{"id":9839,"date":"2012-02-29T22:31:44","date_gmt":"2012-02-29T22:31:44","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=9839"},"modified":"2012-03-01T20:31:52","modified_gmt":"2012-03-01T20:31:52","slug":"leap-day-2012-severe-weather","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/9839","title":{"rendered":"Leap Day 2012 Severe Weather"},"content":{"rendered":"<p>Severe thunderstorms during the early morning hours of <strong><a title=\"29 February 2012 daily weather map\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20120229.html\">February 29th, 2012<\/a><\/strong> produced several tornadoes over Missouri, including one near Branson, and one near Lebanon. (Annotated SPC storm report map <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/StormReports_28Feb2012.gif\">here<\/a>, originally from <a href=\"http:\/\/www.spc.noaa.gov\/climo\/reports\/120228_rpts.html\">here<\/a>) The GOES-13 enhanced infrared images from <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/GOES13_BAND4_0615_29Feb12.GIF\">0615 UTC<\/a> and from <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/GOES13_BAND4_0632_29Feb12.GIF\">0632 UTC<\/a> show a cold cloud top (brightness temperatures near 210 K or -63\u00c2\u00ba C) passing just north of Lebanon (indicated by the blue square in the imagery). Similarly, GOES-13 enhanced infrared images from <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/GOES13_BAND4_0702_29Feb12.GIF\">0702 UTC<\/a> and <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/GOES13_BAND4_0715_29Feb12.GIF\">0715 UTC<\/a> show cold cloud tops (brightness temperatures around 212 K or -61\u00c2\u00ba C) passing just north of Branson (whose position is also indicated by a blue square). (Click <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/GOES13_BAND4_29Feb12Looping.gif\">Here<\/a> for a loop from 0545 UTC to 0845 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\/2012\/02\/NA_GOES_Sounder_DPI_LI_20120229_Loop_4_7.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-13 Sounder DPI LI\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/NA_GOES_Sounder_DPI_LI_20120229_Loop_4_7.gif\" alt=\"GOES-13 Sounder DPI LI\" width=\"480\" height=\"286\" \/><\/a><p class=\"wp-caption-text\">GOES-13 Sounder DPI LI<\/p><\/div>\n<p>Satellite data gave numerous indications that severe weather was possible at these locations. For example, the Sounder-derived Derived Product Imagery (DPI) Lifted Index at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/NA_GOES_Sounder_DPI_LI_20120229_0400.png\">0400 UTC<\/a> and at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/NA_GOES_Sounder_DPI_LI_20120229_0400.png\">0700 UTC<\/a> (See above for the toggle between the images) shows a tongue of instability &#8212; LIs close to -4 at 0400 UTC and dropping by 0700 UTC &#8212; progressing eastward across Missouri.<\/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\/2012\/02\/NearCast_ted_forecastfor07z_Loop.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"UW CIMSS NearCast Product Valid at 0700 UTC 29 February 2012 (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/nearcast_ted_006fh_01m.gif\" alt=\"UW CIMSS NearCast Product Valid at 0700 UTC 29 February 2012 (click image to play animation)\" width=\"480\" height=\"400\" \/><\/a><p class=\"wp-caption-text\">UW CIMSS NearCast Product Valid at 0700 UTC 29 February 2012<\/p><\/div>\n<p>In addition, the <a href=\"http:\/\/cimss.ssec.wisc.edu\/model\/nrc\/\">UW CIMSS NearCasting product<\/a>, above, which product uses a Lagrangian Model to move three-dimensional sounder information into the future (thereby showing where convective instability will develop) suggested that strong instability would help sustain the development of any thunderstorms over Southwestern Missouri. Each of the forecasts in the linked-to loop above focus the instability over southwest Missouri near Branson. The NearCast product indicates where the greatest instability will be in the near future and therefore serves to enhance situational awareness in a region.<\/p>\n<p style=\"text-align: center;\">___________________________________________________________________________________<\/p>\n<p>As the well-organized <strong><a title=\"GOES-13 IR images with surface frontal analyses\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/120229_g13_ir_fronts_anim.gif\">squall line ahead of the advancing cold front<\/a><\/strong> continued eastward, a tornado which produced the first documented EF4 damage of 2012 moved through the southern part of Harrisburg, Illinois around 10:56 UTC <em>(4:56 am local time)<\/em>. This tornado was also responsible for 6 deaths (<strong><a title=\"NWS Paducah KY Public Information Statement\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/120229_pah_pns.text\">NWS Paducah KY Public Information Statement<\/a><\/strong>). See the <strong><a title=\"WeatherMatrix Blog\" href=\"http:\/\/www.accuweather.com\/en\/weather-blogs\/weathermatrix\/800mile-supercell-drops-multiple-tornadoes\/62234\">WeatherMatrix Blog<\/a><\/strong> for a detailed radar-based discussion of this event.