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454 <!-- Background of PhotoSwipe. 455 It's a separate element as animating opacity is faster than rgba(). --> 456 <div class="pswp__bg"></div> 457 458 <!-- Slides wrapper with overflow:hidden. --> 459 <div class="pswp__scroll-wrap"> 460 461 <!-- Container that holds slides. 462 PhotoSwipe keeps only 3 of them in the DOM to save memory. 463 Don't modify these 3 pswp__item elements, data is added later on. --> 464 <div class="pswp__container"> 465 <div class="pswp__item"></div> 466 <div class="pswp__item"></div> 467 <div class="pswp__item"></div> 468 </div> 469 470 <!-- Default (PhotoSwipeUI_Default) interface on top of sliding area. Can be changed. --> 471 <div class="pswp__ui pswp__ui--hidden"> 472 473 <div class="pswp__top-bar"> 474 475 <!-- Controls are self-explanatory. Order can be changed. --> 476 477 <div class="pswp__counter"></div> 478 479 <button class="pswp__button pswp__button--close" title="Close (Esc)"></button> 480 481 482 <button class="pswp__button pswp__button--fs" title="Toggle fullscreen"></button> 483 484 <!-- Preloader demo http://codepen.io/dimsemenov/pen/yyBWoR --> 485 <!-- element will get class pswp__preloader--active when preloader is running --> 486 <div class="pswp__preloader"> 487 <div class="pswp__preloader__icn"> 488 <div class="pswp__preloader__cut"> 489 <div class="pswp__preloader__donut"></div> 490 </div> 491 </div> 492 </div> 493 </div> 494 495 <div class="pswp__share-modal pswp__share-modal--hidden pswp__single-tap"> 496 <div class="pswp__share-tooltip"></div> 497 </div> 498 499 <button class="pswp__button pswp__button--arrow--left" title="Previous (arrow left)"> 500 </button> 501 502 <button class="pswp__button pswp__button--arrow--right" title="Next (arrow right)"> 503 </button> 504 505 <div class="pswp__caption "> 506 <div class="pswp__caption__center"></div> 507 </div> 508 509 </div> 510 511 </div> 512 513</div> 514<div class="row align-items-center no-gutters py-1" id="search-wrapper"> 515 516 <div class="col-auto pl-0 pr-1"> 517 <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> 518 </div> 519 520 <div class="col pl-0 pr-1"> 521 <input type="search" placeholder="Search" name="q" class="form-control form-control-sm" id="search_query_solr"/> 522 </div> 523 <div class="col-auto pl-0"> 524 <button title="Start site search" id="start_site_search_solr" class="btn btn-sm btn-success"><span class="co-search"></span></button> 525 </div> 526</div> 527 528<div class="text-left"> 529 <div id="templateSearchInfo" class="d-none"> 530 <div> 531 <p> 532 Multiple terms: term1 term2<br /> 533 <i>red apples</i><br /> 534 returns results with all terms like:<br /> 535 <i>Fructose levels in <strong>red</strong> and <strong>green</strong> apples</i><br /> 536 </p> 537 <p> 538 Precise match in quotes: "term1 term2"<br /> 539 <i>"red apples"</i><br /> 540 returns results matching exactly like:<br /> 541 <i>Anthocyanin biosynthesis in <strong>red apples</strong></i><br /> 542 </p> 543 544 <p> 545 Exclude a term with -: term1 -term2<br /> 546 <i>apples -red</i><br /> 547 returns results containing <i><strong>apples</strong></i> but not <i><strong>red</strong></i>:<br /> 548 <i>Malic acid in green <strong>apples</strong></i><br /> 549 </p> 550 </div> 551 </div> 552 553 <div class="modal " id="templateSearchResultModal" role="dialog" aria-labelledby="Search results" aria-hidden="true"> 554 <div class="modal-dialog modal-lg modal-dialog-centered"> 555 <div class="modal-content"> 556 <div class="modal-header modal-header--sticky shadow one-column d-block"> 557 <div class="row no-gutters mx-1"> 558 <div class="col mr-3"> 559 <h1 class="" id="resultsSearchHeader"><span id="templateSearchResultNr"></span> hit<span id="templateSearchResultNrPlural">s</span> for <span id="templateSearchResultTerm"></span></h1> 560 </div> 561 <div class="col-auto"> 562 <a id="scrolltopmodal" href="javascript:void(0)" onclick="scrollModalTop();" style="display: none;"><i class="co-home"></i></a> 563 564 </div> 565 <div class="col-auto"> 566 <button data-dismiss="modal" aria-label="Close" class="btn btn-danger mt-1">Close</button> 567 </div> 568 </div> 569 </div> 570 <div class="modal-body one-column"> 571 <!-- $$co-sanitizing-slot1$$ --> 572 <div class="grid-container mx-n3">
572<div class="grid-85 tablet-grid-85"> 573 <button aria-label="Refine" id="refineSearchModal" class="btn btn-primary float-left mt-4">Refine your search</button> 574 <button aria-label="Refine" id="refineSearchModalHide" class="btn btn-danger float-left d-none mt-4">Hide refinement</button> 575 </div></div> 576 <div class="grid-container mx-n3"><div class="grid-100 tablet-grid-100"><div id="templateRefineSearch" class="d-none"></div></div></div> 577 578 <div id="templateSearchResultContainer" class="searchResultsModal mx-n3"></div> 579 <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> 580 </div> 581 582 </div> 583 </div> 584 </div> 585</div> 586 587 <!-- feedback network problems --> 588 <div class="modal " id="templateSearchErrorModal1" role="dialog" aria-labelledby="Search results" aria-hidden="true"> 589 <div class="modal-dialog modal-lg modal-dialog-centered"> 590 <div class="modal-content p-3"> 591 <div class="modal-body text-left"> 592 <h1 class="mt-0 pt-0">Network problems</h1> 593 <div class="co-error">We are sorry, but your search could not be completed due to network problems. Please try again later.</div> 594 </div> 595 </div> 596 </div> 597 </div> 598 599 <!-- feedback server timeout --> 600 <div class="modal " id="templateSearchErrorModal2" role="dialog" aria-labelledby="Search results" aria-hidden="true"> 601 <div class="modal-dialog modal-lg modal-dialog-centered"> 602 <div class="modal-content p-3"> 603 <div class="modal-body text-left"> 604 <h1 class="mt-0 pt-0">Server timeout</h1> 605 <div class="co-error">We are sorry, but your search could not be completed due to server timeouts. Please try again later.</div> 606 </div> 607 </div> 608 </div> 609 </div> 610 611 <!-- feedback invalid search term --> 612 <div class="modal " id="templateSearchErrorModal3" role="dialog" aria-labelledby="Search results" aria-hidden="true"> 613 <div class="modal-dialog modal-lg modal-dialog-centered"> 614 <div class="modal-content p-3"> 615 <div class="modal-body text-left"> 616 <h1 class="mt-0 pt-0">Empty search term</h1> 617 <div class="co-error">You have applied the search with an empty search term. Please revisit and try again.</div> 618 </div> 619 </div> 620 </div> 621 </div> 622 623 <!-- feedback too many requests --> 624 <div class="modal " id="templateSearchErrorModal4" role="dialog" aria-labelledby="Search results" aria-hidden="true"> 625 <div class="modal-dialog modal-lg modal-dialog-centered"> 626 <div class="modal-content p-3"> 627 <div class="modal-body text-left"> 628 <h1 class="mt-0 pt-0">Too many requests</h1> 629 <div class="co-error">We are sorry, but we have received too many parallel search requests. Please try again later.</div> 630 </div> 631 </div> 632 </div> 633 </div> 634 635 <!-- loading --> 636 <div class="modal " id="templateSearchLoadingModal" role="dialog" aria-labelledby="Search results" aria-hidden="true"> 637 <div class="modal-dialog modal-sm modal-dialog-centered"> 638 <div class="modal-content p-3 co_LoadingDotsContainer"> 639 <div class="modal-body"> 640 <div class="text">Searching</div> 641 <div class="dots d-flex justify-content-center"><div class="dot"></div><div class="dot"></div><div class="dot"></div></div></div> 642 </div> 643 </div> 644 </div> 645 646</div> 647<style> 648 /*.modal {*/ 649 /* background: rgba(255, 255, 255, 0.8);*/ 650 /*}*/ 651 .modal-header--sticky { 652 position: sticky; 653 top: 0; 654 background-color: inherit; 655 z-index: 1055; 656 } 657 .grid-container 658 { 659 margin-bottom: 1em; 660 /*padding-left: 0;*/ 661 /*padding-right: 0;*/ 662 } 663 #templateSearchInfo{ 664 display: none; 665 background-color: var(--background-color-primary);
