{"id":68,"date":"2018-01-19T10:50:40","date_gmt":"2018-01-19T10:50:40","guid":{"rendered":"http:\/\/geo2.unibe.ch\/wp\/?p=68"},"modified":"2018-01-30T16:53:47","modified_gmt":"2018-01-30T16:53:47","slug":"greetings-from-antarctica-expedition","status":"publish","type":"post","link":"https:\/\/www.geology.unibe.ch\/index.php\/2018\/01\/19\/greetings-from-antarctica-expedition\/","title":{"rendered":"Greetings from Antarctica Expedition"},"content":{"rendered":"<h1>DEAIS: Deglaciation history of the Eastern Antarctic Ice Sheet<\/h1>\n<div id=\"attachment_73\" style=\"width: 310px\" class=\"wp-caption alignright\"><img aria-describedby=\"caption-attachment-73\" loading=\"lazy\" src=\"http:\/\/geo2.unibe.ch\/wp\/wp-content\/uploads\/2018\/01\/Antarctica02_NakiAkcar-300x182.jpg\" alt=\"Naki Ak\u00e7ar and Serdar Ye\u015filyurt in Antarctica\" class=\"wp-image-73 size-medium\" width=\"300\" height=\"182\" srcset=\"https:\/\/www.geology.unibe.ch\/wp-content\/uploads\/2018\/01\/Antarctica02_NakiAkcar-300x182.jpg 300w, https:\/\/www.geology.unibe.ch\/wp-content\/uploads\/2018\/01\/Antarctica02_NakiAkcar-768x466.jpg 768w, https:\/\/www.geology.unibe.ch\/wp-content\/uploads\/2018\/01\/Antarctica02_NakiAkcar.jpg 800w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><p id=\"caption-attachment-73\" class=\"wp-caption-text\">Naki Ak\u00e7ar and Serdar Ye\u015filyurt in Antarctica<\/p><\/div>\n<p>Our researchers <a href=\"http:\/\/www.geo.unibe.ch\/about_us\/the_institute\/personen\/pd_dr_akar_naki\/index_eng.html\" target=\"_blank\" rel=\"noopener\">Naki Ak\u00e7ar<\/a> and <a href=\"http:\/\/www.geo2.unibe.ch\/personen\/team_ifg_detail_e.php?PID=89072932\" target=\"_blank\" rel=\"noopener\">Serdar Ye\u015filyurt<\/a> started their research expedition in Antarctica. They just arrived and sent their first impressions.<\/p>\n<p>The recent and rapid decay of some parts of the Antarctic Ice Sheet has provoked questions about the rate of this environmental change and on future global sea level rise induced by this change. The existing data on the response of the Antarctic Ice Sheet to this change is mainly limited to satellite measurements with short time scales, i.e. a few decades or less.<\/p>\n<div id=\"attachment_71\" style=\"width: 760px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/www.polarfoundation.org\/news_press\/news\/waking_the_princess\"><img aria-describedby=\"caption-attachment-71\" loading=\"lazy\" src=\"http:\/\/geo2.unibe.ch\/wp\/wp-content\/uploads\/2018\/01\/PEA2-\u00a9-International-Polar-Foundation-1024x602.jpg\" alt=\"Princess Elisabeth Antarctic Research Station\" class=\"wp-image-71 size-large\" width=\"750\" height=\"441\" srcset=\"https:\/\/www.geology.unibe.ch\/wp-content\/uploads\/2018\/01\/PEA2-\u00a9-International-Polar-Foundation-1024x602.jpg 1024w, https:\/\/www.geology.unibe.ch\/wp-content\/uploads\/2018\/01\/PEA2-\u00a9-International-Polar-Foundation-300x176.jpg 300w, https:\/\/www.geology.unibe.ch\/wp-content\/uploads\/2018\/01\/PEA2-\u00a9-International-Polar-Foundation-768x452.jpg 768w, https:\/\/www.geology.unibe.ch\/wp-content\/uploads\/2018\/01\/PEA2-\u00a9-International-Polar-Foundation.jpg 1651w\" sizes=\"(max-width: 750px) 100vw, 750px\" \/><\/a><p id=\"caption-attachment-71\" class=\"wp-caption-text\">Princess Elisabeth Antarctic Research Station PEA2 (c) International Polar Foundation 1<\/p><\/div>\n<p>The understanding of the long-term behaviour of the Antarctic Ice Sheet requires input data from paleo studies over longer time periods, so as to assess its future behaviour and consequent future sea-level rise. For instance, dramatic surface lowering of East Antarctic Ice Sheet (EAIS) during the last million years have been recently reported in several publications. However, the spatial distribution of this unloading and subsequent isostatic rebound remain unexplored.<\/p>\n<p>In this study, we will decipher the pace of deglaciation of the EAIS in the S\u00f8r Rondane Mountains in the Queen Maud Land. To do this, we will participate the BELARE 2017-2018 Expedition and be based at the Belgian Princess Elisabeth Station (PEA). We will focus on the Nunatacks around the PEA: Mount Wider\u00f8e, Mount Nils Larsen and Perlabandet in the western S\u00f8r Rondane Mountains, which are located within 50 km flight distance.&nbsp; We will collect and analyse rock samples from the glacial deposits and glacially abraded bedrock in these target areas. This expedition is financed by the Polar Research Center at the Istanbul Technical University (Turkey).<\/p>\n<div id=\"attachment_79\" style=\"width: 810px\" class=\"wp-caption alignnone\"><img aria-describedby=\"caption-attachment-79\" loading=\"lazy\" src=\"http:\/\/geo2.unibe.ch\/wp\/wp-content\/uploads\/2018\/01\/Antarctica03_NakiAkcar.jpeg\" alt=\"Antarctica\" class=\"size-full wp-image-79\" width=\"800\" height=\"600\" srcset=\"https:\/\/www.geology.unibe.ch\/wp-content\/uploads\/2018\/01\/Antarctica03_NakiAkcar.jpeg 800w, https:\/\/www.geology.unibe.ch\/wp-content\/uploads\/2018\/01\/Antarctica03_NakiAkcar-300x225.jpeg 300w, https:\/\/www.geology.unibe.ch\/wp-content\/uploads\/2018\/01\/Antarctica03_NakiAkcar-768x576.jpeg 768w\" sizes=\"(max-width: 800px) 100vw, 800px\" \/><p id=\"caption-attachment-79\" class=\"wp-caption-text\">Antarctica<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>DEAIS: Deglaciation history of the Eastern Antarctic Ice Sheet Our researchers Naki Ak\u00e7ar and Serdar Ye\u015filyurt started their research expedition in Antarctica. They just arrived and sent their first impressions. The recent and rapid decay<a class=\"moretag\" href=\"https:\/\/www.geology.unibe.ch\/index.php\/2018\/01\/19\/greetings-from-antarctica-expedition\/\"> Read more&hellip;<\/a><\/p>\n","protected":false},"author":2,"featured_media":69,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"ngg_post_thumbnail":0},"categories":[5],"tags":[9,7],"_links":{"self":[{"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/posts\/68"}],"collection":[{"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/comments?post=68"}],"version-history":[{"count":15,"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/posts\/68\/revisions"}],"predecessor-version":[{"id":198,"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/posts\/68\/revisions\/198"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/media\/69"}],"wp:attachment":[{"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/media?parent=68"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/categories?post=68"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/tags?post=68"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}