{"id":1970,"date":"2024-05-27T16:49:36","date_gmt":"2024-05-27T14:49:36","guid":{"rendered":"https:\/\/www.eovision.at\/esa-schoolatlas\/?page_id=1970"},"modified":"2025-03-19T10:51:16","modified_gmt":"2025-03-19T09:51:16","slug":"climate-change-columbia-glacier","status":"publish","type":"page","link":"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/de\/system-erde\/climate-change-columbia-glacier\/","title":{"rendered":"Klima und Klimawandel"},"content":{"rendered":"<h2>Theme: Changes in the ice bodies of the cryosphere<\/h2>\n<p>Consequences of the changing <a class=\"glossaryLink\" title=\"Glossary: climate\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;climate&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Average weather conditions for a particular location over a long period of time, e.g. 30 years.&lt;\/div&gt;\" href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/de\/glossary\/climate\/\" target=\"_blank\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">climate<\/a> are especially clearly visible in the change of the ice bodies on Earth. These changes affect the area extent of the ice as well as the ice thickness.<\/p>\n<h2>Select your Case Study:<\/h2>\n<table>\n<tbody>\n<tr style=\"background-color: #777777;\">\n<th colspan=\"2\" style=\"border:0; padding-left:10px;\"><strong>Retreating glaciers<\/strong><\/th>\n<\/tr>\n<tr>\n<td style=\"width: 120px;\"><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/system-erde\/columbia-glacier\/\"><img decoding=\"async\" class=\"zoom-effect alignleft\" src=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/uploads\/sites\/7\/2023\/11\/cli04_1_columbiaglacier_icon.jpg\" alt=\"\" width=\"100\" height=\"100\"\/><\/a><\/td>\n<td><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/system-erde\/columbia-glacier\/\">Columbia Glacier<\/a>, U.S.A.<br>\nHigher temperatures and the rising sea level lead to a rapid decay of the Columbia Glacier.<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 120px;\"><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/system-erde\/aletsch-glacier\/\"><img decoding=\"async\" class=\"zoom-effect alignleft\" src=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/uploads\/sites\/7\/2023\/11\/cli04_2_aletsch_icon.jpg\" alt=\"\" width=\"100\" height=\"100\"\/><\/a><\/td>\n<td><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/system-erde\/aletsch-glacier\/\">Aletsch Glacier<\/a>, Switzerland<br>\nThe largest glacier of the Alps is an example of the retreat of alpine glaciers.<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 120px;\"><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/system-erde\/kilimanjaro\/\"><img decoding=\"async\" class=\"zoom-effect alignleft\" src=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/uploads\/sites\/7\/2023\/11\/cli04_3_kilimanjaro_icon.jpg\" alt=\"\" width=\"100\" height=\"100\"\/><\/a><\/td>\n<td><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/system-erde\/kilimanjaro\/\">Kilimanjaro Glacier<\/a>, Tanzania<br>\nThere are not many glaciers in the tropical climate zone, and they are shrinking.<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n","protected":false},"excerpt":{"rendered":"<p>Theme: Changes in the ice bodies of the cryosphere Consequences of the changing climate are especially clearly visible in the change of the ice bodies on Earth. These changes affect the area extent of the ice as well as the ice thickness. Select your Case Study: Retreating glaciers Columbia Glacier, U.S.A. Higher temperatures and the [&#x2026;]<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":103,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-1970","page","type-page","status-publish","hentry"],"translation":{"provider":"WPGlobus","version":"3.0.2","language":"de","enabled_languages":["en","es","de","fr","it"],"languages":{"en":{"title":true,"content":true,"excerpt":false},"es":{"title":false,"content":false,"excerpt":false},"de":{"title":true,"content":false,"excerpt":false},"fr":{"title":false,"content":false,"excerpt":false},"it":{"title":false,"content":false,"excerpt":false}}},"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v26.3 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Klima und Klimawandel - ESA Schoolatlas<\/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:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/de\/system-erde\/climate-change-columbia-glacier\/\" \/>\n<meta property=\"og:locale\" content=\"de_DE\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Klima und Klimawandel - 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