{"id":660,"date":"2008-05-22T23:59:58","date_gmt":"2008-05-22T23:59:58","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/660"},"modified":"2008-05-31T01:18:26","modified_gmt":"2008-05-31T01:18:26","slug":"severe-thunderstorms-in-the-central-plains","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/660","title":{"rendered":"Severe thunderstorms over the Front Range and the central Plains"},"content":{"rendered":"<p><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2008\/05\/080522_goes_ir_anim.gif\" title=\"GOES IR images (Animated GIF)\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2008\/05\/080522_goes_ir_anim.gif\" title=\"GOES IR images (Animated GIF)\" alt=\"GOES IR images (Animated GIF)\" align=\"middle\" height=\"360\" width=\"480\" \/><\/a><\/p>\n<p>AWIPS images of the GOES 10.7 \u00c2\u00b5m IR channel <em><strong>(above)<\/strong><\/em> showed the development of severe thunderstorms across parts of Colorado, Wyoming, Nebraska, and Kansas on <strong><a href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20080522.html\" title=\"22 May 2008 daily weather map\" target=\"_blank\">22 May 2008<\/a> <\/strong><em>(<\/em><em>see also:<\/em><strong><em> <a href=\"http:\/\/rammb.cira.colostate.edu\/case_studies\/20080522\/\" title=\"CIRA RAMMB Satellite Case Study\" target=\"_blank\">CIRA RAMMB Satellite Case Study<\/a><\/em><\/strong><em>)<\/em>. According to the <a href=\"http:\/\/www.spc.noaa.gov\/climo\/reports\/080522_rpts.html\" title=\"SPC storm reports\" target=\"_blank\"><strong>SPC storm reports<\/strong><\/a>, a number of tornadoes were produced by these storms (one tornado-related fatality was reported near Greely, Colorado), along with large hail (up to <strong>2.75 inches<\/strong> in diameter near Windsor, Colorado and <strong>3.00 inches<\/strong> in diameter near Grinnell, Kansas).<\/p>\n<p><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2008\/05\/Sfc_Fronts_20080522_1759.png\" title=\"MODIS IR image\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2008\/05\/Sfc_Fronts_20080522_1759.png\" title=\"MODIS IR image\" alt=\"MODIS IR image\" align=\"middle\" height=\"451\" width=\"480\" \/><\/a><\/p>\n<p>A closer view using the 1-km resolution MODIS 11.0 \u00c2\u00b5m IR channel  <em><strong>(above)<\/strong><\/em> from around 17:57 UTC <em>(11:57 am local time)<\/em> revealed a rather diffuse <strong>&#8220;enhanced-v&#8221; signature<\/strong> just east\/northeast of Fort Collins, Colorado <em>(station identifier KFNL)<\/em>. This storm went on to produce tornadoes and large hail in southeastern Wyoming, with one tornado doing extensive damage in the Laramie area.<\/p>\n<p>Another MODIS IR image from around 19:34 UTC <em>(1:34 pm local time)<strong> <\/strong><\/em> displayed impressive detail in the overshooting top structure of the storms developing over western<em><strong> <\/strong><\/em>Kansas and far southwestern Nebraska<em><strong> (below)<\/strong>,<\/em> with the coldest cloud top brightness temperatures in the -70\u00c2\u00ba to -80\u00c2\u00ba C range <em>(black to while enhancement)<\/em>.<\/p>\n<p><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2008\/05\/MODIS_IR_20080522_1934_1.png\" title=\"MODIS IR image\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2008\/05\/MODIS_IR_20080522_1934_1.png\" title=\"MODIS IR image\" alt=\"MODIS IR image\" align=\"middle\" height=\"452\" width=\"481\" \/><\/a><\/p>\n<p>The GOES sounder derived Convective Available Potential Energy (CAPE) product <em><strong>(below)<\/strong><\/em> indicated that the pre-convective environment across northeastern Colorado during the morning hours was becoming unstable, with CAPE values in the 2000-4000 J kg-1 range <em>(yellow to red enhancement)<\/em> at 16:00 UTC <em>(10 am local time)<\/em>. The air mass south of the warm front and east of the dryline (from southern Kansas into Texas) was also very unstable, with CAPE values in some areas over 4000 J kg-1 <em>(purple enhancement)<\/em>.<\/p>\n<p><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2008\/05\/GOES_CAPE_20080522_1600.png\" title=\"GOES sounder CAPE product\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2008\/05\/GOES_CAPE_20080522_1600.png\" title=\"GOES sounder CAPE product\" alt=\"GOES sounder CAPE product\" align=\"middle\" height=\"457\" width=\"485\" \/><\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>AWIPS images of the GOES 10.7 \u00c2\u00b5m IR channel (above) showed the development of severe thunderstorms across parts of Colorado, Wyoming, Nebraska, and Kansas on 22 May 2008 (see also: CIRA RAMMB Satellite Case Study). According to the SPC storm reports, a number of tornadoes were produced by these storms (one tornado-related fatality was reported [&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":[15,19,12,3],"tags":[],"class_list":["post-660","post","type-post","status-publish","format-standard","hentry","category-goes-sounder","category-goes-12","category-modis","category-severe-convection"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/660","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=660"}],"version-history":[{"count":0,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/660\/revisions"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=660"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=660"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=660"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}