type === "attributes") { 806 // console.log(`The ${mutation.attributeName} attribute was modified.`); 807 } 808 } 809 }; 810 811 // Create an observer instance linked to the callback function 812 const observer = new MutationObserver(callbackSearchModal); 813 814 // Start observing the target node for configured mutations 815 observer.observe(targetNodeSearchModal, configSearchModal); 816 817 function _addEventListener() 818 { 819 document.getElementById('search_query_solr').addEventListener('keypress', (e) => { 820 if (e.key === 'Enter') 821 _runSearch(); 822 }); 823 document.getElementById('start_site_search_solr').addEventListener('click', (e) => { 824 _runSearch(); 825 e.stopPropagation(); 826 e.stopImmediatePropagation(); 827 return false; 828 }); 829 830 $('#templateSearchResultModal').scroll(function() { 831 if ($(this).scrollTop()) { 832 $('#scrolltopmodal:hidden').stop(true, true).fadeIn().css("display","inline-block"); 833 } else { 834 $('#scrolltopmodal').stop(true, true).fadeOut(); 835 } 836 }); 837 838 } 839 840 function scrollModalTop() 841 { 842 $('#templateSearchResultModal').animate({ scrollTop: 0 }, 'slow'); 843 // $('#templateSearchResultModal').scrollTop(0); 844 845 } 846 847 function picturesGallery() 848 { 849 $('body').off('click', '.paperlist-avatar img'); 850 $('body').off('click', '#templateSearchResultContainer .paperlist-avatar img'); 851 searchPaperListAvatar = []; 852 searchPaperListAvatarThumb = []; 853 search_pswpElement = document.querySelectorAll('.pswp')[0]; 854 if (typeof search_gallery != "undefined") { 855 search_gallery = null; 856 } 857 $('body').on('click', '#templateSearchResultContainer .paperlist-avatar img', function (e) { 858 if(searchPaperListAvatarThumb.length === 0 && searchPaperListAvatar.length === 0) { 859 $('#templateSearchResultContainer .paperlist-avatar img').each(function () { 860 861 var webversion = $(this).attr('data-web'); 862 var width = $(this).attr('data-width'); 863 var height = $(this).attr('data-height'); 864 var caption = $(this).attr('data-caption'); 865 866 var figure = { 867 src: webversion, 868 w: width, 869 h: height, 870 title: caption 871 }; 872 searchPaperListAvatarThumb.push($(this)[0]); 873 searchPaperListAvatar.push(figure); 874 }); 875 } 876 var target = $(this); 877 var index = $('#templateSearchResultContainer .paperlist-avatar img').index(target); 878 var options = { 879 showHideOpacity:false, 880 bgOpacity:0.8, 881 index:index, 882 spacing:0.15, 883 history: false, 884 focus:false, 885 getThumbBoundsFn: function(index) { 886 var thumbnail = searchPaperListAvatarThumb[index]; 887 var pageYScroll = window.pageYOffset || document.documentElement.scrollTop; 888 var rect = thumbnail.getBoundingClientRect(); 889 return {x:rect.left, y:rect.top + pageYScroll, w:rect.width}; 890 } 891 }; 892 search_gallery = new PhotoSwipe( search_pswpElement, PhotoSwipeUI_Default,[searchPaperListAvatar[index]],options); 893 search_gallery.init(); 894 }); 895 } 896 function showError(code, msg) 897 { 898 console.error(code, msg); 899 900 $("#templateSearchLoadingModal").modal("hide"); 901 902 switch(code) 903 { 904 case -3: // http request fail 905 case -2: // invalid MO response 906 case 4: // CORS 907 case 1: // project 908 $("#templateSearchErrorModal1").modal({}); 909 break; 910 case -1: // timeout 911 $("#templateSearchErrorModal2").modal({}); 912 break; 913 case 2: // empty term 914 $("#templateSearchErrorModal3").modal({}); 915 break; 916 case 3: // DOS 917 $("#templateSearchErrorModal4").modal({}); 918 break; 919 default: 920 $("#templateSearchErrorModal1").modal({}); 921 break; 922 } 923 } 924 function clearForm() { 925 var myFormElement = document.getElementById("library-filters") 926 var elements = myFormElement.elements; 927 $(".form-check-input").prop('checked', false).change().parent().removeClass('active'); 928 for(i=0; i<elements.length; i++) { 929 field_type = elements[i].type.toLowerCase(); 930 switch(field_type) { 931 case "text": 932 case "password": 933 case "textarea": 934 case "hidden": 935 elements[i].value = ""; 936 break; 937 case "radio": 938 case "checkbox": 939 if (elements[i].checked) { 940 elements[i].checked = false; 941 } 942 break; 943 944 case "select-one": 945 case "select-multi": 946 elements[i].selectedIndex = -1; 947 break; 948 949 default: 950 break; 951 } 952 } 953 } 954 955 function generateShowMoreButton(offset, term) 956 { 957 var code = '<button aria-label="ShowMore" id="showMore" class="btn btn-success float-right mr-2" data-offset="' + offset + '">Show more</button>'; 958 return code; 959 } 960 961 function hideModal(id) 962 { 963 $("#"+id).modal('hide'); 964 } 965 966 function showModal(id) 967 { 968 $("#"+id).modal({}); 969 } 970 971 function prepareForPhotoSwipe() 972 { 973 searchPaperListAvatar = []; 974 searchPaperListAvatarThumb = []; 975 search_pswpElement = document.querySelectorAll('.pswp')[0]; 976 } 977 978 function _sendAjax(projectID, term) 979 { 980 let httpRequest = new XMLHttpRequest(); 981 if(searchRunning) 982 { 983 console.log("Search running"); 984 return; 985 } 986 987 if (!httpRequest) { 988 console.error("Giving up :( Cannot create an XMLHTTP instance"); 989 showError(-1); 990 return false; 991 } 992 993 // httpRequest.timeout = 20000; // time in milliseconds 994 httpRequest.withCredentials = false; 995 httpRequest.ontimeout = (e) => { 996 showError(-1, "result timeout"); 997 searchRunning = false; 998 }; 999 httpRequest.onreadystatechange = function() 1000 { 1001 if (httpRequest.readyState === XMLHttpRequest.DONE) 1002 { 1003 searchRunning = false; 1004 1005 if (httpRequest.status === 200) { 1006 let rs = JSON.parse(httpRequest.responseText); 1007 if(rs) 1008 { 1009 if(rs.isError) 1010 { 1011 showError(rs.errorCode, rs.errorMessage); 1012 } 1013 else 1014 { 1015 let html = rs.resultHTMLs; 1016 $("#modal_search_query").val(rs.term); 1017 $("#templateSearchResultTerm").html(rs.term); 1018 $("#templateSearchResultNr").html(rs.resultsNr); 1019 $("#templateRefineSearch").html(rs.filter); 1020 if(rs.filter == false) 1021 { 1022 console.log('filter empty'); 1023 $("#refineSearchModal").removeClass('d-block').addClass('d-none'); 1024 } 1025 1026 if(rs.resultsNr==1) 1027 $("#templateSearchResultNrPlural").hide(); 1028 else 1029 $("#templateSearchResultNrPlural").show(); 1030 if(rs.resultsNr==0) 1031 { 1032 hideModal('templateSearchLoadingModal'); 1033 $("#templateSearchResultContainer").html(""); 1034 $("#templateSearchResultContainerEmpty").removeClass("d-none"); 1035 showModal('templateSearchResultModal'); 1036 } 1037 else 1038 { 1039 if((rs.resultsNr - offset)>0) 1040 { 1041 html = html + generateShowMoreButton(offset, term); 1042 } 1043 $("#templateSearchResultContainerEmpty").addClass("d-none"); 1044 if( offset == INITIAL_OFFSET) 1045 { 1046 hideModal('templateSearchLoadingModal'); 1047 $("#templateSearchResultContainer").html(html); 1048 showModal('templateSearchResultModal'); 1049 } 1050 else 1051 { 1052 $('#showMore').remove(); 1053 startHtml = $("#templateSearchResultContainer").html(); 1054 $("#templateSearchResultContainer").html(startHtml + html); 1055 } 1056 // prepareForPhotoSwipe(); 1057 } 1058 } 1059 } 1060 else 1061 { 1062 showError(-2, "invalid result"); 1063 } 1064 } else { 1065 showError(-3, "There was a problem with the request."); 1066 } 1067 } 1068 }; 1069 if(offset == INITIAL_OFFSET) 1070 { 1071 hideModal('templateSearchResultModal'); 1072 showModal('templateSearchLoadingModal'); 1073 } 1074 1075 httpRequest.open("GET", FINDER_URL+"?project="+projectID+"&term="+encodeURI(term)+((offset>INITIAL_OFFSET)?("&offset="+(offset-INITIAL_OFFSET)) : "")); 1076 httpRequest.send(); 1077 searchRunning = true; 1078 } 1079 1080 function _runSearch() 1081 { 1082 var projectID = document.querySelector('meta[name="global_projectID"]').content; 1083 var term = _searchTrimInput(SEARCH_INPUT.value); 1084 1085 if(term.length > 0) 1086 { 1087 _sendAjax(projectID, term); 1088 } 1089 else 1090 { 1091 showError(2, 'Empty search term') 1092 } 1093 } 1094 function _searchTrimInput(str) { 1095 return str.replace(/^\s+|\s+$/gm, ''); 1096 } 1097 1098 function run() 1099 { 1100 _addEventListener(); 1101 1102 $('#templateSearchInfoBtn, #modalSearchInfoBtn').popover({ 1103 sanitize: false, 1104 html: true, 1105 content: $("#templateSearchInfo").html(), 1106 placement: "bottom", 1107 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>', 1108 title: "Search tips", 1109 }); 1110 $(document).click(function (e) { 1111 let t = $(e.target); 1112 let a = t && t.attr("data-toggle")!=="popover" && t.parent().attr("data-toggle")!=="popover"; 1113 let b = t && $(".popover").has(t).length===0; 1114 if(a && b) 1115 { 1116 $('#templateSearchInfoBtn').popover('hide'); 1117 $('#modalSearchInfoBtn').popover('hide'); 1118 } 1119 }); 1120 $('#templateSearchInfoBtn').on('shown.bs.popover', function () { 1121 $("#templateSearchInfoClose").click(function(e){
