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343                                                                <a   target="_parent" class="" href="https://www.the-cryosphere.net/about/news_and_press/2021-01-13_spectral-characterization-radiative-forcing-and-pigment-content-of-coastal-antarctic-snow-algae.html">Spectral characterization, radiative forcing and pigment content of coastal Antarctic snow algae: approaches to spectrally discriminate red and green communities and their impact on snowmelt</
343a>
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346                                                                <a   target="_parent" class="" href="https://www.the-cryosphere.net/about/news_and_press/2021-01-25_review-article-earths-ice-imbalance.html">Review article: Earth's ice imbalance</a>
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350                                                        </div>
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352                                                                <a   target="_parent" class="" href="https://www.the-cryosphere.net/about/news_and_press/2021-04-01_winter-drainage-of-surface-lakes-on-the-greenland-ice-sheet-from-sentinel-1-sar-imagery.html">Winter drainage of surface lakes on the Greenland Ice Sheet from Sentinel-1 SAR imagery</a>
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355                                                                <a   target="_parent" class="" href="https://www.the-cryosphere.net/about/news_and_press/2021-05-27_creep-and-fracture-of-warm-columnar-freshwater-ice.html">Creep and fracture of warm columnar freshwater ice</a>
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358                                                                <a   target="_parent" class="" href="https://www.the-cryosphere.net/about/news_and_press/2021-06-15_interannual-variability-in-transpolar-drift-summer-sea-ice-thickness-and-potential-impact-of-atlantification.html">Interannual variability in Transpolar Drift summer sea ice thickness and potential impact of Atlantification</a>
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362                                                        </div>
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394                                    </div>
395                                </div>
396                                </div>
397                            </div>
398                        </div>
399                </li>
400                    <li class="nav-item  ">
401                        <a target="_parent" class="nav-link  "  href="https://www.the-cryosphere.net/egu_publications.html">EGU publications</a>
402                </li>
403                    <li class="nav-item  ">
404                        <a target="_parent" class="nav-link  " data-non-mobile-optimized="1" href="https://editor.copernicus.org/TC/"><i class='fal fa-sign-in-alt fa-lg' title='Login'></i></a>
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409				frameborder="0"
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412				src=""></iframe> -->
413                </li>
414                <!-- End Topbar -->
415            </ul>
416</div>
417</div></div>
418
419            </nav>
420
421        </div>
422
423        <section id="banner" class="banner dzsparallaxer use-loading auto-init height-is-based-on-content mode-scroll loaded dzsprx-readyall">
424
425            <div class="divimage dzsparallaxer--target layout__moodboard-banner" data-src="" style=""></div>
426
427            <!-- END_SNIPPET:part7 -->
428
429            <div id="headers-content-container" class="container CMSCONTAINER">
430
431
432
433            <div id="cmsbox_124926" class="cmsbox ">            <span class="header-small text-uppercase"><!-- START_HEADLINE_ORDER_FIRST --><!-- END_HEADLINE_ORDER_FIRST -->&nbsp;</span>
434            <h1 class="display-4 header-get-function home-header hide-md-on-version2023">
435                <!-- START_HEADLINE_ORDER_SECOND -->The Cryosphere<!-- END_HEADLINE_ORDER_SECOND -->&nbsp;
436            </h1>
437</div></div>
438
439        </section>
440
441
442
443        <div id="breadcrumbs" class="breadcrumbs">
444
445            <div class="container">
446
447                <div class="row align-items-center">
448
449                    <div class="d-none d-sm-block text-nowrap pageactions"></div>
450
451                    <!-- START_SEARCH -->
452
453                    <!-- END_SEARCH -->
454
455                    <!-- The template part snippet fo breadcrubs is in source code-->
456
457                    <div class="justify-content-between col-auto col-md CMSCONTAINER" id="breadcrumbs_content_container"><div id="cmsbox_1093391" class="cmsbox "><!-- tpl: templates/get_functions/get_breadcrumbs/index -->
458<div class="breadcrumbGetFunctionContainer">
459    <!-- START_BREADCRUMBS_CONTAINER -->
460    <ol class="breadcrumb">
461        <!-- START_BREADCRUMBS -->
462        <!-- START_SNIPPET:part8 -->
463                <li class="breadcrumb-item active">Home</li>
464        <!-- END_SNIPPET:part8 -->
465        <!-- END_BREADCRUMBS -->
466    </ol>
467    <!-- END_BREADCRUMBS_CONTAINER -->
468</div></div></div>
469
470                    <!-- START_SNIPPET:part10 -->
471
472                    <div class="col col-md-4 text-right page-search CMSCONTAINER" id="search_content_container"><div id="cmsbox_1093297" class="cmsbox "><!-- v1.31 -->
473<!-- 1.31: added placeholder for test system sanitizing-->
474<!-- 1.3: #855 -->
475<!-- 1.2: #166 -->
476<!-- CMS ressources/FinderBreadcrumbBox.html -->
477<!-- START_SITE_SEARCH -->
478<!-- Root element of PhotoSwipe. Must have class pswp. -->
479<div class="pswp" tabindex="-1" role="dialog" aria-hidden="true" >
480
481    <!-- Background of PhotoSwipe.
