{"id":1645,"date":"2023-11-28T17:31:21","date_gmt":"2023-11-28T16:31:21","guid":{"rendered":"https:\/\/www.eovision.at\/esa-schoolatlas\/?page_id=1645"},"modified":"2025-03-19T10:37:26","modified_gmt":"2025-03-19T09:37:26","slug":"cryosphere","status":"publish","type":"page","link":"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/de\/cryosphere\/","title":{"rendered":"Cryosphere"},"content":{"rendered":"<h2>Cryosphere<\/h2>\n<p><img decoding=\"async\" style=\"width: 25%; height: 25%; padding: 0px 15px 5px 0px;\" src=\"https:\/\/esa-schoolatlas.eu\/wp-content\/gismaps_maps\/Images\/s_chapters_cry.jpg\" align=\"left\"\/><br>\nThe cryosphere (from Greek <em>kryos<\/em> for cold) comprises all frozen parts of Earth. These are to a large part the frozen water bodies of the mountain glaciers, polar ice caps and sea ice are part of the hydrosphere. Additionally, the permafrost regions, frozen parts of the <a class=\"glossaryLink\"  title=\"Glossary: soil\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;soil&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Biologically active, porous medium that covers the uppermost layer of Earth&lsquo;s crust.&lt;\/div&gt;\"  href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/de\/glossary\/soil\/\"  target=\"_blank\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>soil<\/a>, are part of the cryosphere.<\/p>\n<p>In total Earth&#x2019;s cryosphere covers about 10 percent of the Earth surface. Due to the <a class=\"glossaryLink\" title=\"Glossary: climate change\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;climate change&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Long-term shifts in temperatures and weather patterns due to natural or man-made effects.&lt;\/div&gt;\" href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/de\/glossary\/climate-change\/\" target=\"_blank\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">climate change<\/a> with rising global temperatures the cryosphere is shrinking.<\/p>\n<h3>Select your Case Study:<\/h3>\n<table>\n<tbody>\n<tr style=\"background-color: #777777;\">\n<th style=\"border: 0; padding-left: 10px;\" colspan=\"2\"><strong>Glaciers, the frozen rivers<\/strong><\/th>\n<\/tr>\n<tr>\n<td><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\" sizes=\"(max-width: 100px) 100vw, 100px\" srcset=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/uploads\/sites\/7\/2023\/11\/cli04_1_columbiaglacier_icon.jpg 100w, https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/uploads\/sites\/7\/2023\/11\/cli04_1_columbiaglacier_icon-80x80.jpg 80w\" 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><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\" sizes=\"(max-width: 100px) 100vw, 100px\" srcset=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/uploads\/sites\/7\/2023\/11\/cli04_2_aletsch_icon.jpg 100w, https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/uploads\/sites\/7\/2023\/11\/cli04_2_aletsch_icon-80x80.jpg 80w\" 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><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\" sizes=\"(max-width: 100px) 100vw, 100px\" srcset=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/uploads\/sites\/7\/2023\/11\/cli04_3_kilimanjaro_icon.jpg 100w, https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/uploads\/sites\/7\/2023\/11\/cli04_3_kilimanjaro_icon-80x80.jpg 80w\" 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 <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> zone, and they are shrinking.<\/td>\n<\/tr>\n<tr style=\"background-color: #777777;\">\n<th style=\"border: 0; padding-left: 10px;\" colspan=\"2\"><strong>The frozen polar caps of Earth<\/strong><\/th>\n<\/tr>\n<tr>\n<td><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/cryosphere\/arctic-sea-ice\/\"><img loading=\"lazy\" decoding=\"async\" class=\"zoom-effect alignleft\" src=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/cry01_1_arctic-ice_icon.jpg\" sizes=\"(max-width: 100px) 100vw, 100px\" srcset=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/cry01_1_arctic-ice_icon.jpg 100w, https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/cry01_1_arctic-ice_icon.jpg 80w\" alt=\"\" width=\"100\" height=\"100\"\/><\/a><\/td>\n<td><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/cryosphere\/arctic-sea-ice\/\">Arctic Sea Ice<\/a><br>\nWhile the sea ice coverage around the North Pole undergoes large seasonal changes, it is shrinking due to climate change.