{"id":6524,"date":"2010-08-29T19:43:22","date_gmt":"2010-08-29T19:43:22","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=6524"},"modified":"2010-08-31T18:53:23","modified_gmt":"2010-08-31T18:53:23","slug":"hurricane-earl","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/6524","title":{"rendered":"Hurricane Earl"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/08\/100829_earl_ir_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-13 10.7 \u00c2\u00b5m IR images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/08\/100829_earl_ir_anim.gif\" alt=\"GOES-13 10.7 \u00c2\u00b5m IR images\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-13 10.7 \u00c2\u00b5m IR images<\/p><\/div>\n<p>GOES-13 10.7 \u00c2\u00b5m IR images <strong><em>(above)<\/em><\/strong> and 0.63 \u00c2\u00b5m visible images <strong><em>(below)<\/em><\/strong> from the <strong><a href=\"http:\/\/cimss.ssec.wisc.edu\/tropic2\/#\">CIMSS Tropical Cyclones<\/a><\/strong> site showed Hurricane Earl after the storm reached Category 1 intensity on <strong>29 August 2010<\/strong>. A Central Dense Overcast (CDO) could be seen developing in the images as Earl approached the Leeward Islands.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/08\/100829_earl_vis_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-13 0.63 \u00c2\u00b5m visible images + surface reports\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/08\/100829_earl_vis_anim.gif\" alt=\"GOES-13 0.63 \u00c2\u00b5m visible images + surface reports\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-13 0.63 \u00c2\u00b5m visible images + surface reports<\/p><\/div>\n<p>A comparison of 85 GHz microwave images at 11:02 UTC and 17:23 UTC <strong><em>(below)<\/em><\/strong> revealed the increasing organization of  banded convective elements around the center of the hurricane.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/08\/100829_earl_mw_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"SSMI\/S-16 and AMSR-E 85 GHz microwave images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/08\/100829_earl_mw_anim.gif\" alt=\"SSMI\/S-16 and AMSR-E 85 GHz microwave images\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">SSMI\/S-16 and AMSR-E 85 GHz microwave images<\/p><\/div>\n<p style=\"text-align: center;\"><strong>=========================================<\/strong><\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/08\/100829_g15_vis_rso_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-15 0.63 \u00c2\u00b5m visible images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/08\/100829_g15_vis_rso_anim.gif\" alt=\"GOES-15 0.63 \u00c2\u00b5m visible images\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-15 0.63 \u00c2\u00b5m visible images<\/p><\/div>\n<p>As a part of the <strong><a href=\"http:\/\/rammb.cira.colostate.edu\/projects\/goes-p\/\">GOES-15 Post Launch Science Test<\/a><\/strong>, the satellite was placed into Rapid Scan Operations (RSO) mode, providing images periodically at 5-minute intervals. GOES-15 0.63 \u00c2\u00b5m visible images <strong><em>(above; also available as a <a title=\"GOES-15 visible images (QuickTime movie)\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/08\/100829_g15_vis_rso.mov\" target=\"_blank\">QuickTime movie<\/a>)<\/em><\/strong> and 10.7 \u00c2\u00b5m IR images <strong><em>(below; also available as a <a title=\"GOES-15 IR images (QuickTime movie)\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/08\/100829_g15_ir4_rso.mov\" target=\"_blank\">QuickTime movie<\/a>)<\/em><\/strong> showed two distinct convective bursts that were developing within the CDO region <em>(the 15 UTC and 18 UTC positions of the center of Earl are marked on the images)<\/em>. The coldest cloud top IR brightness temperatures were <strong>-86\u00c2\u00ba C<\/strong> <em>(darker violet color enhancement)<\/em> at 16:15 UTC and again at 19:25 UTC.<\/p>\n<p>The far eastern portion of the island of Guadeloupe can be seen mapped in dark blue along the lower left edge of the GOES-15 images.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/08\/100829_g15_ir4_rso_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-15 10.7 \u00c2\u00b5m IR images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/08\/100829_g15_ir4_rso_anim.gif\" alt=\"GOES-15 10.7 \u00c2\u00b5m IR images\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-15 10.7 \u00c2\u00b5m IR images<\/p><\/div>\n<p>Be sure to check out the <strong><a href=\"https:\/\/groups.ssec.wisc.edu\/groups\/tropical-cyclones\/field-experiments\/predict\">PREDICT Field Experiment Blog<\/a><\/strong> for additional insights on other tropical cyclone activity in the Atlantic basin.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>GOES-13 10.7 \u00c2\u00b5m IR images (above) and 0.63 \u00c2\u00b5m visible images (below) from the CIMSS Tropical Cyclones site showed Hurricane Earl after the storm reached Category 1 intensity on 29 August 2010. A Central Dense Overcast (CDO) could be seen developing in the images as Earl approached the Leeward Islands. A comparison of 85 GHz [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[11,43,26,2],"tags":[],"class_list":["post-6524","post","type-post","status-publish","format-standard","hentry","category-goes-13","category-goes-15","category-poes","category-tropical-cyclones"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/6524","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=6524"}],"version-history":[{"count":13,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/6524\/revisions"}],"predecessor-version":[{"id":6528,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/6524\/revisions\/6528"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=6524"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=6524"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=6524"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}