1122 $('#templateSearchInfoBtn').popover('hide'); 1123 e.stopPropagation(); 1124 e.stopImmediatePropagation(); 1125 return false; 1126 }); 1127 }) 1128 $('#templateSearchResultModal').on('hidden.bs.modal', function(e) { 1129 $('body').off('click', '#templateSearchResultContainer .paperlist-avatar img'); 1130 var pswpElement = document.querySelectorAll('.pswp')[0]; 1131 var gallery = null; 1132 var paperListAvatar = []; 1133 var paperListAvatarThumb = []; 1134 $('.paperlist-avatar img').each(function(){ 1135 var webversion = $(this).attr('data-web'); 1136 var width = $(this).attr('data-width'); 1137 var height = $(this).attr('data-height'); 1138 var caption =$(this).attr('data-caption'); 1139 1140 var figure = { 1141 src:webversion, 1142 w:width, 1143 h:height, 1144 title:caption 1145 }; 1146 paperListAvatarThumb.push($(this)[0]); 1147 paperListAvatar.push(figure); 1148 }); 1149 $('body').on('click', '.paperlist-avatar img', function (e) { 1150 if(paperListAvatarThumb.length === 0 && paperListAvatar.length === 0){ 1151 $('.paperlist-avatar img').each(function(){ 1152 var webversion = $(this).attr('data-web'); 1153 var width = $(this).attr('data-width'); 1154 var height = $(this).attr('data-height'); 1155 var caption =$(this).attr('data-caption'); 1156 1157 var figure = { 1158 src:webversion, 1159 w:width, 1160 h:height, 1161 title:caption 1162 }; 1163 paperListAvatarThumb.push($(this)[0]); 1164 paperListAvatar.push(figure); 1165 }); 1166 } 1167 var target = $(this); 1168 var index = $('.paperlist-avatar img').index(target); 1169 var options = { 1170 showHideOpacity:true, 1171 bgOpacity:0.8, 1172 index:index, 1173 spacing:0.15, 1174 getThumbBoundsFn: function(index) { 1175 1176 var thumbnail = paperListAvatarThumb[index]; 1177 var pageYScroll = window.pageYOffset || document.documentElement.scrollTop; 1178 var rect = thumbnail.getBoundingClientRect(); 1179 return {x:rect.left, y:rect.top + pageYScroll, w:rect.width}; 1180 } 1181 }; 1182 gallery = new PhotoSwipe( pswpElement, PhotoSwipeUI_Default,[paperListAvatar[index]],options); 1183 gallery.init(); 1184 }); 1185 1186 }); 1187 $('#templateSearchResultModal').on('hide.bs.modal', function(e) { 1188 $("#templateRefineSearch").removeClass('d-block').addClass('d-none'); 1189 $("#refineSearchModalHide").removeClass('d-block').addClass('d-none'); 1190 $("#refineSearchModal").removeClass('d-none').addClass('d-block'); 1191 offset = INITIAL_OFFSET; 1192 }) 1193 1194 $(document).on("click", "#showMore", function(e){ 1195 offset+=INITIAL_OFFSET; 1196 runSearchModal() 1197 e.stopPropagation(); 1198 e.stopImmediatePropagation(); 1199 return false; 1200 }); 1201 1202 1203 1204 $(document).ready(function() { 1205 $(document).on("click", "#refineSearchModal", function (e) { 1206 $("#templateRefineSearch").removeClass('d-none').addClass('d-block'); 1207 $(this).removeClass('d-block').addClass('d-none'); 1208 $("#refineSearchModalHide").removeClass('d-none').addClass('d-block'); 1209 }); 1210 $(document).on("click", "#refineSearchModalHide", function (e) { 1211 $("#templateRefineSearch").removeClass('d-block').addClass('d-none'); 1212 $(this).removeClass('d-block').addClass('d-none'); 1213 $("#refineSearchModal").removeClass('d-none').addClass('d-block'); 1214 }); 1215 1216 $(document).on("click", "#modal_start_site_search", function (e) { 1217 runSearchModal(); 1218 e.stopPropagation(); 1219 e.stopImmediatePropagation(); 1220 return false; 1221 }); 1222 }); 1223 } 1224 1225 function runSearchModal() 1226 { 1227 var projectID = document.querySelector('meta[name="global_projectID"]').content;
1228 var queryString = $('#library-filters').serialize(); 1229 var term = _searchTrimInput($('#modal_search_query').val()); 1230 term+='&'+queryString; 1231 if(term.length > 0) 1232 { 1233 _sendAjax(projectID, term); 1234 } 1235 else 1236 { 1237 showError(2, 'Empty search term') 1238 } 1239 } 1240 1241 if(document.getElementById('search_query_solr')) 1242 { 1243 run(); 1244 } 1245 1246</script>
1246 1247<!-- END_SITE_SEARCH --></div></div> 1248 1249 <!-- END_SNIPPET:part10 --> 1250 1251 </div> 1252 1253 </div> 1254 1255 </div> 1256 1257 </div> 1258 1259</header> 1260 1261<!--=== Content ===--> 1262 1263<main class="one-column version-2023"> 1264 1265 <div id="content" class="container"> 1266 1267 <div id="page_content_container" class="CMSCONTAINER content-container"> 1268 1269 <!-- $$CONTENT$$ --> 1270 1271 <!-- START_LEFT_REMOVABLE_SECTION --> 1272 1273 <!-- END_LEFT_REMOVABLE_SECTION --> 1274 1275 <div id="landing_page" class="cmsbox j-intro-section j-section"><div class="row mt-1"> 1276 <div class="col-12 d-xl-none mt-1"> 1277 <div class="row service_icons mb-3"> 1278 <a href="https://www.the-cryosphere.net/recent_papers.html" class="col-auto pr-0"> 1279 <img src="https://www.the-cryosphere.net/icon_open_access.svg" title="Open access" alt="Open access" /></a> 1280 <a href="https://www.the-cryosphere.net/peer_review/interactive_review_process.html" class="col-auto pr-0"> 1281 <img src="https://www.the-cryosphere.net/icon_public_peer_review.svg" title="Public peer review" alt="Public peer review" /></a> 1282 <a href="https://www.the-cryosphere.net/about/article_level_metrics.html" class="col-auto pr-0 d-none d-md-inline-block"> 1283 <img src="https://www.the-cryosphere.net/icon_article_level_metrics.svg" title="Article level metrics" alt="Article level metrics" /></a> 1284 <a href="https://www.the-cryosphere.net/about/article_processing_charges.html" class="col-auto pr-0 d-none d-xxl-inline-block"> 1285 <img src="https://www.the-cryosphere.net/icon_moderateAPCs.svg" title="Moderate APCs" alt="Moderate APCs" /></a> 1286 </div> 1287 </div> 1288 <div class="col-auto d-none d-lg-block img-responsive"> 1289 <img data-toggle="modal" data-target="#coverModal" class="hover-cursor-pointer" src="https://www.the-cryosphere.net/tc_cover_homepage.png" cofileid="12610" alt="TC cover" title="TC cover" /> 1290 </div> 1291 <div class="col pl-lg-0 mt-1"> 1292 <div class="row service_icons mb-3 d-none d-xl-block"> 1293 <a href="https://www.the-cryosphere.net/recent_papers.html" class="col-auto pr-0"> 1294 <img src="https://www.the-cryosphere.net/icon_open_access.svg" title="Open access" alt="Open access" /></a> 1295 <a href="https://www.the-cryosphere.net/peer_review/interactive_review_process.html" class="col-auto pr-0"> 1296 <img src="https://www.the-cryosphere.net/icon_public_peer_review.svg" title="Public peer review" alt="Public peer review" /></a> 1297 <a href="https://www.the-cryosphere.net/about/article_level_metrics.html" class="col-auto pr-0 d-none d-md-inline-block"> 1298 <img src="https://www.the-cryosphere.net/icon_article_level_metrics.svg" title="Article level metrics" alt="Article level metrics" /></a> 1299 <a href="https://www.the-cryosphere.net/about/article_processing_charges.html" class="col-auto pr-0 d-none d-xxl-inline-block"> 1300 <img src="https://www.the-cryosphere.net/icon_moderateAPCs.svg" title="Moderate APCs" alt="Moderate APCs" /></a> 1301 <a href="https://www.the-cryosphere.net/about/financial_support.html" class="col-auto pr-0 d-none d-xxl-inline-block"> 1302 <img src="https://www.the-cryosphere.net/icon_financial_support.svg" title="Financial support" alt="Financial support" /></a> 1303 1304 </div> 1305 <div class="row"> 1306 <div class="col-12 font-weight-bold">Co-editors-in-chief: Caroline Clason, Chris Derksen, Christian Haas, Christian Hauck, Nanna Bjørnholt Karlsson & Hanna Lee</div> 1307 </div> 1308<div class="row mb-3"> 1309 <div class="col-12"> 1310 eISSN: <span class="" id="cmsvar_111">1994-0424</span> 1311 </div> 1312</div> 1313 <div class="row"> 1314 <div class="col-12"> 1315 <p class="font-weight-normal"> 1316 The Cryosphere (TC) is a not-for-profit international scientific journal dedicated to the publication and discussion of research articles, short communications, and review papers on all aspects of frozen water and frozen ground on Earth and on other planetary bodies. 