482         It's a separate element as animating opacity is faster than rgba(). -->
483    <div class="pswp__bg"></div>
484
485    <!-- Slides wrapper with overflow:hidden. -->
486    <div class="pswp__scroll-wrap">
487
488        <!-- Container that holds slides.
489            PhotoSwipe keeps only 3 of them in the DOM to save memory.
490            Don't modify these 3 pswp__item elements, data is added later on. -->
491        <div class="pswp__container">
492            <div class="pswp__item"></div>
493            <div class="pswp__item"></div>
494            <div class="pswp__item"></div>
495        </div>
496
497        <!-- Default (PhotoSwipeUI_Default) interface on top of sliding area. Can be changed. -->
498        <div class="pswp__ui pswp__ui--hidden">
499
500            <div class="pswp__top-bar">
501
502                <!--  Controls are self-explanatory. Order can be changed. -->
503
504                <div class="pswp__counter"></div>
505
506                <button class="pswp__button pswp__button--close" title="Close (Esc)"></button>
507
508
509                <button class="pswp__button pswp__button--fs" title="Toggle fullscreen"></button>
510
511                <!-- Preloader demo http://codepen.io/dimsemenov/pen/yyBWoR -->
512                <!-- element will get class pswp__preloader--active when preloader is running -->
513                <div class="pswp__preloader">
514                    <div class="pswp__preloader__icn">
515                        <div class="pswp__preloader__cut">
516                            <div class="pswp__preloader__donut"></div>
517                        </div>
518                    </div>
519                </div>
520            </div>
521
522            <div class="pswp__share-modal pswp__share-modal--hidden pswp__single-tap">
523                <div class="pswp__share-tooltip"></div>
524            </div>
525
526            <button class="pswp__button pswp__button--arrow--left" title="Previous (arrow left)">
527            </button>
528
529            <button class="pswp__button pswp__button--arrow--right" title="Next (arrow right)">
530            </button>
531
532            <div class="pswp__caption ">
533                <div class="pswp__caption__center"></div>
534            </div>
535
536        </div>
537
538    </div>
539
540</div>
541<div class="row align-items-center no-gutters py-1" id="search-wrapper">
542
543    <div class="col-auto pl-0 pr-1">
544        <a id="templateSearchInfoBtn" role="button" tabindex="99" data-container="body" data-toggle="popover" data-placement="bottom" data-trigger="click"><span class="fal fa-info-circle"></span></a>
545    </div>
546
547    <div class="col pl-0 pr-1">
548        <input type="search" placeholder="Search" name="q" class="form-control form-control-sm" id="search_query_solr"/>
549    </div>
550    <div class="col-auto pl-0">
551        <button title="Start site search" id="start_site_search_solr" class="btn btn-sm btn-success"><span class="co-search"></span></button>
552    </div>
553</div>
554
555<div class="text-left">
556    <div id="templateSearchInfo" class="d-none">
557        <div>
558            <p>
559                Multiple terms: term1 term2<br />
560                <i>red apples</i><br />
561                returns results with all terms like:<br />
562                <i>Fructose levels in <strong>red</strong> and <strong>green</strong> apples</i><br />
563            </p>
564            <p>
565                Precise match in quotes: "term1 term2"<br />
566                <i>"red apples"</i><br />
567                returns results matching exactly like:<br />
568                <i>Anthocyanin biosynthesis in <strong>red apples</strong></i><br />
569            </p>
570
571            <p>
572                Exclude a term with -: term1 -term2<br />
573                <i>apples -red</i><br />
574                returns results containing <i><strong>apples</strong></i> but not <i><strong>red</strong></i>:<br />
575                <i>Malic acid in green <strong>apples</strong></i><br />
576            </p>
577        </div>
578    </div>
579
580    <div class="modal " id="templateSearchResultModal" role="dialog" aria-labelledby="Search results" aria-hidden="true">
581        <div class="modal-dialog modal-lg modal-dialog-centered">
582            <div class="modal-content">
