{"id":32507,"date":"2019-03-09T23:59:59","date_gmt":"2019-03-09T23:59:59","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=32507"},"modified":"2019-03-20T01:36:01","modified_gmt":"2019-03-20T01:36:01","slug":"unusual-ice-loss-in-the-bering-sea","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/32507","title":{"rendered":"Unusual early ice loss in the Bering Sea"},"content":{"rendered":"<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190201_190309_gcomw2_amsr2_seaIceConcentration_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/seaice_NH_20190304_nasateam2.png\" alt=\"GCOM-W2 AMSR2 Sea Ice Concentration, 01 February - 09 March 2019 [click to play animation | MP4]\" width=\"641\" height=\"854\" \/><\/a><p class=\"wp-caption-text\">GCOM-W1 AMSR2 Sea Ice Concentration, 01 February &#8211; 09 March 2019 [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/190201_190309_gcomw2_amsr2_seaIceConcentration_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>A persistent northward transport of anomalously-warm air across the Bering Sea during the month of February 2019 led to an unusual loss of sea ice there &#8212; daily images of GCOM-W1 AMSR2 Sea Ice Concentration (<a href=\"https:\/\/stratus.ssec.wisc.edu\/cgi-bin\/amsr2snow_main\"><strong>source<\/strong><\/a>) from 01 February to 09 March <em><strong>(above)<\/strong><\/em> showed the northward retreat of ice from the Bering Sea into the Chukchi Sea. The ice reached its maximum northward extent on <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/seaice_NH_20190304_nasateam2.png\"><strong>04 March<\/strong><\/a>; northward ice motion was very pronounced during the <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/icemotion_NH_20190226.png\">25-26 February<\/a><\/strong> and <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/03\/icemotion_NH_20190228.png\">27-28 February<\/a><\/strong> periods. In early March a synoptic pattern change then allowed cold arctic air to flow back toward the south, helping the ice concentration to begin increasing again in the northern portion of the Bering Sea.<\/p>\n<p>Minimal cloudiness on 28 February allowed the northward flow of ice through the Bering Strait to be seen on GOES-17 <em>(GOES-West)<\/em> &#8220;Red&#8221; Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>) images <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/190228_goes17_visible_Bering_Sea_ice_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/02\/G17_VIS_BERING_STRAIT_ICE_28FEB2019_2019059_214538_GOES-17_0001PANEL.GIF\" alt=\"GOES-17 \" width=\"641\" height=\"481\" \/><\/a><p class=\"wp-caption-text\">GOES-17 &#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\/02\/190228_goes17_visible_Bering_Sea_ice_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div><br \/>\n<center><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Bering Sea ice extent for Mar 02 from <a href=\"https:\/\/twitter.com\/NSIDC?ref_src=twsrc%5Etfw\">@NSIDC<\/a> data (210000 km\u00b2) is the lowest daily <a href=\"https:\/\/twitter.com\/hashtag\/seaice?src=hash&amp;ref_src=twsrc%5Etfw\">#seaice<\/a> extent of record for the entire month of March &amp; only 29% of 1981-2010 average. Previous lowest 214000 km\u00b2 on Mar 09, 2018.   <a href=\"https:\/\/twitter.com\/hashtag\/Arctic?src=hash&amp;ref_src=twsrc%5Etfw\">#Arctic<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/akwx?src=hash&amp;ref_src=twsrc%5Etfw\">#akwx<\/a> <a href=\"https:\/\/twitter.com\/Climatologist49?ref_src=twsrc%5Etfw\">@Climatologist49<\/a> <a href=\"https:\/\/twitter.com\/ZLabe?ref_src=twsrc%5Etfw\">@ZLabe<\/a> <a href=\"https:\/\/twitter.com\/YJRosen?ref_src=twsrc%5Etfw\">@YJRosen<\/a> <a href=\"https:\/\/twitter.com\/ArcticResearch?ref_src=twsrc%5Etfw\">@ArcticResearch<\/a> <a href=\"https:\/\/t.co\/IzjwGXELCL\">pic.twitter.com\/IzjwGXELCL<\/a><\/p>\n<p>&mdash; Rick Thoman (@AlaskaWx) <a href=\"https:\/\/twitter.com\/AlaskaWx\/status\/1102243761592000513?ref_src=twsrc%5Etfw\">March 3, 2019<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p lang=\"en\" dir=\"ltr\">Sea ice in the Bering Sea began the month of February with a near record low extent, and then near record southerly winds blew from a region of much above normal SSTs. On the left panel, red is southerly winds &gt; +2.5 std. dev. above average. <a href=\"https:\/\/twitter.com\/AlaskaWx?ref_src=twsrc%5Etfw\">@AlaskaWx<\/a> <a href=\"https:\/\/twitter.com\/IARC_Alaska?ref_src=twsrc%5Etfw\">@IARC_Alaska<\/a> <a href=\"https:\/\/t.co\/cUh6CdQqhd\">pic.twitter.com\/cUh6CdQqhd<\/a><\/p>\n<p>&mdash; Brian Brettschneider (@Climatologist49) <a href=\"https:\/\/twitter.com\/Climatologist49\/status\/1104113393349255169?ref_src=twsrc%5Etfw\">March 8, 2019<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><br \/>\n<\/center><\/p>\n","protected":false},"excerpt":{"rendered":"<p>A persistent northward transport of anomalously-warm air across the Bering Sea during the month of February 2019 led to an unusual loss of sea ice there &#8212; daily images of GCOM-W1 AMSR2 Sea Ice Concentration (source) from 01 February to 09 March (above) showed the northward retreat of ice from the Bering Sea into the [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[37,81,80,79],"tags":[],"class_list":["post-32507","post","type-post","status-publish","format-standard","hentry","category-arctic","category-gcom-w1","category-goes-17","category-microwave"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/32507","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=32507"}],"version-history":[{"count":6,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/32507\/revisions"}],"predecessor-version":[{"id":32514,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/32507\/revisions\/32514"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=32507"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=32507"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=32507"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}