1317 </p> 1318 <p class="font-weight-normal"> 1319 The main subject areas are ice sheets and glaciers, permafrost, river and lake ice, seasonal snow cover, and sea ice, including remote sensing, numerical modeling, in situ, and laboratory approaches, and studies of the interaction of the cryosphere with the Earth system. Manuscripts with a focus on cryospheric research that include perspectives from social science, humanities, and other disciplines outside the natural sciences are also welcome. 1320 </p> 1321 </div> 1322 </div> 1323 </div> 1324</div> 1325<div id="coverModal" class="modal fade" tabindex="-1" role="dialog" aria-hidden="true"> 1326 <div class="modal-dialog"> 1327 <div class="modal-content"> 1328 <div class="modal-header"> 1329 <button type="button" class="close" data-dismiss="modal" aria-label="Close">
1330 <span aria-hidden="true">Ã</span> 1331 </button> 1332 </div> 1333 <div class="container-fluid"> 1334 <div class="row"> 1335 <div class="col-12 p-3"> 1336 <img class="img-fluid" alt="TC cover enlarged" cofileid="20466" src="https://www.the-cryosphere.net/graphic_TC_cover_huge.jpg" /> 1337 </div> 1338 </div> 1339 </div> 1340 </div> 1341 </div> 1342</div></div><div id="cmsbox_126157" class="cmsbox "><h2>Journal metrics</h2> 1343<p>TC is indexed in the Web of Science, Scopus, Google Scholar, etc. We refrain from displaying the journal metrics prominently on the landing page since citation metrics used in isolation do not describe importance, impact, or quality of a journal. However, these metrics can be found on the <a href="https://www.the-cryosphere.net/about/journal_metrics.html">journal metrics page</a>.</p></div><div id="news_container" class="cmsbox "> <h2>News</h2> 1344 <div class="grid-container paperlist-object"> 1345 <div class="hide-on-desktop hide-on-tablet mobile-grid-100"> 1346 <a class="no-border paperlist-avatar-unclickable" target="_blank" href="https://www.copernicus.org/news_and_press/2026-06-30_the-norwegian-university-of-science-and-technology-partners-with-copernicus-publications-to-support-open-access-publishing.html"><img alt="" cofileid="2732113" src="https://www.the-cryosphere.net/ntnu-logo.svg" width="80px"/></a> 1347 </div> 1348 <div class="hide-on-desktop hide-on-tablet mobile-grid-100"> 1349 <span class="published-date">30 Jun 2026</span> 1350 <a target="_blank" href="https://www.copernicus.org/news_and_press/2026-06-30_the-norwegian-university-of-science-and-technology-partners-with-copernicus-publications-to-support-open-access-publishing.html" class="article-title">The Norwegian University of Science and Technology partners with Copernicus Publications to support open-access publishing</a> 1351 <p class="citation">Copernicus Publications has signed a new institutional agreement with Norwegian University of Science and Technology (NTNU). Please read more. <a target="_blank" href="https://www.copernicus.org/news_and_press/2026-06-30_the-norwegian-university-of-science-and-technology-partners-with-copernicus-publications-to-support-open-access-publishing.html"><img cofileid="17978" alt="" src="https://www.the-cryosphere.net/graphic_grey_right_symbol.png"></a></p> 1352 </div> 1353 <div class="grid-85 tablet-grid-85 hide-on-mobile"> 1354 <span class="published-date">30 Jun 2026</span> 1355 <a target="_blank" href="https://www.copernicus.org/news_and_press/2026-06-30_the-norwegian-university-of-science-and-technology-partners-with-copernicus-publications-to-support-open-access-publishing.html" class="article-title">The Norwegian University of Science and Technology partners with Copernicus Publications to support open-access publishing</a> 1356 <p class="citation">Copernicus Publications has signed a new institutional agreement with Norwegian University of Science and Technology (NTNU). Please read more. <a target="_blank" href="https://www.copernicus.org/news_and_press/2026-06-30_the-norwegian-university-of-science-and-technology-partners-with-copernicus-publications-to-support-open-access-publishing.html"><img cofileid="17978" alt="" src="https://www.the-cryosphere.net/graphic_grey_right_symbol.png"></a></p> 1357 </div> 1358 <div class="grid-15 tablet-grid-15 hide-on-mobile text-right"> 1359 <a class="no-border paperlist-avatar-unclickable" target="_blank" href="https://www.copernicus.org/news_and_press/2026-06-30_the-norwegian-university-of-science-and-technology-partners-with-copernicus-publications-to-support-open-access-publishing.html"><img alt="" cofileid="2732113" src="https://www.the-cryosphere.net/ntnu-logo.svg" width="80px"/></a> 1360 </div> 1361 <div class="hide-on-desktop hide-on-tablet mobile-grid-100"> 1362 <a class="paperlist-avatar-unclickable" target="" href="https://www.the-cryosphere.net/about/news_and_press/2026-04-30_greek-mountain-snow-cover-halved-in-past-four-decades-due-to-regional-warming.html"><img alt="" cofileid="2713976" src="https://www.the-cryosphere.net/tc-20-2209-2026-key-figure-80x80.png" width="80px"/></a> 1363 </div> 1364 <div class="hide-on-desktop hide-on-tablet mobile-grid-100">
1365 <span class="published-date">30 Apr 2026</span> 1366 <a target="" href="https://www.the-cryosphere.net/about/news_and_press/2026-04-30_greek-mountain-snow-cover-halved-in-past-four-decades-due-to-regional-warming.html" class="article-title">Greek mountain snow cover halved in past four decades due to regional warming</a> 1367 <p class="citation">The authors' research shows that Greece's highest mountains have lost half of their winter snow over the past four decades. Using a new model that reconstructs daily snow cover from satellite and climate data, they found a rapid and widespread decline driven mainly by rising temperatures. Please read more. <a target="" href="https://www.the-cryosphere.net/about/news_and_press/2026-04-30_greek-mountain-snow-cover-halved-in-past-four-decades-due-to-regional-warming.html"><img cofileid="17978" alt="" src="https://www.the-cryosphere.net/graphic_grey_right_symbol.png"></a></p> 1368 </div> 1369 <div class="grid-85 tablet-grid-85 hide-on-mobile"> 1370 <span class="published-date">30 Apr 2026</span> 1371 <a target="" href="https://www.the-cryosphere.net/about/news_and_press/2026-04-30_greek-mountain-snow-cover-halved-in-past-four-decades-due-to-regional-warming.html" class="article-title">Greek mountain snow cover halved in past four decades due to regional warming</a> 1372 <p class="citation">The authors' research shows that Greece's highest mountains have lost half of their winter snow over the past four decades. Using a new model that reconstructs daily snow cover from satellite and climate data, they found a rapid and widespread decline driven mainly by rising temperatures. Please read more. <a target="" href="https://www.the-cryosphere.net/about/news_and_press/2026-04-30_greek-mountain-snow-cover-halved-in-past-four-decades-due-to-regional-warming.html"><img cofileid="17978" alt="" src="https://www.the-cryosphere.net/graphic_grey_right_symbol.png"></a></p> 1373 </div> 1374 <div class="grid-15 tablet-grid-15 hide-on-mobile text-right"> 1375 <a class=" paperlist-avatar-unclickable" target="" href="https://www.the-cryosphere.net/about/news_and_press/2026-04-30_greek-mountain-snow-cover-halved-in-past-four-decades-due-to-regional-warming.html"><img