<\/td>\n<\/tr>\n<tr>\n<td><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/cryosphere\/greenland\/\"><img loading=\"lazy\" class=\"zoom-effect alignleft\" sizes=\"(max-width: 100px) 100vw, 100px\" srcset=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/cry02_1_greenland_icon.jpg 100w, https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/cry02_1_greenland_icon-80x80.jpg 80w\" alt=\"\" width=\"100\" height=\"100\"\/><\/a><\/td>\n<td><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/cryosphere\/greenland\/\">Jakobshavn Isbrae<\/a>, Greenland (Denmark)<br>\nThe shrinking of the Greenland ice sheet, the second largest ice body on Earth, contributes to the global sea level rise.<\/td>\n<\/tr>\n<tr>\n<td><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/cryosphere\/antarctica\/\"><img loading=\"lazy\" decoding=\"async\" class=\"zoom-effect alignleft\" src=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/cry03_1_antarctica_icon.jpg\" sizes=\"(max-width: 100px) 100vw, 100px\" srcset=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/cry03_1_antarctica_icon.jpg 100w, https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/cry03_1_antarctica_icon.jpg 80w\" alt=\"\" width=\"100\" height=\"100\"\/><\/a><\/td>\n<td><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/cryosphere\/antarctica\/\">Ice of Antarctica<\/a><br>\nThe antarctic ice bodies are the largest on Earth.<\/td>\n<\/tr>\n<tr>\n<td><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/cryosphere\/iceberg-a23a\/\"><img loading=\"lazy\" decoding=\"async\" class=\"zoom-effect alignleft\" src=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/cry04_1_iceberg-a23a_icon.jpg\" sizes=\"(max-width: 100px) 100vw, 100px\" srcset=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/cry04_1_iceberg-a23a_icon.jpg 100w, https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/cry04_1_iceberg-a23a_icon-80x80.jpg 80w\" alt=\"\" width=\"100\" height=\"100\"\/><\/a><\/td>\n<td><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/cryosphere\/iceberg-a23a\/\">Iceberg A23a<\/a>, Antarctic Ocean<br>\nLarge icebergs calving from the ice shelves around the Antarctic ice sheet are an important factor in the proceeding ice loss.<\/td>\n<\/tr>\n<tr style=\"background-color: #777777;\">\n<th style=\"border: 0; padding-left: 10px;\" colspan=\"2\"><strong>Permafrost regions<\/strong><\/th>\n<\/tr>\n<tr>\n<td><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/cryosphere\/batagaika\/\"><img loading=\"lazy\" decoding=\"async\" class=\"zoom-effect alignleft\" src=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/cry05_1_batagaika_icon.jpg\" sizes=\"(max-width: 100px) 100vw, 100px\" srcset=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/cry05_1_batagaika_icon.jpg 100w, https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/cry05_1_batagaika_icon.jpg 80w\" alt=\"\" width=\"100\" height=\"100\"\/><\/a><\/td>\n<td><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/cryosphere\/batagaika\/\">Batagaika Crater<\/a><br>\nThawing permafrost in Siberia due to global warming leads to enhanced <a class=\"glossaryLink\" title=\"Glossary: erosion\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;erosion&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Surface processes (e.g. water flow or wind) removing soil, rock, or dissolved material from the Earth&#x2018;s crust and transporting it to another location where it is deposited.&lt;\/div&gt;\" href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/de\/glossary\/erosion\/\" target=\"_blank\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">erosion<\/a> of the soil.<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p><!-- \/wp:paragraph --><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Cryosphere The cryosphere (from Greek kryos for cold) comprises all frozen parts of Earth. These are to a large part the frozen water bodies of the mountain glaciers, polar ice caps and sea ice are part of the hydrosphere. Additionally, the permafrost regions, frozen parts of the soil, are part of the cryosphere. In total [&#x2026;]<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":1,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-1645","page","type-page","status-publish","hentry"],"translation":{"provider":"WPGlobus","version":"3.0.0","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":false,"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>Cryosphere - 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\/cryosphere\/\" \/>\n<meta property=\"og:locale\" content=\"de_DE\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Cryosphere - 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