583                <div class="modal-header modal-header--sticky shadow one-column d-block">
584                    <div class="row no-gutters mx-1">
585                        <div class="col mr-3">
586                                <h1 class="" id="resultsSearchHeader"><span id="templateSearchResultNr"></span> hit<span id="templateSearchResultNrPlural">s</span> for <span id="templateSearchResultTerm"></span></h1>
587                            </div>
588                        <div class="col-auto">
589                            <a id="scrolltopmodal" href="javascript:void(0)" onclick="scrollModalTop();" style="display: none;"><i class="co-home"></i></a>
590
591                        </div>
592                        <div class="col-auto">
593                                <button data-dismiss="modal" aria-label="Close" class="btn btn-danger mt-1">Close</button>
594                            </div>
595                    </div>
596                </div>
597                <div class="modal-body one-column">
598                    <!-- $$co-sanitizing-slot1$$ -->
599                    <div class="grid-container mx-n3">
599<div class="grid-85 tablet-grid-85">
600                        <button aria-label="Refine" id="refineSearchModal" class="btn btn-primary float-left mt-4">Refine your search</button>
601                        <button aria-label="Refine" id="refineSearchModalHide" class="btn btn-danger float-left d-none mt-4">Hide refinement</button>
602                    </div></div>
603                    <div class="grid-container mx-n3"><div class="grid-100 tablet-grid-100"><div id="templateRefineSearch" class="d-none"></div></div></div>
604
605                <div id="templateSearchResultContainer" class="searchResultsModal mx-n3"></div>
606                <div class="grid-container mb-0"><div class="grid-100 tablet-grid-100"><div id="templateSearchResultContainerEmpty" class="co-notification d-none">There are no results for your search term.</div></div></div>
607            </div>
608
609            </div>
610        </div>
611    </div>
612</div>
613
614    <!-- feedback network problems -->
615    <div class="modal " id="templateSearchErrorModal1"  role="dialog" aria-labelledby="Search results" aria-hidden="true">
616        <div class="modal-dialog modal-lg modal-dialog-centered">
617            <div class="modal-content p-3">
618                <div class="modal-body text-left">
619                    <h1 class="mt-0 pt-0">Network problems</h1>
620                    <div class="co-error">We are sorry, but your search could not be completed due to network problems. Please try again later.</div>
621                </div>
622            </div>
623        </div>
624    </div>
625
626    <!-- feedback server timeout -->
627    <div class="modal " id="templateSearchErrorModal2" role="dialog" aria-labelledby="Search results" aria-hidden="true">
628        <div class="modal-dialog modal-lg modal-dialog-centered">
629            <div class="modal-content p-3">
630                <div class="modal-body text-left">
631                    <h1 class="mt-0 pt-0">Server timeout</h1>
632                    <div class="co-error">We are sorry, but your search could not be completed due to server timeouts. Please try again later.</div>
633                </div>
634            </div>
635        </div>
636    </div>
637
638    <!-- feedback invalid search term -->
639    <div class="modal " id="templateSearchErrorModal3"  role="dialog" aria-labelledby="Search results" aria-hidden="true">
640        <div class="modal-dialog modal-lg modal-dialog-centered">
641            <div class="modal-content p-3">
642                <div class="modal-body text-left">
643                    <h1 class="mt-0 pt-0">Empty search term</h1>
644                    <div class="co-error">You have applied the search with an empty search term. Please revisit and try again.</div>
645                </div>
646            </div>
647        </div>
648    </div>
649
650    <!-- feedback too many requests -->
651    <div class="modal " id="templateSearchErrorModal4"  role="dialog" aria-labelledby="Search results" aria-hidden="true">
652        <div class="modal-dialog modal-lg modal-dialog-centered">
653            <div class="modal-content p-3">
654                <div class="modal-body text-left">
