{"id":20888,"date":"2021-01-13T14:40:34","date_gmt":"2021-01-13T13:40:34","guid":{"rendered":"https:\/\/www.ig.cas.cz\/?page_id=20888"},"modified":"2021-01-13T14:40:50","modified_gmt":"2021-01-13T13:40:50","slug":"permafrost-in-central-europe","status":"publish","type":"page","link":"https:\/\/www.ig.cas.cz\/en\/permafrost-in-central-europe\/","title":{"rendered":"Distribution, Thickness and Evolution of Permafrost in Central Europe in Late Quaternary"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;4.6.0&#8243; _module_preset=&#8221;default&#8221;][et_pb_row column_structure=&#8221;3_5,2_5&#8243; _builder_version=&#8221;4.6.0&#8243; _module_preset=&#8221;default&#8221;][et_pb_column type=&#8221;3_5&#8243; _builder_version=&#8221;4.6.0&#8243; _module_preset=&#8221;default&#8221;][et_pb_text _builder_version=&#8221;4.6.0&#8243; _module_preset=&#8221;default&#8221;]<\/p>\n<p><strong>Distribution, Thickness and Evolution of Permafrost in Central Europe in Late Quaternary<\/strong><\/p>\n<p>The project deals with topical palaeo-geographical theme of Late Quaternary permafrost changes in non-alpine Central Europe. We intend to answer still-discussed and largely unresolved problems of what were the glacier\u2013permafrost interactions around the southern limit of the Scandinavian ice sheet, how permafrost extent and thickness responded to climate fluctuations during stadials and interstadials and at the Pleistocene\u2013\u2013Holocene transition, or how it degraded during the Holocene. We address these issues through an innovative approach that combines mathematical modelling of permafrost dynamics using palaeo-temperatures obtained from borehole temperature logs and proxy records with empirical reconstructions based on distribution and chronology of relict permafrost-related landforms and sedimentary structures. The project outputs will help to better understand the palaeo-environmental evolution of mid-latitude areas where permafrost has played an important role in the past as well as to assess the changes in present-day permafrost regions and to forecast their future dynamics.<\/p>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;2_5&#8243; _builder_version=&#8221;4.6.0&#8243; _module_preset=&#8221;default&#8221;][et_pb_text _builder_version=&#8221;4.6.0&#8243; _module_preset=&#8221;default&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<\/p>\n<p>Team:<\/p>\n<p><strong><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/jan-safanda\/\">Dr. Jan \u0160afanda<\/a>, principal researcher<\/strong><br \/><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/petr-dedecek\/\">Petr D\u011bde\u010dek<\/a>, researcher<br \/><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/tomas-uxa\/\">Dr. Tom\u00e1\u0161 Uxa<\/a>, researcher<br \/><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/vladimir-cermak\/\">Dr. Vladim\u00edr \u010cerm\u00e1k<\/a>, researcher<\/p>\n<p>Project duration: 2021 &#8211; 2023<\/p>\n<p>[\/et_pb_text][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/permafrost-4463510_1280.jpg&#8221; title_text=&#8221;Permafrost 4463510 1280&#8243; _builder_version=&#8221;4.6.0&#8243; _module_preset=&#8221;default&#8221;][\/et_pb_image][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Distribution, Thickness and Evolution of Permafrost in Central Europe in Late Quaternary The project deals with topical palaeo-geographical theme of Late Quaternary permafrost changes in non-alpine Central Europe. We intend to answer still-discussed and largely unresolved problems of what were the glacier\u2013permafrost interactions around the southern limit of the Scandinavian ice sheet, how permafrost extent [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":""},"categories":[],"tags":[],"class_list":["post-20888","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v25.9 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Distribution, Thickness and Evolution of Permafrost in Central Europe in Late Quaternary - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.ig.cas.cz\/en\/permafrost-in-central-europe\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Distribution, Thickness and Evolution of Permafrost in Central Europe in Late Quaternary - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.\" \/>\n<meta property=\"og:description\" content=\"Distribution, Thickness and Evolution of Permafrost in Central Europe in Late Quaternary The project deals with topical palaeo-geographical theme of Late Quaternary permafrost changes in non-alpine Central Europe. We intend to answer still-discussed and largely unresolved problems of what were the glacier\u2013permafrost interactions around the southern limit of the Scandinavian ice sheet, how permafrost extent [&hellip;]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/www.ig.cas.cz\/en\/permafrost-in-central-europe\/\" \/>\n<meta property=\"og:site_name\" content=\"Dom\u016f\" \/>\n<meta property=\"article:publisher\" content=\"https:\/\/www.facebook.com\/GFUAVCR\/\" \/>\n<meta property=\"article:modified_time\" content=\"2021-01-13T13:40:50+00:00\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data1\" content=\"1 minute\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\/\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"https:\/\/www.ig.cas.cz\/en\/permafrost-in-central-europe\/\",\"url\":\"https:\/\/www.ig.cas.cz\/en\/permafrost-in-central-europe\/\",\"name\":\"Distribution, Thickness and Evolution of Permafrost in Central Europe in Late Quaternary - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.