{"id":27132,"date":"2018-02-24T23:59:23","date_gmt":"2018-02-24T23:59:23","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=27132"},"modified":"2018-02-26T21:15:56","modified_gmt":"2018-02-26T21:15:56","slug":"severe-weather-in-the-mid-south-and-heavy-snow-in-the-upper-midwest","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/27132","title":{"rendered":"Severe weather in the Mid-South, and heavy snow in the Upper Midwest"},"content":{"rendered":"<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/180224_goes16_water_vapor_surface_weather_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/G16_WV9_24FEB20189_960x1280_B9_2018055_210039_0001PANEL_00025.GIF\" alt=\"GOES-16 Mid-level Water Vapor (6.9 \u00b5m), with hourly plots of surface weather type [click to play Animated GIF | MP4 also available]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Mid-level Water Vapor <em>(6.9 \u00b5m)<\/em> images, with hourly plots of surface weather type [click to play Animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/180224_goes16_water_vapor_surface_weather_anim.mp4\"><strong>MP4<\/strong><\/a> also available]<\/p><\/div>GOES-16 <em>(GOES-East)<\/em> Mid-level Water Vapor (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band09.pdf\"><strong>6.9 \u00b5m<\/strong><\/a>) images <em><strong>(above)<\/strong><\/em> showed the flow of moisture from the lower Mississippi Valley into the Ohio Valley on <a href=\"http:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20180224.html\"><strong>24 February 2018<\/strong><\/a> &#8212; this fueled the development of flooding rainfall and <a href=\"http:\/\/www.spc.noaa.gov\/climo\/reports\/180224_rpts.html\"><strong>severe thunderstorms<\/strong><\/a> (for more details, see the <a href=\"https:\/\/satelliteliaisonblog.com\/2018\/02\/25\/24-feb-2018-southeast-us-heavy-rain\/\"><strong>Satellite Liaison Blog<\/strong><\/a>). A special <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/180224_21UTC_KLZK_RAOB.GIF\"><strong>21 UTC sounding<\/strong><\/a> from Little Rock AR indicated 37.3 mm or 1.47 inches of Total Precipitable Water (TPW) within the atmospheric column.<\/p>\n<p>1-minute interval <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/23225\">Mesoscale Sector<\/a><\/strong> GOES-16 &#8220;Red&#8221; Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>) and &#8220;Clean&#8221; Infrared Window (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band13.pdf\"><strong>10.3 \u00b5m<\/strong><\/a>) images<em><strong> (below)<\/strong> <\/em>revealed the development of a small supercell thunderstorm just north of the Kentucky\/Tennessee border &#8212; this storm produced an EF-2\u00a0 tornado that was responsible for 1 fatality (<a href=\"http:\/\/www.weather.gov\/lmk\/SevereWeatherFloodingFebruary24-252018\"><strong>NWS Louisville damage survey<\/strong><\/a>). This (along with another in Arkansas) was the first US tornado-related death in 283 days (a new record in terms of length), with the last occurring in Wisconsin on <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/23962\"><strong>16 May 2017<\/strong><\/a>.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/180224_goes16_visible_infrared_spc_storm_reports_KY_TN_severe_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/958x638_AGOES16_B213_G16_VIS_IR_MESO_TN_KY_SVR_24FEB2018_2018055_220658_0002PANELS.GIF\" alt=\"GOES-16 &quot;Red&quot; Visible&lt;em&gt; (0.64 \u00b5m, left)&lt;\/em&gt; and &quot;Clean&quot; Infrared Window &lt;em&gt;(10.3 \u00b5m, right)&lt;\/em&gt; images, with hourly surface reports plotted in yellow and SPC storm reports plotted in red [click to play Animated GIF | &lt;a href=&quot;https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/180224_goes16_visible_infrared_spc_storm_reports_KY_TN_severe_anim.mp4&quot;&gt;&lt;strong&gt;MP4&lt;\/strong&gt;&lt;\/a&gt; also available]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible<em> (0.64 \u00b5m, left)<\/em> and &#8220;Clean&#8221; Infrared Window <em>(10.3 \u00b5m, right)<\/em> images, with hourly surface reports plotted in yellow and SPC storm reports plotted in red [click to play Animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/180224_goes16_visible_infrared_spc_storm_reports_KY_TN_severe_anim.mp4\"><strong>MP4<\/strong><\/a> also