{"id":5755,"date":"2010-05-23T23:59:19","date_gmt":"2010-05-23T23:59:19","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=5755"},"modified":"2010-05-25T00:36:37","modified_gmt":"2010-05-25T00:36:37","slug":"atlantic-tropical-invest-90l","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/5755","title":{"rendered":"Atlantic Tropical Invest 90L"},"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\/05\/100523_vis_invest_anim.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"GOES-13 visible images + lower-tropospheric atmospheric motion vectors\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/05\/100523_vis_invest_anim.gif\" title=\"GOES-13 visible images + lower-tropospheric atmospheric motion vectors\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-13 visible images + lower-tropospheric atmospheric motion vectors<\/p><\/div>\n<p>An animation of GOES-13 visible images from the  <strong><a href=\"http:\/\/cimss.ssec.wisc.edu\/tropic2\/\">CIMSS Tropical Cyclones<\/a><\/strong> site <strong><em>(above)<\/em><\/strong> showed the development of a discrete low-level  cyclonic circulation associated with the first Atlantic Basin tropical cyclone &#8220;<strong><a href=\"http:\/\/www.aoml.noaa.gov\/hrd\/tcfaq\/A20.html\">Invest<\/a><\/strong>&#8221; of the season on <strong><a href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20100523.html\">23 May 2010<\/a><\/strong>. An overlay of lower-tropospheric atmospheric motion vectors <em>(along with a handful of ship reports)<\/em> also showed a broad cyclonic circulation around this developing cloud feature.<\/p>\n<p>GOES-13 IR images <strong><em>(below)<\/em><\/strong> showed that there were some large clusters of cold-topped convection located off to the northeast, but this deep convection did not appear to be directly related to the developing low-level cyclonic circulation seen on visible imagery. <\/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\/05\/100523_ir_invest_anim.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"GOES-13 IR images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/05\/100523_ir_invest_anim.gif\" title=\"GOES-13 IR images\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-13 IR images<\/p><\/div>\n<p>GOES-13 water vapor imagery with an overlay of deep layer <em>(850-200 hPa)<\/em> wind shear <strong><em>(below)<\/em><\/strong> showed  2 factors present that were unfavorable for the rapid intensification of Invest 90L: very dry air aloft moving in from the west, along with increasing values of wind shear &#8212; however, model guidance suggested that there was a small chance that this system could eventually develop into a subtropical cyclone.<\/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\/05\/100523_wv_shear_invest_anim.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"GOES-13 water vapor images + deep layer wind shear\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/05\/100523_wv_shear_invest_anim.gif\" title=\"GOES-13 water vapor images + deep layer wind shear\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-13 water vapor images + deep layer wind shear<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>An animation of GOES-13 visible images from the CIMSS Tropical Cyclones site (above) showed the development of a discrete low-level cyclonic circulation associated with the first Atlantic Basin tropical cyclone &#8220;Invest&#8221; of the season on 23 May 2010. An overlay of lower-tropospheric atmospheric motion vectors (along with a handful of ship reports) also showed a [&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":[11,25,2],"tags":[],"class_list":["post-5755","post","type-post","status-publish","format-standard","hentry","category-goes-13","category-satellite-winds","category-tropical-cyclones"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/5755","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=5755"}],"version-history":[{"count":9,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/5755\/revisions"}],"predecessor-version":[{"id":5772,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/5755\/revisions\/5772"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=5755"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=5755"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=5755"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}