{"id":55891,"date":"2023-12-09T23:02:00","date_gmt":"2023-12-09T23:02:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=55891"},"modified":"2023-12-15T17:46:50","modified_gmt":"2023-12-15T17:46:50","slug":"severe-thunderstorms-across-the-mid-south-and-deep-south","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/55891","title":{"rendered":"30-second imagery of severe thunderstorms across the Mid-South and Deep South"},"content":{"rendered":"<p><div style=\"width: 1292px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_goes16_30second_visible_infrared_spcStormReports_Clarksville_TN_tornado_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/G16_VIS_TN_SPC_09DEC2023_B213_2023343_194325_0002PANELS_FRAME00044.GIF\" alt=\"\" width=\"1282\" height=\"964\" \/><\/a><p class=\"wp-caption-text\">30-second GOES-16 \u201cRed\u201d Visible (0.64 \u00b5m, top) and \u201cClean\u201d Infrared Window (10.3 \u00b5m, bottom) images, with time-matched (+\/- 3 minutes) plots of SPC Storm Reports, from 1900 UTC to 2013 UTC on 09 December [click to play animated GIF |\u00a0<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_goes16_30second_visible_infrared_spcStormReports_Clarksville_TN_tornado_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Overlapping 1-minute <a href=\"https:\/\/www.nco.ncep.noaa.gov\/status\/satellite\/\"><strong>Mesoscale Domain Sectors<\/strong><\/a> from GOES-16 <em>(GOES-East)<\/em> provided imagery at 30-second intervals during an outbreak of severe thunderstorms (<a href=\"https:\/\/www.spc.noaa.gov\/climo\/reports\/231209_rpts.html\"><strong>SPC Storm Reports<\/strong><\/a>) across parts of the Mid-South and Deep South on <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20231209.html\"><strong>09 December 2023<\/strong><\/a>. \u201cRed\u201d Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>) and \u201cClean\u201d Infrared Window (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band13.pdf\"><strong>10.3 \u00b5m<\/strong><\/a>) images\u00a0<em><strong>(above)<\/strong><\/em> included time-matched plots of SPC Storm Reports for a\u00a0 thunderstorm that produced a <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231210_kohx_Clarksville_damage_survey.text\"><strong>EF3-rated tornado<\/strong><\/a> which was responsible for 3 deaths and 62 injuries in the Clarksville, Tennessee (KCKV) area. The coldest cloud-top 10.3 \u00b5m infrared\u00a0 brightness temperatures were in the -60 to -65\u00baC range (darker red enhancement).<\/p>\n<p>1-minute GOES-16 Visible and Infrared images with\/without an overlay of <a href=\"https:\/\/www.goes-r.gov\/spacesegment\/glm.html\"><strong>GLM<\/strong><\/a>\u00a0<a href=\"https:\/\/rammb2.cira.colostate.edu\/wp-content\/uploads\/2020\/10\/GLM_Quick_Guide_Gridded_Products_June_2018.pdf\"><strong>Flash Extent Density<\/strong><\/a>\u00a0<em><strong>(below)<\/strong><\/em> showed pulses of cold overshooting tops (brighter white infrared pixels) and brief lightning jumps associated with the Clarksville supercell thunderstorm as it moved across Montgomery County in Tennessee into Todd County in Kentucky.<\/p>\n<p><div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_goes16_visible_infrared_glmFlashExtetDensity_Clarksville_TN_tornado_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/nc3_2p_fed-20231209_194155.png\" width=\"1715\" height=\"828\" \/><\/a><p class=\"wp-caption-text\">1-minute GOES-16 \u201cRed\u201d Visible (0.64 \u00b5m, top) and \u201cClean\u201d Infrared Window (10.3 \u00b5m, bottom) images, with\/without an overlay of GLM Flash Extent Density, from 1900 UTC to 2045 UTC on 09 December [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_goes16_visible_infrared_glmFlashExtetDensity_Clarksville_TN_tornado_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>30-second GOES-16 Infrared images <em><strong>(below)<\/strong><\/em> showed a later thunderstorm that produced a <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231210_kohx_Madison_damage_survey.text\"><strong>EF2-rated tornado<\/strong><\/a> which was responsible for an additional 3 fatalities in Madison, Tennessee (just north of Nashville KBNA).<\/p>\n<p><div style=\"width: 1290px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_goes16_infrared_spcStormReports_BNA_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/G16_IR_TN_SVR_09DEC2023_B13_2023343_224655_GOES-16_0001PANEL_FRAME00094.GIF\" width=\"1280\" height=\"960\" \/><\/a><p class=\"wp-caption-text\">30-second GOES-16 \u201cClean\u201d Infrared Window (10.3 \u00b5m) images, with time-matched (+\/- 3 minutes) plots of SPC Storm Reports, from 2200 UTC to 2320 UTC on 09 December [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_goes16_infrared_spcStormReports_BNA_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>1-minute GOES-16 Infrared images with\/without an overlay of GLM Flash Extent Density <em><strong>(below)<\/strong><\/em> showed lightning activity associated with the thunderstorm that produced the Madison tornado (in Davidson County) &#8212; as with the Clarksville storm, pulses of cold overshooting tops and brief lightning jumps were observed as the tornadic thunderstorm progressed across the area.<\/p>\n<p><div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_goes16_infrared_glmFlashExtetDensity_Madison_TN_tornado_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/tn2_ir_fed-20231209_220355.png\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">1-minute GOES-16 \u201cClean\u201d Infrared Window (10.3 \u00b5m) images, with\/without an overlay of GLM Flash Extent Density, from 2130 UTC to 2330 UTC on 09 December [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_goes16_infrared_glmFlashExtetDensity_Madison_TN_tornado_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Cursor sampling of 2-km resolution GOES-16 10.3 \u00b5m brightness temperature along with the operational Cloud Top Temperature and <a href=\"http:\/\/cimss.ssec.wisc.edu\/clavrx\/documentation.html\"><strong>CLAVR-x<\/strong><\/a> Cloud Top Height derived products for the Clarksville TN tornadic thunderstorm and the Madison TN tornadic thunderstorm <em><strong>(below)<\/strong><\/em> indicated that Cloud Top Temperatures were in the -65 to -66\u00b0C range, with Cloud Top Heights in the 43000-45000 ft range (the CLAVR-x Cloud Top Height product was shown here, since its 2-km resolution was superior to the legacy 10-km resolution Cloud Top Height product currently available in AWIPS).