<\/p>\n<p>An AWIPS image of 1-km resolution POES AVHRR 10.8 \u00c2\u00b5m IR data at 11:03 UTC <em>(shortly after the tornado moved through Harrisburg IL)<\/em> with overlays of severe storm reports <strong><em>(below)<\/em><\/strong> shows that the Harrisburg supercell produced hail up to 2.50 inches in diameter and a number of damaging wind reports between 09:41 UTC and 10:56 UTC as it moved northeastward from far eastern Missouri across southern Illinois.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/120229_poes_avhrr_ir_severe_reports_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"POES AVHRR 10.8 \u00c2\u00b5m IR image + Hail, Severe Wind Gust, and Tornado reports\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/120229_poes_avhrr_ir_severe_reports_anim.gif\" alt=\"POES AVHRR 10.8 \u00c2\u00b5m IR image + Hail, Severe Wind Gust, and Tornado reports\" width=\"480\" height=\"400\" \/><\/a><p class=\"wp-caption-text\">POES AVHRR 10.8 \u00c2\u00b5m IR image + Hail, Severe Wind Gust, and Tornado reports<\/p><\/div>\n<p>As seen in the 1-km resolution POES AVHRR image comparison below, along the pre-frontal squall line the 10.8 \u00c2\u00b5m cloud top IR brightness temperatures were as cold as -73\u00c2\u00ba C <em>(darker black color enhancement in the IR image),<\/em> cloud top heights were as high as 12 km <em>(darker green on the Cloud Top Height product),<\/em> and a large area of cloud tops was designated as &#8220;Overshooting&#8221; the tropopause <em>(violet on the Cloud Type product)<\/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\/2012\/02\/120229_poes_avhrr_ir_hgt_type_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"POES AVHRR 10.8 \u00c2\u00b5m IR image + Cloud Top Height, and Cloud Type products\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/120229_poes_avhrr_ir_hgt_type_anim.gif\" alt=\"POES AVHRR 10.8 \u00c2\u00b5m IR image + Cloud Top Height, and Cloud Type products\" width=\"480\" height=\"400\" \/><\/a><p class=\"wp-caption-text\">POES AVHRR 10.8 \u00c2\u00b5m IR image + Cloud Top Height, and Cloud Type products<\/p><\/div>\n<p>A sequence of 4-km resolution GOES-13 10.7 \u00c2\u00b5m IR images with an overlay of Automated Overshooting Tops Detection <strong><em>(below)<\/em><\/strong> showed an overshooting top associated with the supercell at 10.15 UTC over southern Illinois &#8212; nearly 45 minutes before the tornado moved through Harrisburg <em>(station identifier KHSB)<\/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\/2012\/02\/120229_g13_ir_overshooting_tops_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-13 10.7 \u00c2\u00b5m IR images + Overshooting Top Detection\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/02\/120229_g13_ir_overshooting_tops_anim.gif\" alt=\"GOES-13 10.7 \u00c2\u00b5m IR images + Overshooting Top Detection\" width=\"480\" height=\"400\" \/><\/a><p class=\"wp-caption-text\">GOES-13 10.7 \u00c2\u00b5m IR images + Overshooting Top Detection<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>Severe thunderstorms during the early morning hours of February 29th, 2012 produced several tornadoes over Missouri, including one near Branson, and one near Lebanon. (Annotated SPC storm report map here, originally from here) The GOES-13 enhanced infrared images from 0615 UTC and from 0632 UTC show a cold cloud top (brightness temperatures near 210 K [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[22,10,15,11,26,3],"tags":[],"class_list":["post-9839","post","type-post","status-publish","format-standard","hentry","category-avhrr","category-general-interpretation","category-goes-sounder","category-goes-13","category-poes","category-severe-convection"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/9839","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\/19"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=9839"}],"version-history":[{"count":34,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/9839\/revisions"}],"predecessor-version":[{"id":9855,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/9839\/revisions\/9855"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=9839"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=9839"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=9839"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}