{"id":351,"date":"2007-02-02T19:24:14","date_gmt":"2007-02-02T19:24:14","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/2007\/02\/02\/fatal-tornado-outbreak-in-florida\/"},"modified":"2007-02-08T15:34:45","modified_gmt":"2007-02-08T15:34:45","slug":"fatal-tornado-outbreak-in-florida","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/351","title":{"rendered":"Fatal tornado outbreak in Florida"},"content":{"rendered":"<p><a target=\"_blank\" title=\"GOES-12 10.7\u00c2\u00b5m IR image\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/02\/070202_G12_IR4_24.GIF\"><img loading=\"lazy\" decoding=\"async\" width=\"480\" height=\"360\" align=\"middle\" alt=\"GOES-12 10.7\u00c2\u00b5m IR image\" title=\"GOES-12 10.7\u00c2\u00b5m IR image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/02\/070202_G12_IR4_24.GIF\" \/><\/a><br \/>\nGOES-12 10.7\u00c2\u00b5m InfraRed (IR) imagery <em><strong>(above; <a title=\"GOES-12 IR images (Java animation)\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/02\/070202_g12_ir4.html\">Java animation<\/a>)<\/strong><\/em> shows the development of multiple lines of convection that produced numerous reports of damaging winds and tornadoes across northern and central Florida during the pre-dawn hours\u00c2\u00a0 on <a target=\"_blank\" title=\"02 February 2007 daily weather map\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20070202.html\"><strong>02 February 2007<\/strong><\/a>.  The counties where damaging winds and\/or tornadoes were reported are highlighted in blue around the times of the <a title=\"SPC storm reports\" target=\"_blank\" href=\"http:\/\/www.spc.noaa.gov\/climo\/reports\/070201_rpts.html\"><strong>SPC storm reports<\/strong><\/a>. At least 3 of these tornadoes have been rated as producing <a title=\"tornado survey\" target=\"_blank\" href=\"http:\/\/www.srh.noaa.gov\/mlb\/surveys\/020207\/index.html\"><strong>EF-3 damage<\/strong><\/a>, and 20  deaths have been reported so far as a result of these storms.  While fairly cold IR cloud top temperatures were noted at times <em>(-60\u00c2\u00ba to -66\u00c2\u00ba C, red to dark red enhancement),<\/em> there were no &#8220;enhanced-V&#8221; or other typical  severe storm IR signatures associated with this convection.<\/p>\n<p>.<br \/>\nThese supercells formed within an environment of <a target=\"_blank\" title=\"GOES-12 IR image, surface reports, 500mb winds\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/02\/070202_00z_ir_winds.jpg\"><strong>high vertical wind shear<\/strong><\/a>, which enabled the thunderstorm updrafts to develop strong rotation; in addition, a <a title=\"GOES-12 water vapor image, upper level winds\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/02\/070202_10z_wv_winds.jpg\"><strong>strong upper tropospheric jet stream<\/strong><\/a> was located over the southeastern US, producing high wind speeds aloft and supporting large-scale lift over Florida. The lines of severe convection were forming within a zone of pre-frontal <a target=\"_blank\" title=\"winds-derived lower-tropospheric convergence\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/02\/wg8conv-4.gif\"><strong>lower-tropospheric convergence<\/strong><\/a>; while it was too cloudy to sample the immediate pre-convective environment, GOES-12 sounder derived product imagery (DPI) at <strong><a title=\"AWIPS images of GOES sounder derived products\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/02\/070202_00z_sounder_ir.jpg\">00 UTC<\/a><\/strong> and at <strong>12:00 UTC<\/strong> <em><strong>(below)<\/strong><\/em>  did show that the air mass ahead of the approaching frontal boundary was relatively moist <em>(PW values of 40-50 mm)<\/em> with modest winter-season instability <em>(LI values of 0\u00c2\u00ba to -6\u00c2\u00ba C, CAPE values of 0 to 1000 J\/kg).<\/em><br \/>\n<a title=\"AWIPS images of GOES sounder derived products\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/02\/070202_12z_sounder_ir.jpg\"><img loading=\"lazy\" decoding=\"async\" width=\"480\" height=\"463\" align=\"middle\" title=\"AWIPS images of GOES sounder derived products\" alt=\"AWIPS images of GOES sounder derived products\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/02\/070202_12z_sounder_ir.jpg\" \/><\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>GOES-12 10.7\u00c2\u00b5m InfraRed (IR) imagery (above; Java animation) shows the development of multiple lines of convection that produced numerous reports of damaging winds and tornadoes across northern and central Florida during the pre-dawn hours\u00c2\u00a0 on 02 February 2007. The counties where damaging winds and\/or tornadoes were reported are highlighted in blue around the times of [&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":[15,19,3],"tags":[],"class_list":["post-351","post","type-post","status-publish","format-standard","hentry","category-goes-sounder","category-goes-12","category-severe-convection"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/351","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=351"}],"version-history":[{"count":0,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/351\/revisions"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=351"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=351"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=351"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}