655                    <h1 class="mt-0 pt-0">Too many requests</h1>
656                    <div class="co-error">We are sorry, but we have received too many parallel search requests. Please try again later.</div>
657                </div>
658            </div>
659        </div>
660    </div>
661
662    <!-- loading -->
663    <div class="modal " id="templateSearchLoadingModal"  role="dialog" aria-labelledby="Search results" aria-hidden="true">
664        <div class="modal-dialog modal-sm modal-dialog-centered">
665            <div class="modal-content p-3 co_LoadingDotsContainer">
666                <div class="modal-body">
667                    <div class="text">Searching</div>
668                    <div class="dots d-flex justify-content-center"><div class="dot"></div><div class="dot"></div><div class="dot"></div></div></div>
669            </div>
670        </div>
671    </div>
672
673</div>
674<style>
675    /*.modal {*/
676    /*    background: rgba(255, 255, 255, 0.8);*/
677    /*}*/
678    .modal-header--sticky {
679        position: sticky;
680        top: 0;
681        background-color: inherit;
682        z-index: 1055;
683    }
684    .grid-container
685    {
686        margin-bottom: 1em;
687        /*padding-left: 0;*/
688        /*padding-right: 0;*/
689    }
690    #templateSearchInfo{
691        display: none;
692        background-color: var(--background-color-primary);
693        margin-top: 1px;
694        z-index: 5;
695        border: 1px solid var(--color-primary);
696        opacity: .8;
697        font-size: .7rem;
698        border-radius: .25rem;
699    }
700
701
702    #templateSearchLoadingModal .co_LoadingDotsContainer
703    {
704        z-index: 1000;
705    }
706    #templateSearchLoadingModal .co_LoadingDotsContainer .text
707    {
708        text-align: center;
709        font-weight: bold;
710        padding-bottom: 1rem;
711    }
712    #templateSearchLoadingModal .co_LoadingDotsContainer .dot
713    {
714        background-color: #0072BC;
715        border: 2px solid white;
716        border-radius: 50%;
717        float: left;
718        height: 2rem;
719        width: 2rem;
720        margin: 0 5px;
721        -webkit-transform: scale(0);
722        transform: scale(0);
723        -webkit-animation: animation_dots_breath 1000ms ease infinite 0ms;
724        animation: animation_dots_breath 1000ms ease infinite 0ms;
725    }
726    #templateSearchLoadingModal .co_LoadingDotsContainer .dot:nth-child(2)
727    {
728        -webkit-animation: animation_dots_breath 1000ms ease infinite 300ms;
729        animation: animation_dots_breath 1000ms ease infinite 300ms;
730    }
731    #templateSearchLoadingModal .co_LoadingDotsContainer .dot:nth-child(3)
732    {
733        -webkit-animation: animation_dots_breath 1000ms ease infinite 600ms;
734        animation: animation_dots_breath 1000ms ease infinite 600ms;
735    }
736    #templateSearchResultModal [class*="grid-"] {
737        padding-left: 10px !important;
738        padding-right: 10px !important;
739    }
740    #templateSearchResultTerm {
741        font-weight: bold;
742    }
743
744    #resultsSearchHeader {
745        display: block !important;
746    }
747    #scrolltopmodal {
748        font-size: 3.0em;
749        margin-top: 0 !important;
750        margin-right: 15px;
751    }
752
753    @-webkit-keyframes animation_dots_breath {
754        50% {
755            -webkit-transform: scale(1);
756            transform: scale(1);
757            opacity: 1;
758        }
759        100% {
760            opacity: 0;
761        }
762    }
763    @keyframes animation_dots_breath {
764        50% {
765            -webkit-transform: scale(1);
766            transform: scale(1);
767            opacity: 1;
768        }
769        100% {
770            opacity: 0;
771        }
772    }
773
774    @media (min-width: 768px) and (max-width: 991px) {
775        #templateSearchResultModal .modal-dialog {
776            max-width: 90%;
777        }
778    }
779
780</style>
781<script>
782
783    if(document.querySelector('meta[name="global_moBaseURL"]').content == "https://meetingorganizer.copernicus.org/")
784        FINDER_URL = document.querySelector('meta[name="global_moBaseURL"]').content.replace('meetingorganizer', 'finder-app')+"search/library.php";
785    else