alt="" cofileid="2713976" src="https://www.the-cryosphere.net/tc-20-2209-2026-key-figure-80x80.png" width="80px"/></a> 1376 </div> 1377 <div class="hide-on-desktop hide-on-tablet mobile-grid-100"> 1378 <a class="no-border paperlist-avatar-unclickable" target="_blank" href="https://www.egu.eu/news/1740/bringing-so-called-negative-results-into-interactive-open-access-publications-with-the-new-egu-manuscript-formats-lessons-limitations-errors-surprises-shortcomings-and-opportunities-for-new-science/"><img alt="" cofileid="454898" src="https://www.the-cryosphere.net/graphic-logo-egu-80px.png" width="80px"/></a> 1379 </div> 1380 <div class="hide-on-desktop hide-on-tablet mobile-grid-100"> 1381 <span class="published-date">28 Apr 2026</span> 1382 <a target="_blank" href="https://www.egu.eu/news/1740/bringing-so-called-negative-results-into-interactive-open-access-publications-with-the-new-egu-manuscript-formats-lessons-limitations-errors-surprises-shortcomings-and-opportunities-for-new-science/" class="article-title">Bringing so-called 'negative' results into interactive open access publications</a> 1383 <p class="citation">EGU has today introduced a new manuscript type: LESSONS â Limitations, Errors, Surprises, Shortcomings and Opportunities for New Science. Please read more. <a target="_blank" href="https://www.egu.eu/news/1740/bringing-so-called-negative-results-into-interactive-open-access-publications-with-the-new-egu-manuscript-formats-lessons-limitations-errors-surprises-shortcomings-and-opportunities-for-new-science/"><img cofileid="17978" alt="" src="https://www.the-cryosphere.net/graphic_grey_right_symbol.png"></a></p> 1384 </div>
1385 <div class="grid-85 tablet-grid-85 hide-on-mobile"> 1386 <span class="published-date">28 Apr 2026</span> 1387 <a target="_blank" href="https://www.egu.eu/news/1740/bringing-so-called-negative-results-into-interactive-open-access-publications-with-the-new-egu-manuscript-formats-lessons-limitations-errors-surprises-shortcomings-and-opportunities-for-new-science/" class="article-title">Bringing so-called 'negative' results into interactive open access publications</a> 1388 <p class="citation">EGU has today introduced a new manuscript type: LESSONS â Limitations, Errors, Surprises, Shortcomings and Opportunities for New Science. Please read more. <a target="_blank" href="https://www.egu.eu/news/1740/bringing-so-called-negative-results-into-interactive-open-access-publications-with-the-new-egu-manuscript-formats-lessons-limitations-errors-surprises-shortcomings-and-opportunities-for-new-science/"><img cofileid="17978" alt="" src="https://www.the-cryosphere.net/graphic_grey_right_symbol.png"></a></p> 1389 </div> 1390 <div class="grid-15 tablet-grid-15 hide-on-mobile text-right"> 1391 <a class="no-border paperlist-avatar-unclickable" target="_blank" href="https://www.egu.eu/news/1740/bringing-so-called-negative-results-into-interactive-open-access-publications-with-the-new-egu-manuscript-formats-lessons-limitations-errors-surprises-shortcomings-and-opportunities-for-new-science/"><img alt="" cofileid="454898" src="https://www.the-cryosphere.net/graphic-logo-egu-80px.png" width="80px"/></a> 1392 </div> 1393 <div class="j-news-archive-link grid-100 tablet-grid-100 mobile-grid-100"> 1394 <a class="btn btn-primary" href="https://www.the-cryosphere.net/about/news_and_press.html">News archive</a> 1395 </div> 1396 </div> 1397</div><div id="recent_paper" class="cmsbox j-article j-article-section"><div id="recent-paper-content"> 1398 1399 <div id="recent_paper_header"> 1400 <h2>Recent papers</h2> 1401 </div> 1402 <div class="grid-container paperlist-object in-range paperList-final" 1403 data-diff="0"> 1404 <div class="grid-100 hide-on-desktop hide-on-tablet"> 1405 <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/5585/2026/tc-20-5585-2026-avatar-web.png"> 1406 <img class="img-responsive" src="https://tc.copernicus.org/articles/20/5585/2026/tc-20-5585-2026-avatar-thumb80.png" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-web="https://tc.copernicus.org/articles/20/5585/2026/tc-20-5585-2026-avatar-web.png" data-width="600" data-height="371" width="80" height="80"> 1407 1408 </a> 1409 </div> 1410 <div class="grid-85 tablet-grid-85"> 1411 <div class="published-date"> 01 Oct 2026</div> 1412 <a class="article-title" target="_parent" href="https://tc.copernicus.org/articles/20/5585/2026/">Reduced surface hoar in a warming world</a> 1413 <div class="authors">William Rudisill, Dan Feldman, Adrienne Marshall, and Arielle Koshkin</div> 1414 <div class="citation">The Cryosphere, 20, 5585–5607, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/tc-20-5585-2026,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/tc-20-5585-2026,</span> 2026</div> 1415 <span class="show-hide journal-contentLinkColor triangle short_summary_button_138823" 1416 data-show=".short_summary_138823" 1417 data-hide=".short_summary_button_138823" 1418 >Short summary</span> 1419 <div class="j-widget__max short_summary short_summary_138823" style="display: none"> 1420 <div class="widget dark-border"> 1421 <div class="legend journal-contentLinkColor">Short summary</div> 1422 <div class="content"> 1423 Surface hoar crystals occasionally grow on the top of snowpacks overnight. Little work has focused on climatic conditions leading to surface hoar. We use data from three field campaigns in the Colorado Rockies to investigate. We show that surface hoar events decline as the climate warms, and that there may be 14 % fewer events per year in the future. There is still work needed to reconcile measured amounts of surface hoar crystals, models, and the relationship with turbulent air. 1424 </div> 1425 <div><a href="#" class="show-hide triangle" data-hide=".short_summary_138823" 1426 data-show=".short_summary_button_138823">Hide</a></div> 1427 </div> 1428 </div> 1429 </div>
1430 <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> 1431 <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/5585/2026/tc-20-5585-2026-avatar-web.png"> 1432 <img class="img-responsive" src="https://tc.copernicus.org/articles/20/5585/2026/tc-20-5585-2026-avatar-thumb80.png" data-web="https://tc.copernicus.org/articles/20/5585/2026/tc-20-5585-2026-avatar-web.png" data-width="600" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-height="371" width="80" height="80"> 1433 </a> 1434 </div> 1435 </div> 1436 <div class="grid-container paperlist-object in-range paperList-final" 1437 data-diff="0"> 1438 <div class="grid-100 hide-on-desktop hide-on-tablet"> 1439 <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/5559/2026/tc-20-5559-2026-avatar-web.png"> 1440 <img class="img-responsive" src="https://tc.copernicus.org/articles/20/5559/2026/tc-20-5559-2026-avatar-thumb80.png" data-caption="© OpenTopoMap contributors" data-web="https://tc.copernicus.org/articles/20/5559/2026/tc-20-5559-2026-avatar-web.png" data-width="600" data-height="585" width="80" height="80"> 1441 1442 </a> 1443 </div> 1444 <div class="grid-85 tablet-grid-85"> 1445 <div class="published-date"> 30 Sep 2026</div> 1446 <a class="article-title" target="_parent" href="https://tc.copernicus.org/articles/20/5559/2026/">Seven decades of glacier loss on the Nevados de Chillán volcanic complex, Chile</a> 1447 <div class="authors">Millie C. Spencer, Alfonso Fernandez, Emma Tyrrell, Robert Clasing, Enrique Muñoz, Pablo A. Mendoza, Jorge Berkhoff, and Noah P. Molotch</div> 1448 <div class="citation">The Cryosphere, 20, 5559–5583, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/tc-20-5559-2026,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/tc-20-5559-2026,</span> 2026</div> 1449 <span class="show-hide journal-contentLinkColor triangle short_summary_button_135582" 1450 data-show=".short_summary_135582" 1451 data-hide=".short_summary_button_135582" 1452 >Short summary</span> 1453 <div class="j-widget__max short_summary short_summary_135582" style="display: none"> 1454 <div class="widget dark-border"> 1455 <div class="legend journal-contentLinkColor">Short summary</div> 1456 <div class="content"> 1457 Mountain glaciers are important freshwater reservoirs. Quantifying their loss is essential for forecasting water availability. While glacier retreat is well studied in many regions, glacier loss on the Nevados de Chillán volcanic complex in south-central Chile remains uncertain. Using satellite and drone images, we find all 28 glaciers on Nevados de Chillán lost volume over the past 7 decades, with melt rates accelerating markedly since 2000. 