available]<\/p><\/div>Farther to the north, bands of elevated convection (oriented generally west to east) developed across Minnesota and Wisconsin, as seen in GOES-16 Visible (0.64 \u00b5m) and Infrared Window (10.3 \u00b5m) images <em><strong>(below)<\/strong><\/em>. Snowfall rates were 1-2 inches per hour at some locations, with many <a href=\"https:\/\/www.weather.gov\/mpx\/24Feb2018HeavySnow\"><strong>storm total accumulations<\/strong><\/a> of 7 to 9 inches. Note the small-scale &#8220;ripple structure&#8221; that was present along the tops of many of these convective bands (orthogonal to the long axis of each band).<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/180224_goes16_visible_MN_WI_banding_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/G16_visible_banding-20180224_213220.png\" alt=\"GOES-16 \" width=\"640\" height=\"349\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible (0\/64 \u00b5m) images [click to play animation]<\/p><\/div><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/180224_goes16_infrared_MN_WI_banding_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/G16_infrared_banding-20180224_213220.png\" alt=\"GOES-16 \" width=\"640\" height=\"349\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Clean &#8221; Infrared Widow (10.3 \u00b5m) images [click to play animation]<\/p><\/div>Comparisons of Terra and Aqua MODIS Visible (0.65 \u00b5m) and Infrared Window (11.0 \u00b5m) images <em><strong>(below)<\/strong><\/em> also showed these bands of elevated convection that helped to enhance snowfall rates. The layer of instability aloft was evident on the <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/180224_KMPX_RAOBS.GIF\"><strong>00 UTC sounding<\/strong><\/a> from Chanhassen MN.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/180224_1720utc_terra_modis_visible_infrared_MN_WI_banding_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/180224_1720utc_terra_modis_visible_infrared_MN_WI_banding_anim.gif\" alt=\"Terra MODIS Visible (0.65 \u00b5m) and Infrared Window (11.0 \u00b5m) images [click to enlarge]\" width=\"640\" height=\"426\" \/><\/a><p class=\"wp-caption-text\">Terra MODIS Visible (0.65 \u00b5m) and Infrared Window (11.0 \u00b5m) images [click to enlarge]<\/p><\/div><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/180224_1901utc_aqua_modis_visible_infrared_MN_WI_banding_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/02\/180224_1901utc_aqua_modis_visible_infrared_MN_WI_banding_anim.gif\" alt=\"Aqua MODIS Visible (0.65 \u00b5m) and Infrared Window (11.0 \u00b5m) images [click to enlarge]\" width=\"640\" height=\"426\" \/><\/a><p class=\"wp-caption-text\">Aqua MODIS Visible (0.65 \u00b5m) and Infrared Window (11.0 \u00b5m) images [click to enlarge]<\/p><\/div><\/p>\n","protected":false},"excerpt":{"rendered":"<p>GOES-16 (GOES-East) Mid-level Water Vapor (6.9 \u00b5m) images (above) showed the flow of moisture from the lower Mississippi Valley into the Ohio Valley on 24 February 2018 &#8212; this fueled the development of flooding rainfall and severe thunderstorms (for more details, see the Satellite Liaison Blog). A special 21 UTC sounding from Little Rock AR [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":27134,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[70,74,12,3,71,5],"tags":[],"class_list":["post-27132","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-aqua","category-goes-16","category-modis","category-severe-convection","category-terra","category-winter-weather"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/27132","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=27132"}],"version-history":[{"count":17,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/27132\/revisions"}],"predecessor-version":[{"id":27152,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/27132\/revisions\/27152"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/27134"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=27132"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=27132"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=27132"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}