666 margin-top: 1px; 667 z-index: 5; 668 border: 1px solid var(--color-primary); 669 opacity: .8; 670 font-size: .7rem; 671 border-radius: .25rem; 672 } 673 674 675 #templateSearchLoadingModal .co_LoadingDotsContainer 676 { 677 z-index: 1000; 678 } 679 #templateSearchLoadingModal .co_LoadingDotsContainer .text 680 { 681 text-align: center; 682 font-weight: bold; 683 padding-bottom: 1rem; 684 } 685 #templateSearchLoadingModal .co_LoadingDotsContainer .dot 686 { 687 background-color: #0072BC; 688 border: 2px solid white; 689 border-radius: 50%; 690 float: left; 691 height: 2rem; 692 width: 2rem; 693 margin: 0 5px; 694 -webkit-transform: scale(0); 695 transform: scale(0); 696 -webkit-animation: animation_dots_breath 1000ms ease infinite 0ms; 697 animation: animation_dots_breath 1000ms ease infinite 0ms; 698 } 699 #templateSearchLoadingModal .co_LoadingDotsContainer .dot:nth-child(2) 700 { 701 -webkit-animation: animation_dots_breath 1000ms ease infinite 300ms; 702 animation: animation_dots_breath 1000ms ease infinite 300ms; 703 } 704 #templateSearchLoadingModal .co_LoadingDotsContainer .dot:nth-child(3) 705 { 706 -webkit-animation: animation_dots_breath 1000ms ease infinite 600ms; 707 animation: animation_dots_breath 1000ms ease infinite 600ms; 708 } 709 #templateSearchResultModal [class*="grid-"] { 710 padding-left: 10px !important; 711 padding-right: 10px !important; 712 } 713 #templateSearchResultTerm { 714 font-weight: bold; 715 } 716 717 #resultsSearchHeader { 718 display: block !important; 719 } 720 #scrolltopmodal { 721 font-size: 3.0em; 722 margin-top: 0 !important; 723 margin-right: 15px; 724 } 725 726 @-webkit-keyframes animation_dots_breath { 727 50% { 728 -webkit-transform: scale(1); 729 transform: scale(1); 730 opacity: 1; 731 } 732 100% { 733 opacity: 0; 734 } 735 } 736 @keyframes animation_dots_breath { 737 50% { 738 -webkit-transform: scale(1); 739 transform: scale(1); 740 opacity: 1; 741 } 742 100% { 743 opacity: 0; 744 } 745 } 746 747 @media (min-width: 768px) and (max-width: 991px) { 748 #templateSearchResultModal .modal-dialog { 749 max-width: 90%; 750 } 751 } 752 753</style>
754<script> 755 756 if(document.querySelector('meta[name="global_moBaseURL"]').content == "https://meetingorganizer.copernicus.org/") 757 FINDER_URL = document.querySelector('meta[name="global_moBaseURL"]').content.replace('meetingorganizer', 'finder-app')+"search/library.php"; 758 else 759 FINDER_URL = document.querySelector('meta[name="global_moBaseURL"]').content.replace('meetingorganizer', 'finder')+"search/library.php"; 760 761 SEARCH_INPUT = document.getElementById('search_query_solr'); 762 SEARCH_INPUT_MODAL = document.getElementById('search_query_modal'); 763 searchRunning = false; 764 765 offset = 20; 766 INITIAL_OFFSET = 20; 767 768 var MutationObserver = window.MutationObserver || window.WebKitMutationObserver || window.MozMutationObserver; 769 const targetNodeSearchModal = document.getElementById("templateSearchResultModal"); 770 const configSearchModal = { attributes: true, childList: true, subtree: true }; 771 772 // Callback function to execute when mutations are observed 773 const callbackSearchModal = (mutationList, observer) => { 774 for (const mutation of mutationList) { 775 if (mutation.type === "childList") { 776 // console.log("A child node has been added or removed."); 777 picturesGallery(); 778 } else if (mutation.type === "attributes") { 779 // console.log(`The ${mutation.attributeName} attribute was modified.`); 780 } 781 } 782 }; 783 784 // Create an observer instance linked to the callback function 785 const observer = new MutationObserver(callbackSearchModal); 786 787 // Start observing the target node for configured mutations 788 observer.observe(targetNodeSearchModal, configSearchModal); 789 790 function _addEventListener() 791 { 792 document.getElementById('search_query_solr').addEventListener('keypress', (e) => { 793 if (e.key === 'Enter') 794 _runSearch(); 795 }); 796 document.getElementById('start_site_search_solr').addEventListener('click', (e) => { 797 _runSearch(); 798 e.stopPropagation(); 799 e.stopImmediatePropagation(); 800 return false; 801 }); 802 803 $('#templateSearchResultModal').scroll(function() { 804 if ($(this).scrollTop()) { 805 $('#scrolltopmodal:hidden').stop(true, true).fadeIn().css("display","inline-block"); 806 } else { 807 $('#scrolltopmodal').stop(true, true).fadeOut(); 808 } 809 }); 810 811 } 812 813 function scrollModalTop() 814 { 815 $('#templateSearchResultModal').animate({ scrollTop: 0 }, 'slow'); 816 // $('#templateSearchResultModal').scrollTop(0); 817 818 } 819 820 function picturesGallery() 821 { 822 $('body').off('click', '.paperlist-avatar img'); 823 $('body').off('click', '#templateSearchResultContainer .paperlist-avatar img'); 824 searchPaperListAvatar = []; 825 searchPaperListAvatarThumb = []; 826 search_pswpElement = document.querySelectorAll('.pswp')[0]; 827 if (typeof search_gallery != "undefined") { 828 search_gallery = null; 829 } 830 $('body').on('click', '#templateSearchResultContainer .paperlist-avatar img', function (e) { 831 if(searchPaperListAvatarThumb.length === 0 && searchPaperListAvatar.length === 0) { 832 $('#templateSearchResultContainer .paperlist-avatar img').each(function () { 833 834 var webversion = $(this).attr('data-web'); 835 var width = $(this).attr('data-width'); 836 var height = $(this).attr('data-height'); 837 var caption = $(this).attr('data-caption'); 838 839 var figure = { 840 src: webversion, 841 w: width, 842 h: height, 843 title: caption 844 }; 845 searchPaperListAvatarThumb.push($(this)[0]); 846 searchPaperListAvatar.push(figure); 847 }); 848 } 849 var target = $(this); 850 var index = $('#templateSearchResultContainer .paperlist-avatar img').index(target); 851 var options = { 852 showHideOpacity:false, 853 bgOpacity:0.8, 854 index:index, 855 spacing:0.15, 856 history: false, 857 focus:false, 858 getThumbBoundsFn: function(index) { 859 var thumbnail = searchPaperListAvatarThumb[index]; 860 var pageYScroll = window.pageYOffset || document.documentElement.scrollTop; 861 var rect = thumbnail.getBoundingClientRect(); 862 return {x:rect.left, y:rect.top + pageYScroll, w:rect.width}; 863 } 864 }; 865 search_gallery = new PhotoSwipe( search_pswpElement, PhotoSwipeUI_Default,[searchPaperListAvatar[index]],options); 866 search_gallery.init(); 867 }); 868 } 869 function showError(code, msg) 870 { 871 console.error(code, msg); 872 873 $("#templateSearchLoadingModal").modal("hide"); 874 875 switch(code) 876 { 877 case -3: // http request fail 878 case -2: // invalid MO response 879 case 4: // CORS 880 case 1: // project 881 $("#templateSearchErrorModal1").modal({}); 882 break; 883 case -1: // timeout 884 $("#templateSearchErrorModal2").modal({}); 885 break; 886 case 2: // empty term 887 $("#templateSearchErrorModal3").modal({}); 888 break; 889 case 3: // DOS 890 $("#templateSearchErrorModal4").modal({}); 891 break; 892 default: 893 $("#templateSearchErrorModal1").modal({}); 894 break; 895 } 896 } 897 function clearForm() { 898 var myFormElement = document.getElementById("library-filters") 899 var elements = myFormElement.elements; 900 $(".form-check-input").prop('checked', false).change().parent().removeClass('active'); 901 for(i=0; i<elements.length; i++) { 902 field_type = elements[i].type.toLowerCase(); 903 switch(field_type) { 904 case "text": 905 case "password": 906 case "textarea": 907 case "hidden": 908 elements[i].value = ""; 909 break; 910 case "radio": 911 case "checkbox": 912 if (elements[i].checked) { 913 elements[i].checked = false; 914 } 915 break; 916 917 case "select-one": 918 case "select-multi": 919 elements[i].selectedIndex = -1; 920 break; 921 922 default: 923 break; 924 } 925 } 926 } 927 928 function generateShowMoreButton(offset, term) 929 { 930 var code = '<button aria-label="ShowMore" id="showMore" class="btn btn-success float-right mr-2" data-offset="' + offset + '">Show more</button>'; 931 return code; 932 } 933 934 function hideModal(id) 935 { 936 $("#"+id).modal('hide'); 937 } 938 939 function showModal(id) 940 { 941 $("#"+id).modal({}); 942 } 943 944 function prepareForPhotoSwipe() 945 { 946 searchPaperListAvatar = []; 947 searchPaperListAvatarThumb = []; 948 search_pswpElement = document.querySelectorAll('.pswp')[0]; 949 } 950 951 function _sendAjax(projectID, term) 952 { 953 let httpRequest = new XMLHttpRequest(); 954 if(searchRunning) 955 { 956 console.log("Search running"); 957 return; 958 } 959 960 if (!httpRequest) { 961 console.error("Giving up :( Cannot create an XMLHTTP instance"); 962 showError(-1); 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1001 else 1002 $("#templateSearchResultNrPlural").show(); 1003 if(rs.resultsNr==0) 1004 { 1005 hideModal('templateSearchLoadingModal'); 1006 $("#templateSearchResultContainer").html(""); 1007 $("#templateSearchResultContainerEmpty").removeClass("d-none"); 1008 showModal('templateSearchResultModal'); 1009 } 1010 else 1011 { 1012 if((rs.resultsNr - offset)>0) 1013 { 1014 html = html + generateShowMoreButton(offset, term); 1015 } 1016 $("#templateSearchResultContainerEmpty").addClass("d-none"); 1017 if( offset == INITIAL_OFFSET) 1018 { 1019 hideModal('templateSearchLoadingModal'); 1020 $("#templateSearchResultContainer").html(html); 1021 showModal('templateSearchResultModal'); 1022 } 1023 else 1024 { 1025 $('#showMore').remove(); 1026 startHtml = $("#templateSearchResultContainer").html(); 1027 $("#templateSearchResultContainer").html(startHtml + html); 1028 } 1029 // prepareForPhotoSwipe(); 1030 } 1031 } 1032 } 1033 else 1034 { 1035 showError(-2, "invalid result"); 1036 } 1037 } else { 1038 showError(-3, "There was a problem with the request."); 1039 } 1040 } 1041 }; 1042 if(offset == INITIAL_OFFSET) 1043 { 1044 hideModal('templateSearchResultModal'); 1045 showModal('templateSearchLoadingModal'); 1046 } 1047 1048 httpRequest.open("GET", FINDER_URL+"?project="+projectID+"&term="+encodeURI(term)+((offset>INITIAL_OFFSET)?