\",\"isPartOf\":{\"@id\":\"https:\/\/www.ig.cas.cz\/#website\"},\"datePublished\":\"2021-01-13T13:40:34+00:00\",\"dateModified\":\"2021-01-13T13:40:50+00:00\",\"breadcrumb\":{\"@id\":\"https:\/\/www.ig.cas.cz\/en\/permafrost-in-central-europe\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\/\/www.ig.cas.cz\/en\/permafrost-in-central-europe\/\"]}]},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\/\/www.ig.cas.cz\/en\/permafrost-in-central-europe\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Dom\u016f\",\"item\":\"https:\/\/www.ig.cas.cz\/en\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"Distribution, Thickness and Evolution of Permafrost in Central Europe in Late Quaternary\"}]},{\"@type\":\"WebSite\",\"@id\":\"https:\/\/www.ig.cas.cz\/#website\",\"url\":\"https:\/\/www.ig.cas.cz\/\",\"name\":\"Dom\u016f\",\"description\":\"Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.\",\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"https:\/\/www.ig.cas.cz\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"en-US\"}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"Distribution, Thickness and Evolution of Permafrost in Central Europe in Late Quaternary - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/www.ig.cas.cz\/en\/permafrost-in-central-europe\/","og_locale":"en_US","og_type":"article","og_title":"Distribution, Thickness and Evolution of Permafrost in Central Europe in Late Quaternary - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.","og_description":"Distribution, Thickness and Evolution of Permafrost in Central Europe in Late Quaternary The project deals with topical palaeo-geographical theme of Late Quaternary permafrost changes in non-alpine Central Europe. We intend to answer still-discussed and largely unresolved problems of what were the glacier\u2013permafrost interactions around the southern limit of the Scandinavian ice sheet, how permafrost extent [&hellip;]","og_url":"https:\/\/www.ig.cas.cz\/en\/permafrost-in-central-europe\/","og_site_name":"Dom\u016f","article_publisher":"https:\/\/www.facebook.com\/GFUAVCR\/","article_modified_time":"2021-01-13T13:40:50+00:00","twitter_card":"summary_large_image","twitter_misc":{"Est. reading time":"1 minute"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"WebPage","@id":"https:\/\/www.ig.cas.cz\/en\/permafrost-in-central-europe\/","url":"https:\/\/www.ig.cas.cz\/en\/permafrost-in-central-europe\/","name":"Distribution, Thickness and Evolution of Permafrost in Central Europe in Late Quaternary - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.","isPartOf":{"@id":"https:\/\/www.ig.cas.cz\/#website"},"datePublished":"2021-01-13T13:40:34+00:00","dateModified":"2021-01-13T13:40:50+00:00","breadcrumb":{"@id":"https:\/\/www.ig.cas.cz\/en\/permafrost-in-central-europe\/#breadcrumb"},"inLanguage":"en-US","potentialAction":[{"@type":"ReadAction","target":["https:\/\/www.ig.cas.cz\/en\/permafrost-in-central-europe\/"]}]},{"@type":"BreadcrumbList","@id":"https:\/\/www.ig.cas.cz\/en\/permafrost-in-central-europe\/#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Dom\u016f","item":"https:\/\/www.ig.cas.cz\/en\/"},{"@type":"ListItem","position":2,"name":"Distribution, Thickness and Evolution of Permafrost in Central Europe in Late Quaternary"}]},{"@type":"WebSite","@id":"https:\/\/www.ig.cas.cz\/#website","url":"https:\/\/www.ig.cas.cz\/","name":"Dom\u016f","description":"Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.","potentialAction":[{"@type":"SearchAction","target":{"@type":"EntryPoint","urlTemplate":"https:\/\/www.ig.cas.cz\/?s={search_term_string}"},"query-input":{"@type":"PropertyValueSpecification","valueRequired":true,"valueName":"search_term_string"}}],"inLanguage":"en-US"}]}},"_links":{"self":[{"href":"https:\/\/www.ig.cas.cz\/en\/wp-json\/wp\/v2\/pages\/20888","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.ig.cas.cz\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.ig.cas.cz\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.ig.cas.cz\/en\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.ig.cas.cz\/en\/wp-json\/wp\/v2\/comments?post=20888"}],"version-history":[{"count":0,"href":"https:\/\/www.ig.cas.cz\/en\/wp-json\/wp\/v2\/pages\/20888\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.ig.cas.cz\/en\/wp-json\/wp\/v2\/media?parent=20888"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.ig.cas.cz\/en\/wp-json\/wp\/v2\/categories?post=20888"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.ig.cas.cz\/en\/wp-json\/wp\/v2\/tags?post=20888"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}