{"id":96,"date":"2021-11-04T14:02:26","date_gmt":"2021-11-04T13:02:26","guid":{"rendered":"https:\/\/www.eovision.at\/esa-schoolatlas\/?page_id=96"},"modified":"2025-03-12T13:54:31","modified_gmt":"2025-03-12T12:54:31","slug":"atmosphere","status":"publish","type":"page","link":"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/it\/atmosphere\/","title":{"rendered":"Atmosphere"},"content":{"rendered":"<h2>Atmosphere<\/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_atm.jpg\" align=\"left\"\/><br>\nThe gaseous component of the Earth system has a total mass of more than 5000 billion tons. Nevertheless the atmosphere (from Greek <em>atmos<\/em> for vapour) is only a relatively thin layer &#x2013; all relevant weather phenomena take place in the troposphere, which extends to an altitude of 12 to 15 kilometers only.<\/p>\n<p>Almost nothing has remained from the primary atmosphere that formed together with the Earth some 4500 million years ago. <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\/it\/glossary\/erosion\/\" target=\"_blank\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">Erosion<\/a> and, later, life have changed its composition to what we breathe now &#x2013; a mixture of 78% nitrogen, 21% oxygen and a number of other constituents, among which <a class=\"glossaryLink\" title=\"Glossary: water vapour\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;water vapour&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Water in its gaseous state; in the atmosphere the most important factor of the natural greenhouse effect.&lt;\/div&gt;\" href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/it\/glossary\/water-vapour\/\" target=\"_blank\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">water vapour<\/a> and carbon dioxide are most important.<\/p>\n<p>Life on Earth needs the atmosphere not only for breathing. It is an important shield against cosmic <a class=\"glossaryLink\" title=\"Glossary: radiation\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;radiation&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Energy transfer in the form of electromagnetic waves or particles that release energy when absorbed by an object.&lt;\/div&gt;\" href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/it\/glossary\/radiation\/\" target=\"_blank\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">radiation<\/a>, too.<\/p>\n<p>&#xA0;<\/p>\n<h3>Select your Case Study:<\/h3>\n<table>\n<tbody>\n<tr style=\"background-color: #777777;\">\n<th colspan=\"2\" style=\"border:0; padding-left:10px;\"><strong>Trace Gases<\/strong><\/th>\n<\/tr>\n<tr>\n<td style=\"width: 120px;\"><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/atmosphere\/ch4\/\"><img decoding=\"async\" class=\"zoom-effect alignleft\" src=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/atm05_3_ch4_icon.jpg\" alt=\"\" width=\"100\" height=\"100\"\/><\/a><\/td>\n<td><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/atmosphere\/ch4\/\">Methane<\/a>, South-East Asia<br>\nAmong other sources, rice cultivation significantly contributes to the concentration of Methane in South-East Asia.<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 120px;\"><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/atmosphere\/ozone-hole\/\"><img decoding=\"async\" class=\"zoom-effect alignleft\" src=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/wp-content\/gismaps_maps\/Images\/atm05_4_ozone_icon.jpg\" alt=\"\" width=\"100\" height=\"100\"\/><\/a><\/td>\n<td><a href=\"https:\/\/esa-schoolatlas.eu\/esa-schoolatlas\/atmosphere\/ozone-hole\/\">Ozone Hole<\/a>, Antarctica<br>\nThe emission of industrially produced chemical components have led to a reduction of stratospheric ozone in the Antarctic region.<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n","protected":false},"excerpt":{"rendered":"<p>Atmosphere The gaseous component of the Earth system has a total mass of more than 5000 billion tons. Nevertheless the atmosphere (from Greek atmos for vapour) is only a relatively thin layer &#x2013; all relevant weather phenomena take place in the troposphere, which extends to an altitude of 12 to 15 kilometers only. Almost nothing [&#x2026;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-96","page","type-page","status-publish","hentry"],"translation":{"provider":"WPGlobus","version":"3.0.0","language":"it","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":true,"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>- 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\" 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