1458 </div> 1459 <div><a href="#" class="show-hide triangle" data-hide=".short_summary_135582" 1460 data-show=".short_summary_button_135582">Hide</a></div> 1461 </div> 1462 </div> 1463 </div> 1464 <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> 1465 <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/5559/2026/tc-20-5559-2026-avatar-web.png"> 1466 <img class="img-responsive" src="https://tc.copernicus.org/articles/20/5559/2026/tc-20-5559-2026-avatar-thumb80.png" data-web="https://tc.copernicus.org/articles/20/5559/2026/tc-20-5559-2026-avatar-web.png" data-width="600" data-caption="© OpenTopoMap contributors" data-height="585" width="80" height="80"> 1467 </a> 1468 </div> 1469 </div> 1470 <div class="grid-container paperlist-object type-0 in-range paperList-discussion" 1471 data-diff="0"> 1472 <div class="grid-100 hide-on-desktop hide-on-tablet"> 1473 </div>
1474 <div class="grid-85 tablet-grid-85"> 1475 <div class="published-date"> 30 Sep 2026</div> 1476 <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2026/egusphere-2026-3861/">Distinct and synergistic influences of sea ice rheology and seabed stress on simulated Arctic fast ice</a> 1477 <div class="authors">Augustin Lambotte, Thierry Fichefet, François Massonnet, Pierre Rampal, Laurent Brodeau, Jean-François Lemieux, Frédéric Dupont, Martin Vancoppenolle, Antoine Barthélemy, and Pierre-Yves Barriat</div> 1478 <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2026-3861,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2026-3861,</span> 2026</div> 1479 <div class="statusMessage"><span>Preprint under review for TC</span> <nobr>(discussion: open, 0 comments)</nobr></div> 1480 <span class="show-hide journal-contentLinkColor triangle short_summary_button_143031" 1481 data-show=".short_summary_143031" 1482 data-hide=".short_summary_button_143031" 1483 >Short summary</span> 1484 <div class="j-widget__max short_summary short_summary_143031" style="display: none"> 1485 <div class="widget dark-border"> 1486 <div class="legend journal-contentLinkColor">Short summary</div> 1487 <div class="content"> 1488 Arctic fast ice influences the ocean and is important for Arctic communities and animals. Using the ocean and sea ice model NEMO-SI<sup>3</sup>, we study the interactions between sea ice mechanical formulation and grounding scheme. While the grounding scheme is the most important mechanism, its effect varies with the mechanical formulation. Our results highlight the importance of accurately simulating fast ice thickness and point to future developments for sea ice mechanical frameworks in numerical models. 1489 </div> 1490 <div><a href="#" class="show-hide triangle" data-hide=".short_summary_143031" 1491 data-show=".short_summary_button_143031">Hide</a></div> 1492 </div> 1493 </div> 1494 </div> 1495 <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> 1496 </div> 1497 </div> 1498 <div class="grid-container paperlist-object type-0 in-range paperList-discussion" 1499 data-diff="0"> 1500 <div class="grid-100 hide-on-desktop hide-on-tablet"> 1501 </div> 1502 <div class="grid-85 tablet-grid-85"> 1503 <div class="published-date"> 30 Sep 2026</div> 1504 <a class="article-title" target="_parent" href="https://egusphere.copernicus.org/preprints/2026/egusphere-2026-4857/">Nonlinear-Constrained Geographically Weighted Regression: Enabling Multidimensional Dynamics Analysis Using Monostatic Terrestrial Radar Interferometry at Helheim Glacier</a> 1505 <div class="authors">Chentong Zhang, Xianwei Wang, Yi Zhou, David M. Holland, and Denise Holland</div> 1506 <div class="citation">EGUsphere, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/egusphere-2026-4857,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/egusphere-2026-4857,</span> 2026</div> 1507 <div class="statusMessage"><span>Preprint under review for TC</span> <nobr>(discussion: open, 0 comments)</nobr></div> 1508 <span class="show-hide journal-contentLinkColor triangle short_summary_button_145317" 1509 data-show=".short_summary_145317" 1510 data-hide=".short_summary_button_145317" 1511 >Short summary</span> 1512 <div class="j-widget__max short_summary short_summary_145317" style="display: none"> 1513 <div class="widget dark-border"> 1514 <div class="legend journal-contentLinkColor">
1514Short summary</div> 1515 <div class="content"> 1516 Monostatic Terrestrial Radar Interferometry (TRI) enables high-frequency glacier observations but provides only one-dimensional velocity. We propose nonlinear-constrained Geographically Weighted Regression to integrate TRI and external constraints for multidimensional velocity retrieval. and it shows excellent consistency when validated. Applied to Helheim Glacier, it reveals semidiurnal and diurnal velocity and strain-rate variations, likely driven by tides and meltwater, and their transition. 1517 </div> 1518 <div><a href="#" class="show-hide triangle" data-hide=".short_summary_145317" 1519 data-show=".short_summary_button_145317">Hide</a></div> 1520 </div> 1521 </div> 1522 </div> 1523 <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> 1524 </div> 1525 </div> 1526 <div class="grid-container paperlist-object in-range paperList-final" 1527 data-diff="0"> 1528 <div class="grid-100 hide-on-desktop hide-on-tablet"> 1529 <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/5533/2026/tc-20-5533-2026-avatar-web.png"> 1530 <img class="img-responsive" src="https://tc.copernicus.org/articles/20/5533/2026/tc-20-5533-2026-avatar-thumb80.png" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-web="https://tc.copernicus.org/articles/20/5533/2026/tc-20-5533-2026-avatar-web.png" data-width="600" data-height="266" width="80" height="80"> 1531 1532 </a> 1533 </div> 1534 <div class="grid-85 tablet-grid-85"> 1535 <div class="published-date"> 29 Sep 2026</div> 1536 <a class="article-title" target="_parent" href="https://tc.copernicus.org/articles/20/5533/2026/">In-situ tracer percolation experiments to quantify the influence of near-surface melting on Svalbard snow signatures</a> 1537 <div class="authors">Dorothea Elisabeth Baur, Andrea Spolaor, Federico Scoto, and Elizabeth R. Thomas</div> 1538 <div class="citation">The Cryosphere, 20, 5533–5558, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/tc-20-5533-2026,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/tc-20-5533-2026,</span> 2026</div> 1539 <span class="show-hide journal-contentLinkColor triangle short_summary_button_137879" 1540 data-show=".short_summary_137879" 1541 data-hide=".short_summary_button_137879" 1542 >Short summary</span> 1543 <div class="j-widget__max short_summary short_summary_137879" style="display: none"> 1544 <div class="widget dark-border"> 1545 <div class="legend journal-contentLinkColor">Short summary</div> 1546 <div class="content"> 1547 The Arctic is warming rapidly, and winter rain-on-snow events are becoming more common. These events can alter snow layers and disturb climate information stored in glaciers. We studied how small rain-on-snow events affect snow structure and water isotopes near Ny-Ålesund, Svalbard. Field experiments show that meltwater flow creates complex features, but isotope changes remain confined to them, meaning seasonal climate signals can still be preserved where enough snow accumulates. 1548 </div> 1549 <div><a href="#" class="show-hide triangle" data-hide=".short_summary_137879" 1550 data-show=".short_summary_button_137879">Hide</a></div> 1551 </div> 1552 </div> 1553 </div>