("&offset="+(offset-INITIAL_OFFSET)) : "")); 1049 httpRequest.send(); 1050 searchRunning = true; 1051 } 1052 1053 function _runSearch() 1054 { 1055 var projectID = document.querySelector('meta[name="global_projectID"]').content; 1056 var term = _searchTrimInput(SEARCH_INPUT.value); 1057 1058 if(term.length > 0) 1059 { 1060 _sendAjax(projectID, term); 1061 } 1062 else 1063 { 1064 showError(2, 'Empty search term') 1065 } 1066 } 1067 function _searchTrimInput(str) { 1068 return str.replace(/^\s+|\s+$/gm, ''); 1069 } 1070 1071 function run() 1072 { 1073 _addEventListener(); 1074 1075 $('#templateSearchInfoBtn, #modalSearchInfoBtn').popover({ 1076 sanitize: false, 1077 html: true, 1078 content: $("#templateSearchInfo").html(), 1079 placement: "bottom", 1080 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>', 1081 title: "Search tips", 1082 }); 1083 $(document).click(function (e) { 1084 let t = $(e.target); 1085 let a = t && t.attr("data-toggle")!=="popover" && t.parent().attr("data-toggle")!=="popover"; 1086 let b = t && $(".popover").has(t).length===0; 1087 if(a && b) 1088 { 1089 $('#templateSearchInfoBtn').popover('hide'); 1090 $('#modalSearchInfoBtn').popover('hide'); 1091 } 1092 }); 1093 $('#templateSearchInfoBtn').on('shown.bs.popover', function () { 1094 $("#templateSearchInfoClose").click(function(e){
1095 $('#templateSearchInfoBtn').popover('hide'); 1096 e.stopPropagation(); 1097 e.stopImmediatePropagation(); 1098 return false; 1099 }); 1100 }) 1101 $('#templateSearchResultModal').on('hidden.bs.modal', function(e) { 1102 $('body').off('click', '#templateSearchResultContainer .paperlist-avatar img'); 1103 var pswpElement = document.querySelectorAll('.pswp')[0]; 1104 var gallery = null; 1105 var paperListAvatar = []; 1106 var paperListAvatarThumb = []; 1107 $('.paperlist-avatar img').each(function(){ 1108 var webversion = $(this).attr('data-web'); 1109 var width = $(this).attr('data-width'); 1110 var height = $(this).attr('data-height'); 1111 var caption =$(this).attr('data-caption'); 1112 1113 var figure = { 1114 src:webversion, 1115 w:width, 1116 h:height, 1117 title:caption 1118 }; 1119 paperListAvatarThumb.push($(this)[0]); 1120 paperListAvatar.push(figure); 1121 }); 1122 $('body').on('click', '.paperlist-avatar img', function (e) { 1123 if(paperListAvatarThumb.length === 0 && paperListAvatar.length === 0){ 1124 $('.paperlist-avatar img').each(function(){ 1125 var webversion = $(this).attr('data-web'); 1126 var width = $(this).attr('data-width'); 1127 var height = $(this).attr('data-height'); 1128 var caption =$(this).attr('data-caption'); 1129 1130 var figure = { 1131 src:webversion, 1132 w:width, 1133 h:height, 1134 title:caption 1135 }; 1136 paperListAvatarThumb.push($(this)[0]); 1137 paperListAvatar.push(figure); 1138 }); 1139 } 1140 var target = $(this); 1141 var index = $('.paperlist-avatar img').index(target); 1142 var options = { 1143 showHideOpacity:true, 1144 bgOpacity:0.8, 1145 index:index, 1146 spacing:0.15, 1147 getThumbBoundsFn: function(index) { 1148 1149 var thumbnail = paperListAvatarThumb[index]; 1150 var pageYScroll = window.pageYOffset || document.documentElement.scrollTop; 1151 var rect = thumbnail.getBoundingClientRect(); 1152 return {x:rect.left, y:rect.top + pageYScroll, w:rect.width}; 1153 } 1154 }; 1155 gallery = new PhotoSwipe( pswpElement, PhotoSwipeUI_Default,[paperListAvatar[index]],options); 1156 gallery.init(); 1157 }); 1158 1159 }); 1160 $('#templateSearchResultModal').on('hide.bs.modal', function(e) { 1161 $("#templateRefineSearch").removeClass('d-block').addClass('d-none'); 1162 $("#refineSearchModalHide").removeClass('d-block').addClass('d-none'); 1163 $("#refineSearchModal").removeClass('d-none').addClass('d-block'); 1164 offset = INITIAL_OFFSET; 1165 }) 1166 1167 $(document).on("click", "#showMore", function(e){ 1168 offset+=INITIAL_OFFSET; 1169 runSearchModal() 1170 e.stopPropagation(); 1171 e.stopImmediatePropagation(); 1172 return false; 1173 }); 1174 1175 1176 1177 $(document).ready(function() { 1178 $(document).on("click", "#refineSearchModal", function (e) { 1179 $("#templateRefineSearch").removeClass('d-none').addClass('d-block'); 1180 $(this).removeClass('d-block').addClass('d-none'); 1181 $("#refineSearchModalHide").removeClass('d-none').addClass('d-block'); 1182 }); 1183 $(document).on("click", "#refineSearchModalHide", function (e) { 1184 $("#templateRefineSearch").removeClass('d-block').addClass('d-none'); 1185 $(this).removeClass('d-block').addClass('d-none'); 1186 $("#refineSearchModal").removeClass('d-none').addClass('d-block'); 1187 }); 1188 1189 $(document).on("click", "#modal_start_site_search", function (e) { 1190 runSearchModal(); 1191 e.stopPropagation(); 1192 e.stopImmediatePropagation(); 1193 return false; 1194 }); 1195 }); 1196 } 1197 1198 function runSearchModal() 1199 { 1200 var projectID = document.querySelector('meta[name="global_projectID"]').content;
1201 var queryString = $('#library-filters').serialize(); 1202 var term = _searchTrimInput($('#modal_search_query').val()); 1203 term+='&'+queryString; 1204 if(term.length > 0) 1205 { 1206 _sendAjax(projectID, term); 1207 } 1208 else 1209 { 1210 showError(2, 'Empty search term') 1211 } 1212 } 1213 1214 if(document.getElementById('search_query_solr')) 1215 { 1216 run(); 1217 } 1218 1219</script>
1219 1220<!-- END_SITE_SEARCH --></div></div> 1221 1222 <!-- END_SNIPPET:part10 --> 1223 1224 </div> 1225 1226 </div> 1227 1228 </div> 1229 1230 </div> 1231 1232</header> 1233 1234<!--=== Content ===--> 1235 1236<main class="one-column version-2023"> 1237 1238 <div id="content" class="container"> 1239 1240 <div id="page_content_container" class="CMSCONTAINER content-container"> 1241 1242 <!-- $$CONTENT$$ --> 1243 1244 <!-- START_LEFT_REMOVABLE_SECTION --> 1245 1246 <!-- END_LEFT_REMOVABLE_SECTION --> 1247 1248 <div id="cmsbox_89190" class="cmsbox "><h1>Scheduled special issues</h1></div><div id="special-issues-scheduled-content" class="cmsbox "> <p>The following special issues are scheduled for publication in ESSD:</p> 1249 1250 <div class="grid-container grid-parent special-issue-tabs"> 1251 <div class="grid-20 tablet-grid-20 mobile-grid-100 grid-parent"> 1252 <a class="show-hide triangle" data-hide="#chronologically" data-show="#alphabetically" href="#">Alphabetically</a> 1253 </div> 1254 <div class="grid-20 tablet-grid-20 mobile-grid-100 grid-parent"> 1255 <a class="show-hide triangle active" data-hide="#alphabetically" data-show="#chronologically" href="#">Chronologically</a> 1256 </div> 1257 </div> 1258 <div class="grid-container grid-parent"> 1259 <div class="grid-100 tablet-grid-100 mobile-grid-100 grid-parent" id="alphabetically" style="display: none;"> 1260 <h2 class="group-special-issue">A</h2> 1261 <div class="grid-container grid-parent special-issue triangle_special_issues"> 1262 <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> 1263 <a href="https://essd.copernicus.org/articles/special_issue760_1401.html">Advances in annual to decadal prediction, projection, and attribution</a> 1264 (WCD/ESD/ESSD/GMD inter-journal SI) 1265 </div> 1266 <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 1267 20 May 2026–31 May 2028 | Chaim Garfinkel (Hebrew University of Jerusalem, Israel), Stephanie Fiedler (Heidelberg University, Germany), and Graciela Raga (Universidad Nacional Autónoma de México, Mexico) | 1268 <a href="javascript:void(0);" class="info-link show-hide" id="info-alphabetically-link-1401" data-show="#info-alphabetically-content-1401" data-hide="#info-alphabetically-link-1401">Information</a> 1269 </div> 1270 <div class="j-widget__max short_summary" id="info-alphabetically-content-1401" style="display: none"> 1271 <div class="widget dark-border"> 1272 <div class="legend journal-contentLinkColor">Information</div> 1273 <div class="content" id="1401"> 1274 <p>There is a crucial societal need to develop an integrated capability to understand, attribute, and predict annual to decadal changes in the Earthâs climate system, including capabilities for early warning of potential high-impact events and changes. To meet this need, the climate science community needs to provide actionable scientific information that meets the evolving needs of societies all over the world. This goal is shared by the World Climate Research Programme (WCRP) Lighthouse Activity on Explaining and Predicting Earth System Change (EPESC) and by the WCRPâs core project Atmospheric Processes and their Role in Climate (APARC) Large Ensembles for Attribution of Dynamically-driven ExtRemes (LEADER) activity.