{"id":336697,"date":"2016-12-12T23:12:00","date_gmt":"2016-12-12T20:12:00","guid":{"rendered":"http:\/\/www.fyysika.ee\/?guid=0a07294c4e937b9ef1681be72fa7eed1"},"modified":"2016-12-12T23:12:00","modified_gmt":"2016-12-12T20:12:00","slug":"nasausgs-provide-global-view-of-speed-of-ice","status":"publish","type":"post","link":"https:\/\/www.fyysika.ee\/?p=336697","title":{"rendered":"NASA\/USGS Provide Global View of Speed of Ice"},"content":{"rendered":"<p><a href=\"http:\/\/www.jpl.nasa.gov\/news\/news.php?release=2016-316&#038;rn=news.xml&#038;rst=6698\"><br \/>\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/www.jpl.nasa.gov\/images\/earth\/climate\/20161212\/earth20161212-226.jpg\" align=\"left\" alt=\"Texture on the surface of flowing ice\" width=\"100\" height=\"75\" border=\"0\" \/><\/a><\/p>\n<p>\t\tGlaciers and ice sheets move in unique patterns, as evidenced by a new capability that uses satellites to map ice flow speeds in Greenland, Antarctica and mountain ranges.\n\t\t<\/p>\n<p><br clear=\"all\"\/><\/p>\n","protected":false},"excerpt":{"rendered":"<p>\t\tGlaciers and ice sheets move in unique patterns, as evidenced by a new capability that uses satellites to map ice flow speeds in Greenland, Antarctica and mountain ranges. <\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_genesis_hide_title":false,"_genesis_hide_breadcrumbs":false,"_genesis_hide_singular_image":false,"_genesis_hide_footer_widgets":false,"_genesis_custom_body_class":"","_genesis_custom_post_class":"","_genesis_layout":"","footnotes":""},"categories":[179],"tags":[],"class_list":{"0":"post-336697","1":"post","2":"type-post","3":"status-publish","4":"format-standard","6":"category-rss-kosmos","7":"entry"},"_links":{"self":[{"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=\/wp\/v2\/posts\/336697","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=336697"}],"version-history":[{"count":0,"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=\/wp\/v2\/posts\/336697\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=336697"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=336697"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.fyysika.ee\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=336697"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}