1554 <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> 1555 <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/5533/2026/tc-20-5533-2026-avatar-web.png"> 1556 <img class="img-responsive" src="https://tc.copernicus.org/articles/20/5533/2026/tc-20-5533-2026-avatar-thumb80.png" data-web="https://tc.copernicus.org/articles/20/5533/2026/tc-20-5533-2026-avatar-web.png" data-width="600" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-height="266" width="80" height="80"> 1557 </a> 1558 </div> 1559 </div> 1560</div> 1561<!--
1561<script id="recent-template" data-journal-url="https://tc.copernicus.org/articles/" data-journal-shot-cut="tc" type="x-tmpl-mustache">--> 1562 <!-- {{%FILTERS}} 1563 <div class="grid-container paperlist-object{{#hasType}} type-{{type}}{{/hasType}}{{^hidden}} in-range{{/hidden}}{{#hidden}} hidden{{/hidden}} paperList-{{htmlSelectorSuffix}}" 1564 data-diff="{{publishedDateDifference}}"> 1565 1566 {{#listSubtitle}} 1567 <div class="grid-100"> 1568 <span class="article-subtitle">{{{.}}}</span> 1569 </div> 1570 {{/listSubtitle}} 1571 <div class="grid-100 hide-on-desktop hide-on-tablet"> 1572 {{#hasAvatar}} 1573 <a class="paperlist-avatar" href="{{avatarWeb|absoluteUrl}}"> 1574 <img class="img-responsive" src="{{avatarThumb|absoluteUrl}}" data-web="{{avatarWeb|absoluteUrl}}" data-width="{{avatarWidth}}" data-height="{{avatarHeight}}"> 1575 </a> 1576 {{/hasAvatar}} 1577 </div> 1578 <div class="grid-85 tablet-grid-85"> 1579 1580 {{#publishedDate}} 1581 <div class="published-date"> {{. | date.d M Y}}</div> 1582 {{/publishedDate}} 1583 {{#manuscriptTypeTitle}} 1584 <div class="manuscriptType" > | {{.}}</div> 1585 {{/manuscriptTypeTitle}} 1586 <a class="article-title" target="_parent" href="{{articleLink |absoluteUrl}}">{{{title}}}</a> 1587 1588 <div class="authors">{{{authorsText}}}</div> 1589 {{#hasFullCitation}} 1590 <div class="citation">{{journalCitation}}, {{volumeNumber}}, {{#citationByArticleNumber}}{{articleNumber}}{{/citationByArticleNumber}}{{^citationByArticleNumber}}{{#pageNumberPrefix}}{{.}} {{/pageNumberPrefix}}{{firstPage}}-{{lastPage}}{{/citationByArticleNumber}}, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/{{doi}},</nobr><span class="hide-on-desktop">https://doi.org/{{doi}},</span> {{year}}{{^statusMessage}}{{#views}} |<nobr> {{.|number_format}} views</nobr>{{/views}}{{/statusMessage}}</div> 1591 {{/hasFullCitation}} 1592 {{^hasFullCitation}} 1593 <div class="citation">{{journalCitation}}, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/{{doi}},</nobr><span class="hide-on-desktop">https://doi.org/{{doi}},</span> {{year}}</div> 1594 {{/hasFullCitation}} 1595 {{#statusMessage}} 1596 <div class="statusMessage"><span>{{.}}</span> <nobr>{{statusExtension}}</nobr>{{#views}} |<nobr> {{.|number_format}} views</nobr>{{/views}}</div> 1597 {{/statusMessage}} 1598 1599 {{#shortSummary}} 1600 <image class="show-hide short-summary-button short_summary_button_{{id}}" data-show=".short_summary_{{id}}" 1601 data-hide=".short_summary_button_{{id}}" 1602 height="14" width="50" src="{{assetsPath}}{{projectShortCut}}_icon_summary.png" 1603 xlink:href="{{assetsPath}}{{projectShortCut}}_icon_summary.svg"/> 1604 <div class="j-widget__max short_summary_{{id}}" style="display: none"> 1605 1606 <fieldset> 1607 <legend>Short summary</legend> 1608 <div class="content"> 1609 {{{.}}} 1610 </div> 1611 <a href="#" class="show-hide triangle" data-hide=".short_summary_{{id}}" 1612 data-show=".short_summary_button_{{id}}">Hide</a> 1613 </fieldset> 1614 </div> 1615 {{/shortSummary}} 1616 </div> 1617 <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> 1618 {{#hasAvatar}} 1619 <a class="paperlist-avatar" href="{{avatarWeb|absoluteUrl}}"> 1620 <img class="img-responsive" src="{{avatarThumb|absoluteUrl}}" data-web="{{avatarWeb|absoluteUrl}}" data-width="{{avatarWidth}}" data-height="{{avatarHeight}}"> 1621 </a> 1622 {{/hasAvatar}} 1623 </div> 1624 1625 </div>--> 1626<!--</script>
1626--> 1627</div><div id="highlight-articles" class="cmsbox landing-page"><div id="highlight-paper-content"> 1628 1629 <div id="highlight-articles-header"> 1630 <h2>Highlight articles</h2> 1631 </div> 1632 <div class="grid-container paperlist-object in-range paperList-final" 1633 data-diff="0"> 1634 <div class="grid-100 hide-on-desktop hide-on-tablet"> 1635 <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/5099/2026/tc-20-5099-2026-avatar-web.png"> 1636 <img class="img-responsive" src="https://tc.copernicus.org/articles/20/5099/2026/tc-20-5099-2026-avatar-thumb80.png" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-web="https://tc.copernicus.org/articles/20/5099/2026/tc-20-5099-2026-avatar-web.png" data-width="600" data-height="354" width="80" height="80"> 1637 1638 </a> 1639 </div> 1640 <div class="grid-85 tablet-grid-85"> 1641 <div class="published-date"> 10 Sep 2026</div> 1642 <a class="article-title" target="_parent" href="https://tc.copernicus.org/articles/20/5099/2026/">Evaluating surface mass balance variability from climate models using GPS Bedrock Vertical Time Series data</a> 1643 <div class="authors">Jenan Rajavarathan, Matt King, Christopher Watson, and Nicolaj Hansen</div> 1644 <div class="citation">The Cryosphere, 20, 5099–5113, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/tc-20-5099-2026,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/tc-20-5099-2026,</span> 2026</div> 1645 <span class="show-hide journal-contentLinkColor triangle short_summary_button_139125" 1646 data-show=".short_summary_139125" 1647 data-hide=".short_summary_button_139125" 1648 >Short summary</span> 1649 <span class="show-hide journal-contentLinkColor triangle ce_comment_button_139125 ml-2" 1650 data-show=".ce_comment_139125" 1651 data-hide=".ce_comment_button_139125">Editorial statement</span> 1652 <div class="j-widget__max short_summary short_summary_139125" style="display: none"> 1653 <div class="widget dark-border"> 1654 <div class="legend journal-contentLinkColor">Short summary</div> 1655 <div class="content"> 1656 Antarctic surface mass balance (SMB) is a source of major uncertainty in ice-sheet mass balance estimates, but its evaluation remains limited. We introduce a novel method using continuous, bedrock-fixed GPS vertical displacements as a spatially integrated constraint on low-frequency SMB variability over hundreds of kilometres. Applied across Antarctica, it reveals systematic, region-dependent differences with modelled SMB-driven displacements, guiding SMB model refinement. 1657 </div> 1658 <div><a href="#" class="show-hide triangle" data-hide=".short_summary_139125" 1659 data-show=".short_summary_button_139125">Hide</a></div> 1660 </div> 1661 </div> 1662 <div class="j-widget__max ce_comment ce_comment_139125 mt-3" style="display: none"> 1663 <div class="widget dark-border"> 1664 <div class="legend journal-contentLinkColor">Editorial statement</div> 1665 <div class="content"> 1666 The surface mass balance (SMB) of polar ice sheets is vital to their overall mass gain or loss. However, evaluating SMB across Antarctica is extremely difficult because observations that can validate climate-model estimates are widely lacking. In this manuscript, the authors present a highly original approach to this problem: they use GPS observations to evaluate SMB models. Analysis of GPS data from sites across Antarctica is used to evaluate the variability in SMB from several atmospheric models. The findings are timely and important, especially as more SMB models are available at increasingly fine spatial resolution. Overall, the study contributes valuable insights into estimates of ice-sheet mass variability and its varying contribution to sea-level change. 1667 </div> 1668 <div><a href="#" class="show-hide triangle" data-hide=".ce_comment_139125" 1669 data-show=".ce_comment_button_139125">Hide</a></div> 1670 </div> 1671 </div> 1672 </div>
