{"id":11390,"date":"2017-01-24T08:55:11","date_gmt":"2017-01-24T08:55:11","guid":{"rendered":"http:\/\/revoscience.com\/en\/?p=11390"},"modified":"2017-01-24T08:55:11","modified_gmt":"2017-01-24T08:55:11","slug":"frost-build-near-mars-north-pole","status":"publish","type":"post","link":"https:\/\/www.revoscience.com\/en\/frost-build-near-mars-north-pole\/","title":{"rendered":"Frost build-up near Mars north pole"},"content":{"rendered":"<figure id=\"attachment_11391\" aria-describedby=\"caption-attachment-11391\" style=\"width: 640px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-11391\" src=\"http:\/\/revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif\" alt=\"\" width=\"640\" height=\"360\" title=\"\"><figcaption id=\"caption-attachment-11391\" class=\"wp-caption-text\">Credit: ESA\/Mars Express \u2013 CC BY-SA 3.0 IGO<\/figcaption><\/figure>\n<p><span style=\"color: #000000;\">This animated gif shows the build up of frosts in a 73 x 41 km section of the north polar ice cap of Mars between November and December 2004.<\/span><\/p>\n<p><span style=\"color: #000000;\">The images were taken by the High Resolution Stereo Camera on<a href=\"https:\/\/en.wikipedia.org\/wiki\/European_Space_Agency\" target=\"_blank\" rel=\"noopener\"> ESA<\/a>\u2019s Mars Express during its first year at the Red Planet. It has been orbiting Mars for over 13 years.<\/span><\/p>\n<p><span style=\"color: #000000;\">The first image was taken on 23 November 2004 during orbit 1087, and the second of the same area on 30 December 2004, during orbit 1219. The images are centred at 79.94\u00baN \/ 44.11\u00baE. The interleaving frames in the gif are <a href=\"https:\/\/en.wikipedia.org\/wiki\/Interpolation\" target=\"_blank\" rel=\"noopener\">interpolated<\/a> to give a smooth appearance.<\/span><\/p>\n<p>[pullquote]During the warmer summer months, most of the carbon dioxide ice turns directly into vapour and escapes into the atmosphere, leaving behind the water-ice layers.[\/pullquote]<\/p>\n<p><span style=\"color: #000000;\">The north polar icecap comprises layers of water-ice that extend to a depth of around 2 km. The layers result from seasonal melting and deposition of ice mixed with dust.<\/span><\/p>\n<p><span style=\"color: #000000;\">During winter the water-ice is covered by a thin layer of carbon dioxide ice that is a few centimetres to around a metre thick.<\/span><\/p>\n<p><span style=\"color: #000000;\">During the warmer summer months, most of the carbon dioxide ice turns directly into vapour and escapes into the atmosphere, leaving behind the water-ice layers.<\/span><\/p>\n<p><span style=\"color: #000000;\">But when the seasons start to change again, a thin veneer of solid carbon dioxide begins to encroach, as seen in these images, which captures subtle changes between summer and autumn.<\/span><\/p>\n<p><span style=\"color: #000000;\">The original images are available in the<\/span> <a href=\"http:\/\/archives.esac.esa.int\/psa\" target=\"_blank\" rel=\"noopener\">Mars Express archive<\/a><span style=\"color: #000000;\">, and are shown at 50 m\/pixel.<\/span><\/p>\n","protected":false},"excerpt":{"rendered":"<p>This animated gif shows the build up of frosts in a 73 x 41 km section of the north polar ice cap of Mars between November and December 2004. The images were taken by the High Resolution Stereo Camera on ESA\u2019s Mars Express during its first year at the Red Planet. It has been orbiting [&hellip;]<\/p>\n","protected":false},"author":6,"featured_media":11391,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[20],"tags":[],"class_list":["post-11390","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-space-news"],"featured_image_urls":{"full":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif",640,360,false],"thumbnail":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu-150x150.gif",150,150,true],"medium":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu-300x169.gif",300,169,true],"medium_large":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif",640,360,false],"large":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif",640,360,false],"1536x1536":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif",640,360,false],"2048x2048":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif",640,360,false],"ultp_layout_landscape_large":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif",640,360,false],"ultp_layout_landscape":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif",640,360,false],"ultp_layout_portrait":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif",600,338,false],"ultp_layout_square":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif",600,338,false],"newspaper-x-single-post":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif",640,360,false],"newspaper-x-recent-post-big":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif",550,309,false],"newspaper-x-recent-post-list-image":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif",95,53,false],"web-stories-poster-portrait":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif",640,360,false],"web-stories-publisher-logo":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif",96,54,false],"web-stories-thumbnail":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2017\/01\/imagefrostbu.gif",150,84,false]},"author_info":{"info":["Amrita Tuladhar"]},"category_info":"<a href=\"https:\/\/www.revoscience.com\/en\/category\/news\/space-news\/\" rel=\"category tag\">Space\/ AstroPhysics<\/a>","tag_info":"Space\/ AstroPhysics","comment_count":"0","_links":{"self":[{"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/posts\/11390","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/users\/6"}],"replies":[{"embeddable":true,"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/comments?post=11390"}],"version-history":[{"count":0,"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/posts\/11390\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/media\/11391"}],"wp:attachment":[{"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/media?parent=11390"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/categories?post=11390"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/tags?post=11390"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}