</p> 1275<p>In pursuit of this goal, this special issue welcomes research that addresses prediction, projection, and attribution of phenomena and events acting on annual to decadal timescales. This includes evaluating existing and developing new methodologies to attribute and predict changes and extremes driven by the atmospheric or oceanic circulation. We also seek advances that can lead to more reliable quantitative attribution statements to support the Global Annual to Decadal Climate Update and State of the Climate reports issued by the World Meteorological Organization and to improved projections.</p> 1276<p>While early warnings of changes in the Earth system are now potentially possible through, e.g., operational decadal predictions, there are several challenges: there is a lack of understanding of the dynamical mechanisms that enable such projections, and there is evidence that global models underestimate some predictable signals and that there are systematic discrepancies between simulated and observed trends. The special issue seeks research that highlights these challenges and improves our understanding of the causes of regional climate changes, needed both to attribute recent events and to gain further confidence in forecasts.</p> 1277<p>A particular focus of this special issue is papers that analyze output from the Large Ensemble Single Forcing Model Intercomparison Project (LESFMIP; Smith et al., 2022), as these coordinated model experiments will enable the impacts of different external drivers to be isolated that otherwise would be buried under internal variability while also offering a testbed for methods to extract predictable signals with the correct amplitude.</p> 1278 </div> 1279 <div class="row"> 1280 <div class="col-auto"> 1281 <a href="#" class="show-hide triangle" data-hide="#info-alphabetically-content-1401" 1282 data-show="#info-alphabetically-link-1401">Hide</a> 1283 </div> 1284 <div class="col text-right"> 1285 <a class="si-mobile-native-share" href="#" data-title="Advances in annual to decadal prediction, projection, and attribution" data-url="https://essd.copernicus.org/articles/special_issue760_1401.html" data-id="1401" style="display: none;"> 1286 <i class="fas fa-lg fa-share-alt"></i> 1287 </a> 1288 <a class="desktop-share" href="#" data-title="Advances in annual to decadal prediction, projection, and attribution" data-url="https://essd.copernicus.org/articles/special_issue760_1401.html" data-id="1401" title="Copy to clipboard"> 1289 <i class="fas fa-lg fa-share-alt"></i> 1290 </a> 1291 </div> 1292 </div> 1293 </div> 1294 </div> 1295 </div> 1296 1297 1298 <div class="grid-container grid-parent special-issue triangle_special_issues">
1299 <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> 1300 <a href="https://essd.copernicus.org/articles/special_issue10_1389.html">Aerosol, fog, climate, and biogeochemistry in southern Africa</a> 1301 (ACP/AMT/AR/ESSD inter-journal SI) 1302 </div> 1303 <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 1304 01 Jan 2026–31 Dec 2028 | Paola Formenti (Centre national de la recherche scientifique, France), Hendrik Andersen (Karlsruhe Institute of Technology, Germany), and Kirsten Elger (GFZ Helmholtz Centre for Geosciences, Germany) | 1305 <a href="javascript:void(0);" class="info-link show-hide" id="info-alphabetically-link-1389" data-show="#info-alphabetically-content-1389" data-hide="#info-alphabetically-link-1389">Information</a> 1306 </div> 1307 <div class="j-widget__max short_summary" id="info-alphabetically-content-1389" style="display: none"> 1308 <div class="widget dark-border"> 1309 <div class="legend journal-contentLinkColor">Information</div> 1310 <div class="content" id="1389"> 1311 <p>The purpose of this special issue is the compilation of modelling and observational studies on the role of atmospheric aerosols in the life cycle and composition of fog and low clouds in southern Africa as well as their mutual links with climate and biogeochemistry.</p> 1312<p>The special issue is motivated by new results from the AeroFog project, focusing on the hyperarid coastal deserts of Namibia, on the western coast of southern Africa. AeroFog is based on two intensive, ground-based field deployments, which took place in May and September 2024 along the coast and in the desert, and the long-term monitoring and analysis of remote-sensing products. Observations, satellite measurements, and modelling address the aerosol radiative, chemical, and microphysical interactions relevant to fog as well as the meteorological fields and dynamical processes that influence aerosol emission, transport, and deposition. Building on the diverse expertise of scientists in both the Northern and the Southern hemispheres, AeroFog aims to develop a holistic understanding of the mechanisms by which nutrients and pollutants are found in fog and the effect of fog on the biogeochemistry of regional ecosystems. The special issue comprises papers with complementary goals so as to encourage the exchange of ideas among previous, current, and planned large-scale projects and activities in the region.</p> 1313 </div> 1314 <div class="row"> 1315 <div class="col-auto"> 1316 <a href="#" class="show-hide triangle" data-hide="#info-alphabetically-content-1389" 1317 data-show="#info-alphabetically-link-1389">Hide</a> 1318 </div> 1319 <div class="col text-right"> 1320 <a class="si-mobile-native-share" href="#" data-title="Aerosol, fog, climate, and biogeochemistry in southern Africa" data-url="https://essd.copernicus.org/articles/special_issue10_1389.html" data-id="1389" style="display: none;"> 1321 <i class="fas fa-lg fa-share-alt"></i> 1322 </a> 1323 <a class="desktop-share" href="#" data-title="Aerosol, fog, climate, and biogeochemistry in southern Africa" data-url="https://essd.copernicus.org/articles/special_issue10_1389.html" data-id="1389" title="Copy to clipboard"> 1324 <i class="fas fa-lg fa-share-alt"></i> 1325 </a> 1326 </div> 1327 </div> 1328 </div> 1329 </div> 1330 </div> 1331 1332 <h2 class="group-special-issue">C</h2> 1333 <div class="grid-container grid-parent special-issue triangle_special_issues">
1334 <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> 1335 <a href="https://essd.copernicus.org/articles/special_issue365_1307.html">Coupled Model Intercomparison Project Phase 7 (CMIP7) forcings and inputs – development, documentation, and evaluation</a> 1336 (GMD/ESSD inter-journal SI) 1337 </div> 1338 <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 1339 11 Mar 2024–31 Mar 2029 | ESSD topic editors | Coordinators: John Dunne (NOAA Geophysical Fluid Dynamics Laboratory, United States), Helene Hewitt (Met Office, United Kingdom), and Eleanor O'Rourke (WCRP-CMIP International Project Office, United Kingdom) | 1340 <a href="javascript:void(0);" class="info-link show-hide" id="info-alphabetically-link-1307" data-show="#info-alphabetically-content-1307" data-hide="#info-alphabetically-link-1307">Information</a> 1341 </div> 1342 <div class="j-widget__max short_summary" id="info-alphabetically-content-1307" style="display: none"> 1343 <div class="widget dark-border"> 1344 <div class="legend journal-contentLinkColor">Information</div> 1345 <div class="content" id="1307"> 1346 <p>The natural and anthropogenic climate drivers that impact Earthâs radiation balance, influencing climate states and <q>forcing</q> climate change are termed <q>climate forcing</q> agents. Globally representative forcing estimates are needed to drive Earth system models to simulate past and project future climate states. The Coupled Model Intercomparison Project (CMIP) <a href="https://wcrp-cmip.org/cmip7-task-teams/forcings/"target="_blank">Forcing Task Team</a> aims to identify, develop, document, and deliver forcings for next-generation models participating in the seventh phase of CMIP (CMIP7). This next phase is likely to be a core contribution to the IPCC seventh assessment cycle (AR7). The special issue welcomes papers documenting forcing data development and evaluation, along with those describing CMIP7 forcing characteristics (in contrast to previous versions). We also invite papers that quantify and assess uncertainties in the spatial and temporal forcing distributions and the influence of forcing on the evolution of climate states across Earth system model configurations.</p> 1347 </div> 1348 <div class="row"> 1349 <div class="col-auto"> 1350 <a href="#" class="show-hide triangle" data-hide="#info-alphabetically-content-1307" 1351 data-show="#info-alphabetically-link-1307">Hide</a> 1352 </div> 1353 <div class="col text-right"> 1354 <a class="si-mobile-native-share" href="#" data-title="Coupled Model Intercomparison Project Phase 7 (CMIP7) forcings and inputs – development, documentation, and evaluation" data-url="https://essd.copernicus.org/articles/special_issue365_1307.html" data-id="1307" style="display: none;"> 1355 <i class="fas fa-lg fa-share-alt"></i> 1356 </a> 1357 <a class="desktop-share" href="#" data-title="Coupled Model Intercomparison Project Phase 7 (CMIP7) forcings and inputs – development, documentation, and evaluation" data-url="https://essd.copernicus.org/articles/special_issue365_1307.html" data-id="1307" title="Copy to clipboard"> 1358 <i class="fas fa-lg fa-share-alt"></i> 1359 </a> 1360 </div> 1361 </div> 1362 </div> 1363 </div> 1364 </div> 1365 1366 <h2 class="group-special-issue">M</h2> 1367 <div class="grid-container grid-parent special-issue triangle_special_issues">