1673 <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> 1674 <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/5099/2026/tc-20-5099-2026-avatar-web.png"> 1675 <img class="img-responsive" src="https://tc.copernicus.org/articles/20/5099/2026/tc-20-5099-2026-avatar-thumb80.png" data-web="https://tc.copernicus.org/articles/20/5099/2026/tc-20-5099-2026-avatar-web.png" data-width="600" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-height="354" width="80" height="80"> 1676 </a> 1677 </div> 1678 </div> 1679 <div class="grid-container paperlist-object in-range paperList-final" 1680 data-diff="0"> 1681 <div class="grid-100 hide-on-desktop hide-on-tablet"> 1682 <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/4619/2026/tc-20-4619-2026-avatar-web.png"> 1683 <img class="img-responsive" src="https://tc.copernicus.org/articles/20/4619/2026/tc-20-4619-2026-avatar-thumb80.png" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-web="https://tc.copernicus.org/articles/20/4619/2026/tc-20-4619-2026-avatar-web.png" data-width="600" data-height="278" width="80" height="80"> 1684 1685 </a> 1686 </div> 1687 <div class="grid-85 tablet-grid-85"> 1688 <div class="published-date"> 21 Aug 2026</div> 1689 <a class="article-title" target="_parent" href="https://tc.copernicus.org/articles/20/4619/2026/">Spatial heterogeneity in post-fire permafrost evolution as revealed by satellite radar observations</a> 1690 <div class="authors">Barbara Widhalm, Annett Bartsch, and Benjamin Jones</div> 1691 <div class="citation">The Cryosphere, 20, 4619–4654, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/tc-20-4619-2026,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/tc-20-4619-2026,</span> 2026</div> 1692 <span class="show-hide journal-contentLinkColor triangle short_summary_button_136363" 1693 data-show=".short_summary_136363" 1694 data-hide=".short_summary_button_136363" 1695 >Short summary</span> 1696 <span class="show-hide journal-contentLinkColor triangle ce_comment_button_136363 ml-2" 1697 data-show=".ce_comment_136363" 1698 data-hide=".ce_comment_button_136363">Editorial statement</span> 1699 <div class="j-widget__max short_summary short_summary_136363" style="display: none"> 1700 <div class="widget dark-border"> 1701 <div class="legend journal-contentLinkColor">Short summary</div> 1702 <div class="content"> 1703 This study examines the impacts of wildfires on permafrost thaw in the Arctic spanning up to ~90 years post-fire and explores the potential of using radar satellite observations to enhance our understanding of environmental change. By assessing diverse high-latitude permafrost landscapes, we show that ground deformation anomalies after fires display similar patterns across regions, while radar backscatter varies depen
1703ding on predominant ground temperatures. 1704 </div> 1705 <div><a href="#" class="show-hide triangle" data-hide=".short_summary_136363" 1706 data-show=".short_summary_button_136363">Hide</a></div> 1707 </div> 1708 </div> 1709 <div class="j-widget__max ce_comment ce_comment_136363 mt-3" style="display: none"> 1710 <div class="widget dark-border"> 1711 <div class="legend journal-contentLinkColor">Editorial statement</div> 1712 <div class="content"> 1713 By tracking post-fire tundra recovery up to 90 years using satellite radar across North America, this study reveals that while annual permafrost degradation stabilizes within 7â13 years, seasonal deformation and elevated soil moisture persist for roughly 50 years. This study moves beyond localized, single-site studies to establish a scalable, regional framework across diverse permafrost zones. Ultimately, these findings resolve a major spatial gap in permafrost research by proving that recovery timelines are strongly controlled by regional thermal regimes, providing crucial observational constraints for Earth system models and climate research. 1714 </div> 1715 <div><a href="#" class="show-hide triangle" data-hide=".ce_comment_136363" 1716 data-show=".ce_comment_button_136363">Hide</a></div> 1717 </div> 1718 </div> 1719 </div> 1720 <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> 1721 <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/4619/2026/tc-20-4619-2026-avatar-web.png"> 1722 <img class="img-responsive" src="https://tc.copernicus.org/articles/20/4619/2026/tc-20-4619-2026-avatar-thumb80.png" data-web="https://tc.copernicus.org/articles/20/4619/2026/tc-20-4619-2026-avatar-web.png" data-width="600" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-height="278" width="80" height="80"> 1723 </a> 1724 </div> 1725 </div> 1726 <div class="grid-container paperlist-object in-range paperList-final" 1727 data-diff="0"> 1728 <div class="grid-100 hide-on-desktop hide-on-tablet"> 1729 <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/4005/2026/tc-20-4005-2026-avatar-web.png"> 1730 <img class="img-responsive" src="https://tc.copernicus.org/articles/20/4005/2026/tc-20-4005-2026-avatar-thumb80.png" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-web="https://tc.copernicus.org/articles/20/4005/2026/tc-20-4005-2026-avatar-web.png" data-width="422" data-height="600" width="80" height="80"> 1731 1732 </a> 1733 </div> 1734 <div class="grid-85 tablet-grid-85"> 1735 <div class="published-date"> 21 Jul 2026</div> 1736 <a class="article-title" target="_parent" href="https://tc.copernicus.org/articles/20/4005/2026/">Brief communication: Temperature-driven shrinkage of a disappearing Himalayan glacier</a> 1737 <div class="authors">Koji Fujita and Rijan B. Kayastha</div> 1738 <div class="citation">The Cryosphere, 20, 4005–4015, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/tc-20-4005-2026,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/tc-20-4005-2026,</span> 2026</div> 1739 <span class="show-hide journal-contentLinkColor triangle short_summary_button_139009" 1740 data-show=".short_summary_139009" 1741 data-hide=".short_summary_button_139009" 1742 >Short summary</span>
1743 <span class="show-hide journal-contentLinkColor triangle ce_comment_button_139009 ml-2" 1744 data-show=".ce_comment_139009" 1745 data-hide=".ce_comment_button_139009">Editorial statement</span> 1746 <div class="j-widget__max short_summary short_summary_139009" style="display: none"> 1747 <div class="widget dark-border"> 1748 <div class="legend journal-contentLinkColor">Short summary</div> 1749 <div class="content"> 1750 Glacier AX010 in Nepal, monitored since the 1970s, has been shrinking at an accelerating rate, mainly due to rising temperatures. Drone surveys, modeling, and reanalysis data show mass loss began in the early 1970s and intensified after 2000. While rising temperatures drive shrinkage, precipitation changes have neither accelerated nor mitigated mass loss. At the current rate, the glacier may disappear within 10–20 years. 1751 </div> 1752 <div><a href="#" class="show-hide triangle" data-hide=".short_summary_139009" 1753 data-show=".short_summary_button_139009">Hide</a></div> 1754 </div> 1755 </div> 1756 <div class="j-widget__max ce_comment ce_comment_139009 mt-3" style="display: none"> 1757 <div class="widget dark-border"> 1758 <div class="legend journal-contentLinkColor">Editorial statement</div> 1759 <div class="content"> 1760 This paper describes the rapid, recent decline of Glacier AX010, the glacier with the oldest observational mass balance record in the Nepal Himalayas. It also discusses the likely disappearance of the glacier within the next two decades, highlighting the ongoing importance of monitoring small glaciers in high mountain regions given their vulnerability to climate warming. 