{"id":8307,"date":"2011-06-09T17:36:01","date_gmt":"2011-06-09T17:36:01","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=8307"},"modified":"2011-06-10T22:28:52","modified_gmt":"2011-06-10T22:28:52","slug":"hurricane-adrian-in-the-east-pacific","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/8307","title":{"rendered":"Hurricane Adrian in the East Pacific"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110609_g12_vis_adrian_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-12 0.63 \u00c2\u00b5m visible channel images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110609_g12_vis_adrian_anim.gif\" alt=\"GOES-12 0.63 \u00c2\u00b5m visible channel images\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-12 0.63 \u00c2\u00b5m visible channel images<\/p><\/div>\n<p>&nbsp;<\/p>\n<p>Hurricane Adrian developed into a Category 3 hurricane early in the day on<strong> 09 June 2011<\/strong>. McIDAS images of GOES-12 0.63 \u00c2\u00b5m visible channel data <em><strong>(above)<\/strong><\/em> initially showed a well-defined eye before it began to get partially obscured by the high clouds of a central dense overcast (CDO).<\/p>\n<p>DMSP SSMIS 85 GHz microwave images from the <a title=\"CIMSS Tropical Cyclones site\" href=\"http:\/\/tropic.ssec.wisc.edu\/\"><strong>CIMSS Tropical Cyclones<\/strong><\/a> site <em><strong>(below)<\/strong><\/em> revealed a distinct eye at 12:09 UTC and 14:56 UTC.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110609_adrian_mw_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"DMSP SSMIS 85 GHz microwave images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110609_adrian_mw_anim.gif\" alt=\"DMSP SSMIS 85 GHz microwave images\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">DMSP SSMIS 85 GHz microwave images<\/p><\/div>\n<p>GOES 10.7 \u00c2\u00b5m IR images <em><strong>(below)<\/strong><\/em> also briefly showed a well-defined eye early in the day, which later filled in a bit beneath the CDO as a curved band of cold high clouds began to wrap around the eastern and northern quadrants 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\/2011\/06\/110609_adrian_ir_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES 10.7 \u00c2\u00b5m IR images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110609_adrian_ir_anim.gif\" alt=\"GOES 10.7 \u00c2\u00b5m IR images\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES 10.7 \u00c2\u00b5m IR images<\/p><\/div>\n<p>The circulation of Hurricane Adrian could be clearly seen on an AWIPS image of ASCAT scatterometer winds overlaid on a GOES IR image<em><strong> (below)<\/strong><\/em>.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/Scat_Winds_-_10m_20110609_1633.png\"><img loading=\"lazy\" decoding=\"async\" title=\"ASCAT scatterometer winds (overlaid on GOES IR image)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/Scat_Winds_-_10m_20110609_1633.png\" alt=\"ASCAT scatterometer winds (overlaid on GOES IR image)\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">ASCAT scatterometer winds (overlaid on GOES IR image)<\/p><\/div>\n<p>AWIPS images of the MIMIC Total Precipitable Water (TPW) product <em><strong>(below)<\/strong><\/em> showed that Adrian was tapping moisture from the Inter-Tropical Convergence Zone (ITCZ) \/ &#8220;Monsoon Trough&#8221;, which was located at approximately 10\u00c2\u00ba North latitude over the eastern Pacific Ocean.<\/p>\n<p style=\"text-align: center;\">&nbsp;<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110609_mimic_tpw_adrian_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"MIMIC Total Precipitable Water product\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/MIMIC_TPW_20110609_1700.png\" alt=\"MIMIC Total Precipitable Water product\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">MIMIC Total Precipitable Water product<\/p><\/div>\n<p style=\"text-align: center;\"><strong>===== 10 June Update =====<\/strong><\/p>\n<p style=\"text-align: left;\">Hurricane Adrian intensified to a Category 4 storm on <strong>10 June 2011<\/strong>. 4-km resolution GOES 10.7 \u00c2\u00b5m IR channel images <em><strong>(below; click image to play animation)<\/strong><\/em> continued to show a well-defined eye structure.<\/p>\n<p style=\"text-align: center;\">\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110610_adrian_goes_ir_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"GOES 10.7 \u00c2\u00b5m IR images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110610_1645_adrian_ir.gif\" alt=\"GOES 10.7 \u00c2\u00b5m IR images (click image to play animation)\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES 10.7 \u00c2\u00b5m IR images (click image to play animation)<\/p><\/div>\n<p style=\"text-align: left;\">A closer view of the eye could be seen using 1-km resolution GOES visible channel images <em><strong>(below; click image to play animation)<\/strong><\/em>.<\/p>\n<p style=\"text-align: center;\">\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110610_adrian_goes_vis_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"GOES visible channel images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110610_1600_adrian_vis.gif\" alt=\"GOES visible channel images (click image to play animation)\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES visible channel images (click image to play animation)<\/p><\/div>\n<p style=\"text-align: left;\">The intensity of Hurricane Adrian was expected to decrease as the storm began to move over colder waters, as seen on an image of the Sea Surface Temperature (SST) analysis<em><strong> (below)<\/strong><\/em>.<\/p>\n<p style=\"text-align: center;\">\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110610_adrian_sst.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"Sea Surface Temperature (SST) analysis\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110610_adrian_sst.gif\" alt=\"Sea Surface Temperature (SST) analysis\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">Sea Surface Temperature (SST) analysis<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>&nbsp; Hurricane Adrian developed into a Category 3 hurricane early in the day on 09 June 2011. McIDAS images of GOES-12 0.63 \u00c2\u00b5m visible channel data (above) initially showed a well-defined eye before it began to get partially obscured by the high clouds of a central dense overcast (CDO). DMSP SSMIS 85 GHz microwave images [&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":[19,25,2],"tags":[],"class_list":["post-8307","post","type-post","status-publish","format-standard","hentry","category-goes-12","category-satellite-winds","category-tropical-cyclones"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/8307","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=8307"}],"version-history":[{"count":12,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/8307\/revisions"}],"predecessor-version":[{"id":8310,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/8307\/revisions\/8310"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=8307"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=8307"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=8307"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}