1368 <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> 1369 <a href="https://essd.copernicus.org/articles/special_issue365_1284.html">Model Intercomparison and Improvement Projects (MIIPs) for the polar regions and beyond (GMD/ESSD inter-journal SI)</a> 1370 (GMD/ESSD inter-journal SI) 1371 </div> 1372 <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 1373 25 Sep 2023–indefinite | Gunilla Svensson (Stockholm University, Sweden), Matthew D. Shupe (University of Colorado Colorado Springs, United States), Felix Pithan (Alfred Wegener Institute for Polar and Marine Research, Germany), and Ken Mankoff (Goddard Institute for Space Studies, United States) | 1374 <a href="javascript:void(0);" class="info-link show-hide" id="info-alphabetically-link-1284" data-show="#info-alphabetically-content-1284" data-hide="#info-alphabetically-link-1284">Information</a> 1375 </div> 1376 <div class="j-widget__max short_summary" id="info-alphabetically-content-1284" style="display: none"> 1377 <div class="widget dark-border"> 1378 <div class="legend journal-contentLinkColor">Information</div> 1379 <div class="content" id="1284"> 1380 <p>For this SI we welcome manuscripts on activities such as MIIPs â Model Intercomparison and Improvement Projects that target long-standing issues in the representation of small-scale processes in numerical weather prediction and climate models. The initiatives may have been taken during the 10-year Polar Prediction Project (PPP) that finished at the end of 2022 or during the Polar Coupled Analysis and Prediction for Services (PCAPS
1380) both part of the WMO World Weather Research Program. These programs suggest an emphasis on processes that are especially important for the polar regions, but contributions that are relevant and important for model performance in other regions of the world are also welcome. Specific targets are the representation of stably stratified boundary layers, mixed-phase clouds and atmospheric coupling with snow and or ice-covered surfaces, sea-ice, ocean mixing etc.</p> 1381<p>The intention of this SI is to publish results from MIIPs that establish new and improved workflows to facilitate a more efficient path to improved process representation. This includes research-grade observations that are packaged in an easy-to-use format which combine high-frequency observations of the surface and the atmosphere above to be able to directly compare with the parameterizations used in models using time-step data. The Merged Data File (MDF) format that is defined for both observations and model output come with a series of tools that is transferable between models and observational data collections for both file production and analysis. The SI especially welcome contributions that build on, or further develop the MDF concept including new variables, types of data, sites or new analysis tools such as process-oriented diagnostics or insights in models using the targeted files.</p> 1382 </div> 1383 <div class="row"> 1384 <div class="col-auto"> 1385 <a href="#" class="show-hide triangle" data-hide="#info-alphabetically-content-1284" 1386 data-show="#info-alphabetically-link-1284">Hide</a> 1387 </div> 1388 <div class="col text-right"> 1389 <a class="si-mobile-native-share" href="#" data-title="Model Intercomparison and Improvement Projects (MIIPs) for the polar regions and beyond (GMD/ESSD inter-journal SI)" data-url="https://essd.copernicus.org/articles/special_issue365_1284.html" data-id="1284" style="display: none;"> 1390 <i class="fas fa-lg fa-share-alt"></i> 1391 </a> 1392 <a class="desktop-share" href="#" data-title="Model Intercomparison and Improvement Projects (MIIPs) for the polar regions and beyond (GMD/ESSD inter-journal SI)" data-url="https://essd.copernicus.org/articles/special_issue365_1284.html" data-id="1284" title="Copy to clipboard"> 1393 <i class="fas fa-lg fa-share-alt"></i> 1394 </a> 1395 </div> 1396 </div> 1397 </div> 1398 </div> 1399 </div> 1400 1401 <h2 class="group-special-issue">O</h2> 1402 <div class="grid-container grid-parent special-issue triangle_special_issues"> 1403 <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> 1404 <a href="https://essd.copernicus.org/articles/special_issue25_968.html">Oldest Ice: finding and interpreting climate proxies in ice older than 700 000 years</a> 1405 (TC/CP/ESSD inter-journal SI) 1406 </div> 1407 <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 1408 01 Jan 2013–31 Dec 2027 | ESSD editors | Coordinators: Thomas Blunier (University of Copenhagen, Denmark) and Reinhard Drews (University of Tübingen, Germany) | 1409 <a href="javascript:void(0);" class="info-link show-hide" id="info-alphabetically-link-968" data-show="#info-alphabetically-content-968" data-hide="#info-alphabetically-link-968">Information</a> 1410 </div> 1411 <div class="j-widget__max short_summary" id="info-alphabetically-content-968" style="display: none"> 1412 <div class="widget dark-border"> 1413 <div class="legend journal-contentLinkColor">Information</div> 1414 <div class="content" id="968"> 1415 <p>The glacialâinterglacial cyclicity of the climate system varied in the past, most notably during the transition from a 40 ka to a 100 ka world in the mid-Pleistocene. Gases trapped in Antarctic ice are the most direct access available to investigate the composition of the paleo-atmosphere of that age and processes related to climate variability. The International Partnerships in Ice Core Sciences (IPICS) Oldest Ice endeavour aims at obtaining an undisturbed ice-core record older than 1 Ma. In addition to ice cores, time slices of paleo-records, available, for example, in Antarctic blue-ice fields, provide further valuable information, which complements continuous time series based on ice cores. This special issue will assemble contributions dedicated to the preparatory phase of this global effort to obtain ice samples and time series older than 700 000 years. This includes a consideration of glaciogical and geophysical settings which allow the presence of old ice, results from pre-site surveys and modelling studies, aspects of ice-core and other sampling techniques and analyses, and requirements for drilling and core handling.</p> 1416 </div> 1417 <div class="row"> 1418 <div class="col-auto"> 1419 <a href="#" class="show-hide triangle" data-hide="#info-alphabetically-content-968" 1420 data-show="#info-alphabetically-link-968">Hide</a> 1421 </div> 1422 <div class="col text-right"> 1423 <a class="si-mobile-native-share" href="#" data-title="Oldest Ice: finding and interpreting climate proxies in ice older than 700 000 years" data-url="https://essd.copernicus.org/articles/special_issue25_968.html" data-id="968" style="display: none;"> 1424 <i class="fas fa-lg fa-share-alt"></i> 1425 </a> 1426 <a class="desktop-share" href="#" data-title="Oldest Ice: finding and interpreting climate proxies in ice older than 700 000 years" data-url="https://essd.copernicus.org/articles/special_issue25_968.html" data-id="968" title="Copy to clipboard"> 1427 <i class="fas fa-lg fa-share-alt"></i> 1428 </a> 1429 </div> 1430 </div> 1431 </div> 1432 </div> 1433 </div> 1434 1435 <h2 class="group-special-issue">T</h2> 1436 <div class="grid-container grid-parent special-issue triangle_special_issues">