1761 </div> 1762 <div><a href="#" class="show-hide triangle" data-hide=".ce_comment_139009" 1763 data-show=".ce_comment_button_139009">Hide</a></div> 1764 </div> 1765 </div> 1766 </div> 1767 <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> 1768 <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/4005/2026/tc-20-4005-2026-avatar-web.png"> 1769 <img class="img-responsive" src="https://tc.copernicus.org/articles/20/4005/2026/tc-20-4005-2026-avatar-thumb80.png" data-web="https://tc.copernicus.org/articles/20/4005/2026/tc-20-4005-2026-avatar-web.png" data-width="422" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-height="600" width="80" height="80"> 1770 </a> 1771 </div> 1772 </div> 1773 <div class="grid-container paperlist-object in-range paperList-final" 1774 data-diff="0"> 1775 <div class="grid-100 hide-on-desktop hide-on-tablet"> 1776 <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/3827/2026/tc-20-3827-2026-avatar-web.png"> 1777 <img class="img-responsive" src="https://tc.copernicus.org/articles/20/3827/2026/tc-20-3827-2026-avatar-thumb80.png" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-web="https://tc.copernicus.org/articles/20/3827/2026/tc-20-3827-2026-avatar-web.png" data-width="600" data-height="249" width="80" height="80"> 1778 1779 </a> 1780 </div> 1781 <div class="grid-85 tablet-grid-85"> 1782 <div class="published-date"> 13 Jul 2026</div> 1783 <a class="article-title" target="_parent" href="https://tc.copernicus.org/articles/20/3827/2026/">Contrasting dynamics of lake- and marine-terminating glaciers under same climatic conditions</a> 1784 <div class="authors">Florian Vacek, Faezeh M. Nick, Douglas Benn, Maarten P. A. Zwarts, Walter Immerzeel, and Roderik S. W. van de Wal</div> 1785 <div class="citation">The Cryosphere, 20, 3827–3845, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/tc-20-3827-2026,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/tc-20-3827-2026,</span> 2026</div>
1786 <span class="show-hide journal-contentLinkColor triangle short_summary_button_135500" 1787 data-show=".short_summary_135500" 1788 data-hide=".short_summary_button_135500" 1789 >Short summary</span> 1790 <span class="show-hide journal-contentLinkColor triangle ce_comment_button_135500 ml-2" 1791 data-show=".ce_comment_135500" 1792 data-hide=".ce_comment_button_135500">Editorial statement</span> 1793 <div class="j-widget__max short_summary short_summary_135500" style="display: none"> 1794 <div class="widget dark-border"> 1795 <div class="legend journal-contentLinkColor">Short summary</div> 1796 <div class="content"> 1797 We studied a unique glacier in South Greenland that ends in both a lake and the ocean. Using satellite data and field work, we found that the two glacier fronts behave very differently even under the same climate. At the lake glacier we identify a floating ice tongue and we infer little melt below water. The lake glacier experienced a sudden large breakup. Our work suggests that lake and marine glacier fronts must be treated differently in model simulations. 1798 </div> 1799 <div><a href="#" class="show-hide triangle" data-hide=".short_summary_135500" 1800 data-show=".short_summary_button_135500">Hide</a></div> 1801 </div> 1802 </div> 1803 <div class="j-widget__max ce_comment ce_comment_135500 mt-3" style="display: none"> 1804 <div class="widget dark-border"> 1805 <div class="legend journal-contentLinkColor">Editorial statement</div> 1806 <div class="content"> 1807 This study offers a rare natural experiment by comparing two adjacent glaciers South Greenland with shared upstream conditions but differing terminus environments: one terminating in a lake and the other in the ocean. The clear contrast in their dynamic behaviours, despite similar climate and input conditions, provides valuable insight into the role of terminus type in regulating glacier response. This has broader implications for predicting glacier change and sea-level contributions in a warming climate. 1808 </div> 1809 <div><a href="#" class="show-hide triangle" data-hide=".ce_comment_135500" 1810 data-show=".ce_comment_button_135500">Hide</a></div> 1811 </div> 1812 </div> 1813 </div> 1814 <div class="grid-15 tablet-grid-15 text-right hide-on-mobile"> 1815 <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/3827/2026/tc-20-3827-2026-avatar-web.png"> 1816 <img class="img-responsive" src="https://tc.copernicus.org/articles/20/3827/2026/tc-20-3827-2026-avatar-thumb80.png" data-web="https://tc.copernicus.org/articles/20/3827/2026/tc-20-3827-2026-avatar-web.png" data-width="600" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-height="249" width="80" height="80"> 1817 </a> 1818 </div> 1819 </div> 1820 <div class="grid-container paperlist-object in-range paperList-final" 1821 data-diff="0"> 1822 <div class="grid-100 hide-on-desktop hide-on-tablet"> 1823 <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/3705/2026/tc-20-3705-2026-avatar-web.png"> 1824 <img class="img-responsive" src="https://tc.copernicus.org/articles/20/3705/2026/tc-20-3705-2026-avatar-thumb80.png" data-caption="© Author(s). Distributed under the Creative
1824Commons Attribution 4.0 License." data-web="https://tc.copernicus.org/articles/20/3705/2026/tc-20-3705-2026-avatar-web.png" data-width="600" data-height="377" width="80" height="80"> 1825 1826 </a> 1827 </div> 1828 <div class="grid-85 tablet-grid-85"> 1829 <div class="published-date"> 01 Jul 2026</div> 1830 <a class="article-title" target="_parent" href="https://tc.copernicus.org/articles/20/3705/2026/">Review article: The Foundation-Patuxent-Academy ice stream system, Antarctica</a> 1831 <div class="authors">Neil Ross, Rebecca J. Sanderson, Bernd Kulessa, Martin Siegert, Guy J. G. Paxman, Keir A. Nichols, Matthew R. Siegfried, Stewart S. R. Jamieson, Michael J. Bentley, Tom A. Jordan, Christine L. Batchelor, David Small, Olaf Eisen, Kate Winter, Robert G. Bingham, S. Louise Callard, Rachel Carr, Christine F. Dow, Helen A. Fricker, Emily Hill, Benjamin H. Hills, Coen Hofstede, Hafeez Jeofry, Felipe Napoleoni, and Wilson Sauthoff</div> 1832 <div class="citation">The Cryosphere, 20, 3705–3737, <nobr class="hide-on-mobile hide-on-tablet">https://doi.org/10.5194/tc-20-3705-2026,</nobr><span class="hide-on-desktop">https://doi.org/10.5194/tc-20-3705-2026,</span> 2026</div> 1833 <span class="show-hide journal-contentLinkColor triangle short_summary_button_131777" 1834 data-show=".short_summary_131777" 1835 data-hide=".short_summary_button_131777" 1836 >Short summary</span> 1837 <span class="show-hide journal-contentLinkColor triangle ce_comment_button_131777 ml-2" 1838 data-show=".ce_comment_131777" 1839 data-hide=".ce_comment_button_131777">Editorial statement</span> 1840 <div class="j-widget__max short_summary short_summary_131777" style="display: none"> 1841 <div class="widget dark-border"> 1842 <div class="legend journal-contentLinkColor">Short summary</div> 1843 <div class="content"> 1844 We review research about a group of fast-flowing Antarctic ice streams, the Foundation-Patuxent-Academy System. Previously, we knew little about how these ice streams flow, how they interact with each other and the ocean, what their geological history was, and how they might evolve in a warming world. By reviewing existing research, we have identified the future research needed to determine how these ice streams function, and how they might contribute to future global sea level rise. 1845 </div> 1846 <div><a href="#" class="show-hide triangle" data-hide=".short_summary_131777" 1847 data-show=".short_summary_button_131777">Hide</a></div> 1848 </div> 1849 </div> 1850 <div class="j-widget__max ce_comment ce_comment_131777 mt-3" style="display: none"> 1851 <div class="widget dark-border"> 1852 <div class="legend journal-contentLinkColor">Editorial statement</div> 1853 <div class="content"> 1854 This manuscript provides an overview of a major Antarctic ice stream system, the Foundation-Patuxent-Academy, summarising its glaciological and hydrological properties and while offering a comprehensive overview of the extensive existing literature in the region. The review also outlines critical gaps in knowledge providing an ideal starting point for considerations of future work during the International Polar Year in 2032-33. 1855 1856 </div> 1857 <div><a href="#" class="show-hide triangle" data-hide=".ce_comment_131777" 1858 data-show=".ce_comment_button_131777">Hide</a></div> 1859 </div> 1860 </div> 1861 </div>
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