<\/p>\n<p><div style=\"width: 1926px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_1932utc_goes16_visible_infrared_clavrxCloudTopHeight_cloudTopTemperature_cursor_sample.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_1932utc_goes16_visible_infrared_clavrxCloudTopHeight_cloudTopTemperature_cursor_sample.png\" width=\"1916\" height=\"968\" \/><\/a><p class=\"wp-caption-text\">Cursor sample of GOES-16 10.3 \u00b5m brightness temperature, Cloud Top Temperature derived product and CLAVR-x Cloud Top Height derived product for the Clarksville TN tornadic thunderstorm at 1932 UTC on 09 December [click to enlarge]<\/p><\/div><br \/>\n<div style=\"width: 1926px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_2201utc_goes16_infrared_cloudTopTemperature_clavrxCloudTopHeight_TN.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_2201utc_goes16_infrared_cloudTopTemperature_clavrxCloudTopHeight_TN.png\" width=\"1916\" height=\"968\" \/><\/a><p class=\"wp-caption-text\">Cursor sample of GOES-16 10.3 \u00b5m brightness temperature, Cloud Top Temperature derived product and CLAVR-x Cloud Top Height derived product for the Madison TN tornadic thunderstorm at 2201 UTC on 09 December [click to enlarge]<\/p><\/div>Those GOES-16 Cloud Top Temperature and Cloud Top Height values were a bit colder\/higher than the Most Unstable air parcel Maximum Parcel Level (MU MPL) calculated using rawinsonde data from Nashville, Tennessee rawinsonde data at 1200 UTC on 09 December, shown below (<a href=\"https:\/\/www.spc.noaa.gov\/exper\/soundings\/\"><strong>source<\/strong><\/a>). Unfortunately, a 0000 UTC \/ 10 December Nashville rawinsonde report was not available.<\/p>\n<p><div style=\"width: 1194px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_1200utc_kbna_raob.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_1200utc_kbna_raob.png\" width=\"1184\" height=\"838\" \/><\/a><p class=\"wp-caption-text\">Plot of Nashville, Tennessee rawinsonde data at 1200 UTC on 09 December [click to enlarge]<\/p><\/div>A larger-scale view of 30-second GOES-16 Infrared imagery is shown below, spanning the ~13-hour period from 1900 UTC on 09 December to 0752 UTC on 10 December &#8212; which depicted more of the nighttime SPC Storm Reports across parts of northern Mississippi, Alabama and Georgia.<\/p>\n<p><div style=\"width: 1290px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_goes16_infrared_spcStormReports_anim.mp4\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/G16_IR_SOUTH_SVR_09DEC2023_B13_2023343_230955_GOES-16_0001PANEL_FRAME00500.GIF\" width=\"1280\" height=\"1280\" \/><\/a><p class=\"wp-caption-text\">30-second GOES-16 \u201cClean\u201d Infrared Window (10.3 \u00b5m) images, with time-matched (+\/- 3 minutes) plots of SPC Storm Reports, from 1900 UTC to 0752 UTC on 10 December [click to play MP4 animation]<\/p><\/div>Many of these severe thunderstorms were developing within a corridor of moisture and instability ahead of an advancing cold front, as seen in 5-minute GOES-16 Visible images combined with <a href=\"https:\/\/rammb2.cira.colostate.edu\/wp-content\/uploads\/2020\/01\/QuickGuide_TPW_20180306-1.pdf\"><strong>Total Precipitable Water<\/strong><\/a> and Lifted Index \/ CAPE <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_BaselineDerivedStabilityIndices.pdf\"><strong>Derived Stability Indices<\/strong><\/a> in cloud-free skies <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_goes16_totalPrecpitableWater_liftedIndex_convectiveAvailablePotentialEnergy_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/sus_vis_cape-20231209_200117.png\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">5-minute GOES-16 Visible images, combined with Total Precipitable Water, Lifted Index and CAPE derived products (in cloud-free skies) [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/12\/231209_goes16_totalPrecpitableWater_liftedIndex_convectiveAvailablePotentialEnergy_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>Overlapping 1-minute Mesoscale Domain Sectors from GOES-16 (GOES-East) provided imagery at 30-second intervals during an outbreak of severe thunderstorms (SPC Storm Reports) across parts of the Mid-South and Deep South on 09 December 2023. \u201cRed\u201d Visible (0.64 \u00b5m) and \u201cClean\u201d Infrared Window (10.3 \u00b5m) images\u00a0(above) included time-matched plots of SPC Storm Reports for a\u00a0 thunderstorm [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":55900,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[63,76,74,30,3],"tags":[],"class_list":["post-55891","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-clavrx","category-glm","category-goes-16","category-lightning","category-severe-convection"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/55891","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=55891"}],"version-history":[{"count":35,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/55891\/revisions"}],"predecessor-version":[{"id":56001,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/55891\/revisions\/56001"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/55900"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=55891"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=55891"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=55891"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}