786        FINDER_URL = document.querySelector('meta[name="global_moBaseURL"]').content.replace('meetingorganizer', 'finder')+"search/library.php";
787
788    SEARCH_INPUT = document.getElementById('search_query_solr');
789    SEARCH_INPUT_MODAL = document.getElementById('search_query_modal');
790    searchRunning = false;
791
792    offset = 20;
793    INITIAL_OFFSET = 20;
794
795    var MutationObserver = window.MutationObserver || window.WebKitMutationObserver || window.MozMutationObserver;
796    const targetNodeSearchModal = document.getElementById("templateSearchResultModal");
797    const configSearchModal = { attributes: true, childList: true, subtree: true };
798
799    // Callback function to execute when mutations are observed
800    const callbackSearchModal = (mutationList, observer) => {
801        for (const mutation of mutationList) {
802            if (mutation.type === "childList") {
803                // console.log("A child node has been added or removed.");
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">×</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 – 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 – 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&ndash;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&ndash;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 Chill&aacute;n volcanic complex in south-central Chile remains uncertain. Using satellite and drone images, we find all 28 glaciers on Nevados de Chill&aacute;n lost volume over the past 7 decades, with melt rates accelerating markedly since 2000.&nbsp;
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&ndash;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-&Aring;lesund, 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>
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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>
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1613                    </fieldset>
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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&ndash;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&ndash;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&nbsp;spanning up to ~90 years post-fire&nbsp;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 7–13 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&ndash;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&ndash;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&ndash;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"
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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&ndash;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"
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1859                            </div>
1860                        </div>
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1862                <div class="grid-15 tablet-grid-15 text-right hide-on-mobile">
1863                            <a class="paperlist-avatar" target="_blank" href="https://tc.copernicus.org/articles/20/3705/2026/tc-20-3705-2026-avatar-web.png">
1864                                <img class="img-responsive" src="https://tc.copernicus.org/articles/20/3705/2026/tc-20-3705-2026-avatar-thumb80.png" data-web="https://tc.copernicus.org/articles/20/3705/2026/tc-20-3705-2026-avatar-web.png" data-width="600" data-caption="© Author(s). Distributed under the Creative Commons Attribution 4.0 License." data-height="377" width="80" height="80">
1865                            </a>
1866                </div>
1867            </div>
1868            <p class="j-news-archive-link grid-container grid-parent">
1869                <strong>
1870                            <a class="grid-30 tablet-grid-30 mobile-grid-100" href="https://www.the-cryosphere.net/articles_and_preprints/highlight_articles.html">More highlight articles <img cofileid="17978" alt="" src="https://www.the-cryosphere.net/graphic_grey_right_symbol.png"></a>
1871                        <a  class="grid-30 tablet-grid-30 mobile-grid-100 a-margin__left-2" target="_blank" href="https://www.egu.eu/news/highlight-articles/">All EGU highlight articles <img cofileid="17978" alt="" src="https://www.the-cryosphere.net/graphic_grey_right_symbol.png"></a>
1872                </strong>
1873            </p>
1874</div>
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