{"id":27503,"date":"2020-02-19T15:41:54","date_gmt":"2020-02-19T14:41:54","guid":{"rendered":"https:\/\/npolar.no\/?post_type=faktaside&#038;p=27503"},"modified":"2025-09-01T10:44:10","modified_gmt":"2025-09-01T08:44:10","slug":"albedo","status":"publish","type":"faktaside","link":"https:\/\/npolar.no\/en\/fact\/albedo\/","title":{"rendered":"Albedo effect"},"content":{"rendered":"<div id=\"attachment_2251\" style=\"width: 310px\" class=\"wp-caption alignright\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-2251\" class=\"wp-image-2251 size-medium\" src=\"https:\/\/npolar.no\/wp-content\/uploads\/\/albedo-sea-300x300.jpg\" alt=\"Figure showing the albedo effect on the ocean. The dark ocean absorbs the heat and reflects less back to the atmosphere than snow and ice.\" width=\"300\" height=\"300\" srcset=\"https:\/\/npolar.no\/wp-content\/uploads\/albedo-sea-300x300.jpg 300w, https:\/\/npolar.no\/wp-content\/uploads\/albedo-sea-450x450.jpg 450w, https:\/\/npolar.no\/wp-content\/uploads\/albedo-sea-100x100.jpg 100w, https:\/\/npolar.no\/wp-content\/uploads\/albedo-sea-80x80.jpg 80w, https:\/\/npolar.no\/wp-content\/uploads\/albedo-sea-768x768.jpg 768w, https:\/\/npolar.no\/wp-content\/uploads\/albedo-sea-36x36.jpg 36w, https:\/\/npolar.no\/wp-content\/uploads\/albedo-sea-180x180.jpg 180w, https:\/\/npolar.no\/wp-content\/uploads\/albedo-sea-705x705.jpg 705w, https:\/\/npolar.no\/wp-content\/uploads\/albedo-sea-32x32.jpg 32w, https:\/\/npolar.no\/wp-content\/uploads\/albedo-sea-50x50.jpg 50w, https:\/\/npolar.no\/wp-content\/uploads\/albedo-sea-64x64.jpg 64w, https:\/\/npolar.no\/wp-content\/uploads\/albedo-sea-96x96.jpg 96w, https:\/\/npolar.no\/wp-content\/uploads\/albedo-sea-128x128.jpg 128w, https:\/\/npolar.no\/wp-content\/uploads\/albedo-sea.jpg 800w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><p id=\"caption-attachment-2251\" class=\"wp-caption-text\">The albedo effect on sea. Illustration: Norwegian Polar Institute<\/p><\/div>\n<div id=\"attachment_27506\" style=\"width: 310px\" class=\"wp-caption alignright\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-27506\" class=\"wp-image-27506 size-medium\" src=\"https:\/\/npolar.no\/wp-content\/uploads\/2020\/02\/albedo-land-300x300.jpg\" alt=\"The albedo effect on land. Light-coloured surfaces like snpw and ice return a large part of the sunrays back to the atmosphere (high albedo)\" width=\"300\" height=\"300\" srcset=\"https:\/\/npolar.no\/wp-content\/uploads\/2020\/02\/albedo-land-300x300.jpg 300w, https:\/\/npolar.no\/wp-content\/uploads\/2020\/02\/albedo-land-450x450.jpg 450w, https:\/\/npolar.no\/wp-content\/uploads\/2020\/02\/albedo-land-100x100.jpg 100w, https:\/\/npolar.no\/wp-content\/uploads\/2020\/02\/albedo-land-80x80.jpg 80w, https:\/\/npolar.no\/wp-content\/uploads\/2020\/02\/albedo-land-768x768.jpg 768w, https:\/\/npolar.no\/wp-content\/uploads\/2020\/02\/albedo-land-36x36.jpg 36w, https:\/\/npolar.no\/wp-content\/uploads\/2020\/02\/albedo-land-180x180.jpg 180w, https:\/\/npolar.no\/wp-content\/uploads\/2020\/02\/albedo-land-705x705.jpg 705w, https:\/\/npolar.no\/wp-content\/uploads\/2020\/02\/albedo-land.jpg 800w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><p id=\"caption-attachment-27506\" class=\"wp-caption-text\">The albedo effect on land. Illustration: Norwegian Polar Institute<\/p><\/div>\n<p class=\"s4\">Albedo describes the ability of surfaces to reflect sunlight. Light-coloured surfaces immediately return a large part of the solar energy back to the atmosphere (high albedo). Dark surfaces absorb the energy from the sun and convert it to heat (low albedo). The Albedo Effect is a self-reinforcing effect which is important for the development of climate change globally, including the melting rate of the ice and the temperature of the oceans.<\/p>\n<p class=\"s4\">Ice- and snow-covered areas have high albedo, and the ice-covered polar regions reflect solar radiation which otherwise would be absorbed by oceans and land areas and cause the Earth\u2019s surface to heat up. The proportion of the Earth\u2019s surface that is covered by snow and ice has a great deal to say for how much of the incoming solar radiation is reflected or absorbed. Low albedo (dark surfaces) leads to higher uptake of energy and, hence, warming. Moreover, when more ice and snow melt, there will be more dark surfaces and increased warming. This is therefore a self-reinforcing effect. Climate change in the Arctic and the Antarctic isconsequently important for the development of global climate change.<\/p>\n<p>&nbsp;<\/p>\n","protected":false},"template":"","class_list":["post-27503","faktaside","type-faktaside","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/faktaside\/27503","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/faktaside"}],"about":[{"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/types\/faktaside"}],"wp:attachment":[{"href":"https:\/\/npolar.no\/en\/wp-json\/wp\/v2\/media?parent=27503"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}