1437 <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> 1438 <a href="https://essd.copernicus.org/articles/special_issue760_1406.html">TEAMx (Multi-scale transport and exchange processes in the atmosphere over mountains â programme and experiment)</a> 1439 (WCD/ACP/AMT/ESSD/GMD/TC inter-journal SI) 1440 </div> 1441 <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 1442 01 Jul 2026–30 Jun 2031 | Martin Kohler (Karlsruhe Institute of Technology, Germany), Claudia Acquistapace (University of Padua, Italy), and Graciela Raga (Universidad Nacional Autónoma de México, Mexico) | 1443 <a href="javascript:void(0);" class="info-link show-hide" id="info-alphabetically-link-1406" data-show="#info-alphabetically-content-1406" data-hide="#info-alphabetically-link-1406">Information</a> 1444 </div> 1445 <div class="j-widget__max short_summary" id="info-alphabetically-content-1406" style="display: none"> 1446 <div class="widget dark-border"> 1447 <div class="legend journal-contentLinkColor">Information</div> 1448 <div class="content" id="1406"> 1449 <p>Several terrain-induced processes in the atmospheric boundary layer over mountains affect the transport and exchange of heat, momentum, moisture, aerosols, and trace constituents between the surface and the atmosphere and within the atmosphere.</p> 1450<p>TEAMx (Multi-scale transport and exchange processes in the atmosphere over mountains â programme and experiment) is an international research program that aims at improving our understanding of these processes and their representation in numerical weather and climate prediction models. Measurements were collected in a northâsouth transect through the Alps using a range of different instruments as part of the 1-year-long TEAMx Observational Campaign between September 2024 and September 2025. To sample the mountain boundary layer at multiple spatial and temporal scales, observations from various platforms were combined: surface weather and eddy-covariance stations, surface-based remote sensing instruments, radiosoundings, drone-based measurements, and aircraft flights. The observational data were complemented by numerical modeling for process understanding and model development.</p> 1451<p>This special issue collects observational, modeling, and theoretical studies originating from the TEAMx research programme. In particular, we call for contributions that use data collected during the TEAMx Observational Campaign (TOC), use data collected during other TEAMx-related measurement campaigns (e.g., pre-campaign PC22, HEFEX), and result from funded projects endorsed by TEAMx. Idealized modeling studies and theoretical work dealing with meteorological processes in the mountain boundary layer and their parameterization are also welcome.</p> 1452 </div> 1453 <div class="row"> 1454 <div class="col-auto"> 1455 <a href="#" class="show-hide triangle" data-hide="#info-alphabetically-content-1406" 1456 data-show="#info-alphabetically-link-1406">Hide</a> 1457 </div> 1458 <div class="col text-right"> 1459 <a class="si-mobile-native-share" href="#" data-title="TEAMx (Multi-scale transport and exchange processes in the atmosphere over mountains â programme and experiment)" data-url="https://essd.copernicus.org/articles/special_issue760_1406.html" data-id="1406" style="display: none;"> 1460 <i class="fas fa-lg fa-share-alt"></i> 1461 </a> 1462 <a class="desktop-share" href="#" data-title="TEAMx (Multi-scale transport and exchange processes in the atmosphere over mountains â programme and experiment)" data-url="https://essd.copernicus.org/articles/special_issue760_1406.html" data-id="1406" title="Copy to clipboard"> 1463 <i class="fas fa-lg fa-share-alt"></i> 1464 </a> 1465 </div> 1466 </div> 1467 </div> 1468 </div> 1469 </div> 1470 1471 </div> 1472 </div> 1473 1474 <div class="grid-container grid-parent">
1475 <div class="grid-100 tablet-grid-100 mobile-grid-100 grid-parent" id="chronologically"> 1476 <h2 class="group-special-issue">2026</h2> 1477 <div class="grid-container grid-parent special-issue triangle_special_issues"> 1478 <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> 1479 <a href="https://essd.copernicus.org/articles/special_issue760_1406.html">TEAMx (Multi-scale transport and exchange processes in the atmosphere over mountains â programme and experiment)</a> 1480 (WCD/ACP/AMT/ESSD/GMD/TC inter-journal SI) 1481 </div> 1482 <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 1483 01 Jul 2026–30 Jun 2031 | Martin Kohler (Karlsruhe Institute of Technology, Germany), Claudia Acquistapace (University of Padua, Italy), and Graciela Raga (Universidad Nacional Autónoma de México, Mexico) | 1484 <a href="javascript:void(0);" class="info-link show-hide" id="info-chronologically-link-1406" data-show="#info-chronologically-content-1406" data-hide="#info-chronologically-link-1406">Information</a> 1485 </div> 1486 <div class="j-widget__max short_summary" id="info-chronologically-content-1406" style="display: none"> 1487 <div class="widget dark-border"> 1488 <div class="legend journal-contentLinkColor">Information</div> 1489 <div class="content" id="1406"> 1490 <p>Several terrain-induced processes in the atmospheric boundary layer over mountains affect the transport and exchange of heat, momentum, moisture, aerosols, and trace constituents between the surface and the atmosphere and within the atmosphere.</p> 1491<p>TEAMx (Multi-scale transport and exchange processes in the atmosphere over mountains â programme and experiment) is an international research program that aims at improving our understanding of these processes and their representation in numerical weather and climate prediction models. Measurements were collected in a northâsouth transect through the Alps using a range of different instruments as part of the 1-year-long TEAMx Observational Campaign between September 2024 and September 2025. To sample the mountain boundary layer at multiple spatial and temporal scales, observations from various platforms were combined: surface weather and eddy-covariance stations, surface-based remote sensing instruments, radiosoundings, drone-based measurements, and aircraft flights. The observational data were complemented by numerical modeling for process understanding and model development.</p> 1492<p>This special issue collects observational, modeling, and theoretical studies originating from the TEAMx research programme. In particular, we call for contributions that use data collected during the TEAMx Observational Campaign (TOC), use data collected during other TEAMx-related measurement campaigns (e.g., pre-campaign PC22, HEFEX), and result from funded projects endorsed by TEAMx. Idealized modeling studies and theoretical work dealing with meteorological processes in the mountain boundary layer and their parameterization are also welcome.</p> 1493 </div> 1494 <div class="row"> 1495 <div class="col-auto"> 1496 <a href="#" class="show-hide triangle" data-hide="#info-chronologically-content-1406" 1497 data-show="#info-chronologically-link-1406">Hide</a> 1498 </div> 1499 <div class="col text-right"> 1500 <a class="si-mobile-native-share" href="#" data-title="TEAMx (Multi-scale transport and exchange processes in the atmosphere over mountains â programme and experiment)" data-url="https://essd.copernicus.org/articles/special_issue760_1406.html" data-id="1406" style="display: none;"> 1501 <i class="fas fa-lg fa-share-alt"></i> 1502 </a> 1503 <a class="desktop-share" href="#" data-title="TEAMx (Multi-scale transport and exchange processes in the atmosphere over mountains â programme and experiment)" data-url="https://essd.copernicus.org/articles/special_issue760_1406.html" data-id="1406" title="Copy to clipboard"> 1504 <i class="fas fa-lg fa-share-alt"></i> 1505 </a> 1506 </div> 1507 </div> 1508 </div> 1509 </div> 1510 </div> 1511 1512 <div class="grid-container grid-parent special-issue triangle_special_issues">
