{"id":726,"date":"2013-02-20T17:50:11","date_gmt":"2013-02-20T17:50:11","guid":{"rendered":"https:\/\/crs.hi.is\/?page_id=726"},"modified":"2014-01-13T13:45:15","modified_gmt":"2014-01-13T13:45:15","slug":"ers-12-tandem-data","status":"publish","type":"page","link":"https:\/\/crs.hi.is\/?page_id=726","title":{"rendered":"ERS 1\/2 tandem data"},"content":{"rendered":"<p><strong>What is this data?<\/strong><\/p>\n<p>In the years 1995-2000 ERS-2 satellite repeated approximately the orbit of the ERS-1 satellite with exactly 24 hour delay. This opened a new opportunity for InSAR studies of terrains with relatively fast motion rate and rapidly changing surface. This data proved very valuable for studying eg. the <a title=\"Glaciers\" href=\"https:\/\/crs.hi.is\/?page_id=138\">glacier motion<\/a>.<\/p>\n<p><strong>Where is it available?<\/strong><\/p>\n<p>Information on the availability of ERS 1\/2 tandem data of Icelandic glacier can be found <a href=\"www.raunvis.hi.is\/~eyjolfm\/HBFPSG.htm\" target=\"_blank\">here<\/a>.<\/p>\n<p><strong>References:<\/strong><\/p>\n<ul>\n<li>\u00a0<a href=\"http:\/\/www.esa.int\/Our_Activities\/Observing_the_Earth\/ERS_overview\" target=\"_blank\">http:\/\/www.esa.int\/Our_Activities\/Observing_the_Earth\/ERS_overview<\/a><\/li>\n<\/ul>\n<p><strong>Users:<\/strong><\/p>\n<ul>\n<li><a title=\"Eyj\u00f3lfur Magn\u00fasson\" href=\"https:\/\/crs.hi.is\/?page_id=155\" target=\"_blank\">Eyj\u00f3lfur Magn\u00fasson<\/a><\/li>\n<li><a title=\"Finnur P\u00e1lsson\" href=\"https:\/\/crs.hi.is\/?page_id=159\" target=\"_blank\">Finnur P\u00e1lsson<\/a><\/li>\n<li><a title=\"Helgi Bj\u00f6rnsson\" href=\"https:\/\/crs.hi.is\/?page_id=147\" target=\"_blank\">Helgi Bj\u00f6rnsson<\/a><\/li>\n<li><a title=\"Sverrir Gu\u00f0mundsson\" href=\"https:\/\/crs.hi.is\/?page_id=150\">Sverrir Gu\u00f0mundsson<\/a><\/li>\n<\/ul>\n","protected":false},"excerpt":{"rendered":"<p>What is this data? In the years 1995-2000 ERS-2 satellite repeated approximately the orbit of the ERS-1 satellite with exactly 24 hour delay. This opened a new opportunity for InSAR studies of terrains with relatively fast motion rate and rapidly &hellip; <a href=\"https:\/\/crs.hi.is\/?page_id=726\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":3,"featured_media":0,"parent":448,"menu_order":2,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"_links":{"self":[{"href":"https:\/\/crs.hi.is\/index.php?rest_route=\/wp\/v2\/pages\/726"}],"collection":[{"href":"https:\/\/crs.hi.is\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/crs.hi.is\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/crs.hi.is\/index.php?rest_route=\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/crs.hi.is\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=726"}],"version-history":[{"count":14,"href":"https:\/\/crs.hi.is\/index.php?rest_route=\/wp\/v2\/pages\/726\/revisions"}],"predecessor-version":[{"id":955,"href":"https:\/\/crs.hi.is\/index.php?rest_route=\/wp\/v2\/pages\/726\/revisions\/955"}],"up":[{"embeddable":true,"href":"https:\/\/crs.hi.is\/index.php?rest_route=\/wp\/v2\/pages\/448"}],"wp:attachment":[{"href":"https:\/\/crs.hi.is\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=726"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}