{"id":32983,"date":"2019-04-18T06:55:02","date_gmt":"2019-04-18T06:55:02","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=32983"},"modified":"2019-04-20T03:50:39","modified_gmt":"2019-04-20T03:50:39","slug":"ice-in-the-sea-of-okhotsk","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/32983","title":{"rendered":"Ice in the Sea of Okhotsk"},"content":{"rendered":"<p><div style=\"width: 649px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190418_himawari8_visible_Sea_of_Okhotsk_ice_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/HIM08_VIS_SEA_ICE_18APR2019_2019108_000000_HIMAWARI-8_0001PANEL.GIF\" alt=\"Himawari-8 \" width=\"639\" height=\"479\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 &#8220;Red&#8221; Visible <em>(0.64 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190418_himawari8_visible_Sea_of_Okhotsk_ice_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div><a href=\"https:\/\/www.jma.go.jp\/jma\/indexe.html\"><strong>JMA<\/strong><\/a> Himawari-8 &#8220;Red&#8221; Visible (0.64 \u00b5m) images <em><strong>(above)<\/strong><\/em> revealed circulations of ice within the <a href=\"https:\/\/en.wikipedia.org\/wiki\/Sea_of_Okhotsk\"><strong>Sea of Okhotsk<\/strong><\/a> (east of Sakhalin Island &#8212; station identifier UHSS is Yuzhno-Sakhalinsk, Russia) on 17-18 April 2019. Wind stress from an occluded Gale Force Low moving through that region on the previous day (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190416_190417_surface_analyses_West_Pacific_anim.gif\"><strong>surface analyses<\/strong><\/a>) likely helped to enhance some of the ice circulations.<\/p>\n<p>In a comparison of Himawari-8 &#8220;Red&#8221; Visible (0.64 \u00b5m) and Near-Infrared &#8220;Snow\/Ice&#8221; (1.61 \u00b5m) images <em><strong>(below)<\/strong>,<\/em> note that the ice appears much darker than cloud features (since ice is a strong absorber of radiation at the 1.61 \u00b5m wavelength).<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190418_himawari8_visible_snowIce_Sea_of_Okhotsk_ice_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/HIM08_VIS_NIR_SEA_ICE_18APR2019_2019108_000000_HIMAWARI-8_0002PANELS.GIF\" alt=\"Himawari-8 &quot;Red&quot; Visible (0.64 \u00b5m, left) and Near-Infrared &quot;Snow\/Ice&quot; (1.61 \u00b5m, right) images [click to play animation | MP4]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 &#8220;Red&#8221; Visible <em>(0.64 \u00b5m, left)<\/em> and Near-Infrared &#8220;Snow\/Ice&#8221; <em>(1.61 \u00b5m, right)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190418_himawari8_visible_snowIce_Sea_of_Okhotsk_ice_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Thanks to Thomas Birchard (NWS Honolulu) for bringing this interesting feature to our attention!<\/p>\n","protected":false},"excerpt":{"rendered":"<p>JMA Himawari-8 &#8220;Red&#8221; Visible (0.64 \u00b5m) images (above) revealed circulations of ice within the Sea of Okhotsk (east of Sakhalin Island &#8212; station identifier UHSS is Yuzhno-Sakhalinsk, Russia) on 17-18 April 2019. Wind stress from an occluded Gale Force Low moving through that region on the previous day (surface analyses) likely helped to enhance some [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":32999,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[62],"tags":[],"class_list":["post-32983","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-himawari-8"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/32983","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/users\/18"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=32983"}],"version-history":[{"count":10,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/32983\/revisions"}],"predecessor-version":[{"id":33000,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/32983\/revisions\/33000"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/32999"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=32983"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=32983"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=32983"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}