1513 <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> 1514 <a href="https://essd.copernicus.org/articles/special_issue760_1401.html">Advances in annual to decadal prediction, projection, and attribution</a> 1515 (WCD/ESD/ESSD/GMD inter-journal SI) 1516 </div> 1517 <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 1518 20 May 2026–31 May 2028 | Chaim Garfinkel (Hebrew University of Jerusalem, Israel), Stephanie Fiedler (Heidelberg University, Germany), and Graciela Raga (Universidad Nacional Autónoma de México, Mexico) | 1519 <a href="javascript:void(0);" class="info-link show-hide" id="info-chronologically-link-1401" data-show="#info-chronologically-content-1401" data-hide="#info-chronologically-link-1401">Information</a> 1520 </div> 1521 <div class="j-widget__max short_summary" id="info-chronologically-content-1401" style="display: none"> 1522 <div class="widget dark-border"> 1523 <div class="legend journal-contentLinkColor">Information</div> 1524 <div class="content" id="1401"> 1525 <p>There is a crucial societal need to develop an integrated capability to understand, attribute, and predict annual to decadal changes in the Earthâs climate system, including capabilities for early warning of potential high-impact events and changes. To meet this need, the climate science community needs to provide actionable scientific information that meets the evolving needs of societies all over the world. This goal is shared by the World Climate Research Programme (WCRP) Lighthouse Activity on Explaining and Predicting Earth System Change (EPESC) and by the WCRPâs core project Atmospheric Processes and their Role in Climate (APARC) Large Ensembles for Attribution of Dynamically-driven ExtRemes (LEADER) activity.</p> 1526<p>In pursuit of this goal, this special issue welcomes research that addresses prediction, projection, and attribution of phenomena and events acting on annual to decadal timescales. This includes evaluating existing and developing new methodologies to attribute and predict changes and extremes driven by the atmospheric or oceanic circulation. We also seek advances that can lead to more reliable quantitative attribution statements to support the Global Annual to Decadal Climate Update and State of the Climate reports issued by the World Meteorological Organization and to improved projections.</p> 1527<p>While early warnings of changes in the Earth system are now potentially possible through, e.g., operational decadal predictions, there are several challenges: there is a lack of understanding of the dynamical mechanisms that enable such projections, and there is evidence that global models underestimate some predictable signals and that there are systematic discrepancies between simulated and observed trends. The special issue seeks research that highlights these challenges and improves our understanding of the causes of regional climate changes, needed both to attribute recent events and to gain further confidence in forecasts.</p> 1528<p>A particular focus of this special issue is papers that analyze output from the Large Ensemble Single Forcing Model Intercomparison Project (LESFMIP; Smith et al., 2022), as these coordinated model experiments will enable the impacts of different external drivers to be isolated that otherwise would be buried under internal variability while also offering a testbed for methods to extract predictable signals with the correct amplitude.</p> 1529 </div> 1530 <div class="row"> 1531 <div class="col-auto"> 1532 <a href="#" class="show-hide triangle" data-hide="#info-chronologically-content-1401" 1533 data-show="#info-chronologically-link-1401">Hide</a> 1534 </div> 1535 <div class="col text-right"> 1536 <a class="si-mobile-native-share" href="#" data-title="Advances in annual to decadal prediction, projection, and attribution" data-url="https://essd.copernicus.org/articles/special_issue760_1401.html" data-id="1401" style="display: none;"> 1537 <i class="fas fa-lg fa-share-alt"></i> 1538 </a> 1539 <a class="desktop-share" href="#" data-title="Advances in annual to decadal prediction, projection, and attribution" data-url="https://essd.copernicus.org/articles/special_issue760_1401.html" data-id="1401" title="Copy to clipboard"> 1540 <i class="fas fa-lg fa-share-alt"></i> 1541 </a> 1542 </div> 1543 </div> 1544 </div> 1545 </div> 1546 </div> 1547 1548 <div class="grid-container grid-parent special-issue triangle_special_issues">
1549 <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> 1550 <a href="https://essd.copernicus.org/articles/special_issue10_1389.html">Aerosol, fog, climate, and biogeochemistry in southern Africa</a> 1551 (ACP/AMT/AR/ESSD inter-journal SI) 1552 </div> 1553 <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 1554 01 Jan 2026–31 Dec 2028 | Paola Formenti (Centre national de la recherche scientifique, France), Hendrik Andersen (Karlsruhe Institute of Technology, Germany), and Kirsten Elger (GFZ Helmholtz Centre for Geosciences, Germany) | 1555 <a href="javascript:void(0);" class="info-link show-hide" id="info-chronologically-link-1389" data-show="#info-chronologically-content-1389" data-hide="#info-chronologically-link-1389">Information</a> 1556 </div> 1557 <div class="j-widget__max short_summary" id="info-chronologically-content-1389" style="display: none"> 1558 <div class="widget dark-border"> 1559 <div class="legend journal-contentLinkColor">Information</div> 1560 <div class="content" id="1389"> 1561 <p>The purpose of this special issue is the compilation of modelling and observational studies on the role of atmospheric aerosols in the life cycle and composition of fog and low clouds in southern Africa as well as their mutual links with climate and biogeochemistry.</p> 1562<p>The special issue is motivated by new results from the AeroFog project, focusing on the hyperarid coastal deserts of Namibia, on the western coast of southern Africa. AeroFog is based on two intensive, ground-based field deployments, which took place in May and September 2024 along the coast and in the desert, and the long-term monitoring and analysis of remote-sensing products. Observations, satellite measurements, and modelling address the aerosol radiative, chemical, and microphysical interactions relevant to fog as well as the meteorological fields and dynamical processes that influence aerosol emission, transport, and deposition. Building on the diverse expertise of scientists in both the Northern and the Southern hemispheres, AeroFog aims to develop a holistic understanding of the mechanisms by which nutrients and pollutants are found in fog and the effect of fog on the biogeochemistry of regional ecosystems. The special issue comprises papers with complementary goals so as to encourage the exchange of ideas among previous, current, and planned large-scale projects and activities in the region.</p> 1563 </div> 1564 <div class="row"> 1565 <div class="col-auto"> 1566 <a href="#" class="show-hide triangle" data-hide="#info-chronologically-content-1389" 1567 data-show="#info-chronologically-link-1389">Hide</a> 1568 </div> 1569 <div class="col text-right"> 1570 <a class="si-mobile-native-share" href="#" data-title="Aerosol, fog, climate, and biogeochemistry in southern Africa" data-url="https://essd.copernicus.org/articles/special_issue10_1389.html" data-id="1389" style="display: none;"> 1571 <i class="fas fa-lg fa-share-alt"></i> 1572 </a> 1573 <a class="desktop-share" href="#" data-title="Aerosol, fog, climate, and biogeochemistry in southern Africa" data-url="https://essd.copernicus.org/articles/special_issue10_1389.html" data-id="1389" title="Copy to clipboard"> 1574 <i class="fas fa-lg fa-share-alt"></i> 1575 </a> 1576 </div> 1577 </div> 1578 </div> 1579 </div> 1580 </div> 1581 <h2 class="group-special-issue">2024</h2> 1582 <div class="grid-container grid-parent special-issue triangle_special_issues">
1583 <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> 1584 <a href="https://essd.copernicus.org/articles/special_issue365_1307.html">Coupled Model Intercomparison Project Phase 7 (CMIP7) forcings and inputs – development, documentation, and evaluation</a> 1585 (GMD/ESSD inter-journal SI) 1586 </div> 1587 <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 1588 11 Mar 2024–31 Mar 2029 | ESSD topic editors | Coordinators: John Dunne (NOAA Geophysical Fluid Dynamics Laboratory, United States), Helene Hewitt (Met Office, United Kingdom), and Eleanor O'Rourke (WCRP-CMIP International Project Office, United Kingdom) | 1589 <a href="javascript:void(0);" class="info-link show-hide" id="info-chronologically-link-1307" data-show="#info-chronologically-content-1307" data-hide="#info-chronologically-link-1307">Information</a> 1590 </div> 1591 <div class="j-widget__max short_summary" id="info-chronologically-content-1307" style="display: none"> 1592 <div class="widget dark-border"> 1593 <div class="legend journal-contentLinkColor">Information</div> 1594 <div class="content" id="1307"> 1595 <p>The natural and anthropogenic climate drivers that impact Earthâs radiation balance, influencing climate states and <q>forcing</q> climate change are termed <q>climate forcing</q> agents. Globally representative forcing estimates are needed to drive Earth system models to simulate past and project future climate states. The Coupled Model Intercomparison Project (CMIP) <a href="https://wcrp-cmip.org/cmip7-task-teams/forcings/"target="_blank">Forcing Task Team</a> aims to identify, develop, document, and deliver forcings for next-generation models participating in the seventh phase of CMIP (CMIP7). This next phase is likely to be a core contribution to the IPCC seventh assessment cycle (AR7). The special issue welcomes papers documenting forcing data development and evaluation, along with those describing CMIP7 forcing characteristics (in contrast to previous versions). We also invite papers that quantify and assess uncertainties in the spatial and temporal forcing distributions and the influence of forcing on the evolution of climate states across Earth system model configurations.</p> 1596 </div> 1597 <div class="row"> 1598 <div class="col-auto"> 1599 <a href="#" class="show-hide triangle" data-hide="#info-chronologically-content-1307" 1600 data-show="#info-chronologically-link-1307">Hide</a> 1601 </div> 1602 <div class="col text-right"> 1603 <a class="si-mobile-native-share" href="#" data-title="Coupled Model Intercomparison Project Phase 7 (CMIP7) forcings and inputs – development, documentation, and evaluation" data-url="https://essd.copernicus.org/articles/special_issue365_1307.html" data-id="1307" style="display: none;"> 1604 <i class="fas fa-lg fa-share-alt"></i> 1605 </a> 1606 <a class="desktop-share" href="#" data-title="Coupled Model Intercomparison Project Phase 7 (CMIP7) forcings and inputs – development, documentation, and evaluation" data-url="https://essd.copernicus.org/articles/special_issue365_1307.html" data-id="1307" title="Copy to clipboard"> 1607 <i class="fas fa-lg fa-share-alt"></i> 1608 </a> 1609 </div> 1610 </div> 1611 </div> 1612 </div> 1613 </div> 1614 <h2 class="group-special-issue">2023</h2> 1615 <div class="grid-container grid-parent special-issue triangle_special_issues">
1616 <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> 1617 <a href="https://essd.copernicus.org/articles/special_issue365_1284.html">Model Intercomparison and Improvement Projects (MIIPs) for the polar regions and beyond (GMD/ESSD inter-journal SI)</a> 1618 (GMD/ESSD inter-journal SI) 1619 </div> 1620 <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 1621 25 Sep 2023–indefinite | Gunilla Svensson (Stockholm University, Sweden), Matthew D. Shupe (University of Colorado Colorado Springs, United States), Felix Pithan (Alfred Wegener Institute for Polar and Marine Research, Germany), and Ken Mankoff (Goddard Institute for Space Studies, United States) | 1622 <a href="javascript:void(0);" class="info-link show-hide" id="info-chronologically-link-1284" data-show="#info-chronologically-content-1284" data-hide="#info-chronologically-link-1284">Information</a> 1623 </div> 1624 <div class="j-widget__max short_summary" id="info-chronologically-content-1284" style="display: none"> 1625 <div class="widget dark-border"> 1626 <div class="legend journal-contentLinkColor">Information</div> 1627 <div class="content" id="1284"> 1628 <p>For this SI we welcome manuscripts on activities such as MIIPs â Model Intercomparison and Improvement Projects that target long-standing issues in the representation of small-scale processes in numerical weather prediction and climate models. The initiatives may have been taken during the 10-year Polar Prediction Project (PPP) that finished at the end of 2022 or during the Polar Coupled Analysis and Prediction for Services (PCAPS
1628) both part of the WMO World Weather Research Program. These programs suggest an emphasis on processes that are especially important for the polar regions, but contributions that are relevant and important for model performance in other regions of the world are also welcome. Specific targets are the representation of stably stratified boundary layers, mixed-phase clouds and atmospheric coupling with snow and or ice-covered surfaces, sea-ice, ocean mixing etc.</p> 1629<p>The intention of this SI is to publish results from MIIPs that establish new and improved workflows to facilitate a more efficient path to improved process representation. This includes research-grade observations that are packaged in an easy-to-use format which combine high-frequency observations of the surface and the atmosphere above to be able to directly compare with the parameterizations used in models using time-step data. The Merged Data File (MDF) format that is defined for both observations and model output come with a series of tools that is transferable between models and observational data collections for both file production and analysis. The SI especially welcome contributions that build on, or further develop the MDF concept including new variables, types of data, sites or new analysis tools such as process-oriented diagnostics or insights in models using the targeted files.</p> 1630 </div> 1631 <div class="row"> 1632 <div class="col-auto"> 1633 <a href="#" class="show-hide triangle" data-hide="#info-chronologically-content-1284" 1634 data-show="#info-chronologically-link-1284">Hide</a> 1635 </div> 1636 <div class="col text-right"> 1637 <a class="si-mobile-native-share" href="#" data-title="Model Intercomparison and Improvement Projects (MIIPs) for the polar regions and beyond (GMD/ESSD inter-journal SI)" data-url="https://essd.copernicus.org/articles/special_issue365_1284.html" data-id="1284" style="display: none;"> 1638 <i class="fas fa-lg fa-share-alt"></i> 1639 </a> 1640 <a class="desktop-share" href="#" data-title="Model Intercomparison and Improvement Projects (MIIPs) for the polar regions and beyond (GMD/ESSD inter-journal SI)" data-url="https://essd.copernicus.org/articles/special_issue365_1284.html" data-id="1284" title="Copy to clipboard"> 1641 <i class="fas fa-lg fa-share-alt"></i> 1642 </a> 1643 </div> 1644 </div> 1645 </div> 1646 </div> 1647 </div> 1648 <h2 class="group-special-issue">2013</h2> 1649 <div class="grid-container grid-parent special-issue triangle_special_issues"> 1650 <div class="grid-100 tablet-grid-100 mobile-grid-100 title triangle-content"> 1651 <a href="https://essd.copernicus.org/articles/special_issue25_968.html">Oldest Ice: finding and interpreting climate proxies in ice older than 700 000 years</a> 1652 (TC/CP/ESSD inter-journal SI) 1653 </div> 1654 <div class="grid-100 tablet-grid-100 mobile-grid-100 date"> 1655 01 Jan 2013–31 Dec 2027 | ESSD editors | Coordinators: Thomas Blunier (University of Copenhagen, Denmark) and Reinhard Drews (University of Tübingen, Germany) | 1656 <a href="javascript:void(0);" class="info-link show-hide" id="info-chronologically-link-968" data-show="#info-chronologically-content-968" data-hide="#info-chronologically-link-968">Information</a> 1657 </div> 1658 <div class="j-widget__max short_summary" id="info-chronologically-content-968" style="display: none"> 1659 <div class="widget dark-border"> 1660 <div class="legend journal-contentLinkColor">Information</div> 1661 <div class="content" id="968"> 1662 <p>The glacialâinterglacial cyclicity of the climate system varied in the past, most notably during the transition from a 40 ka to a 100 ka world in the mid-Pleistocene. Gases trapped in Antarctic ice are the most direct access available to investigate the composition of the paleo-atmosphere of that age and processes related to climate variability. The International Partnerships in Ice Core Sciences (IPICS) Oldest Ice endeavour aims at obtaining an undisturbed ice-core record older than 1 Ma. In addition to ice cores, time slices of paleo-records, available, for example, in Antarctic blue-ice fields, provide further valuable information, which complements continuous time series based on ice cores. This special issue will assemble contributions dedicated to the preparatory phase of this global effort to obtain ice samples and time series older than 700 000 years. This includes a consideration of glaciogical and geophysical settings which allow the presence of old ice, results from pre-site surveys and modelling studies, aspects of ice-core and other sampling techniques and analyses, and requirements for drilling and core handling.</p> 1663 </div> 1664 <div class="row"> 1665 <div class="col-auto"> 1666 <a href="#" class="show-hide triangle" data-hide="#info-chronologically-content-968" 1667 data-show="#info-chronologically-link-968">Hide</a> 1668 </div> 1669 <div class="col text-right"> 1670 <a class="si-mobile-native-share" href="#" data-title="Oldest Ice: finding and interpreting climate proxies in ice older than 700 000 years" data-url="https://essd.copernicus.org/articles/special_issue25_968.html" data-id="968" style="display: none;"> 1671 <i class="fas fa-lg fa-share-alt"></i> 1672 </a> 1673 <a class="desktop-share" href="#" data-title="Oldest Ice: finding and interpreting climate proxies in ice older than 700 000 years" data-url="https://essd.copernicus.org/articles/special_issue25_968.html" data-id="968" title="Copy to clipboard"> 1674 <i class="fas fa-lg fa-share-alt"></i> 1675 </a> 1676 </div> 1677 </div> 1678 </div> 1679 </div> 1680 </div> 1681 </div> 1682 </div>
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Line numbers count LF bytes from the start of the resource, as the search results do. Vendor segments are library code the classifier recognised; they are stored but not indexed. Bytes are shown as Latin1 characters, one per byte.