{"id":69351,"date":"2026-03-06T23:59:00","date_gmt":"2026-03-06T23:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=69351"},"modified":"2026-03-10T17:13:02","modified_gmt":"2026-03-10T17:13:02","slug":"tornadoes-responsible-for-fatalities-in-michigan-and-oklahoma","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/69351","title":{"rendered":"Tornadoes responsible for fatalities in Michigan and Oklahoma"},"content":{"rendered":"<p><div style=\"width: 1292px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/G19_VIS_IR_MI_SPC_06MAR2026_loop_GOES-19_2026065_191117_2026065_220117.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/G19_VIS_IR_MI_SPC_06MAR2026_B213_2026065_204617_0002PANELS_FRAME00020.GIF\" width=\"1282\" height=\"964\" \/><\/a><p class=\"wp-caption-text\">5-minute GOES-19 Visible images (0.64 \u00b5m, top) and Infrared images (10.3 \u00b5m, bottom) with SPC Storm Reports in red\/blue, from 1911-2201 UTC on 06 March [click to play animated GIF]<\/p><\/div>5-minute CONUS Sector GOES-19 <em>(GOES-East)<\/em>\u00a0Visible and Infrared images <strong><em>(above)<\/em><\/strong> showed a supercell thunderstorm that developed in northern Indiana and tracked northeast across far southern Lower Michigan on <strong><a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20260306.html\">06 March 2026<\/a><\/strong>. This thunderstorm formed in the vicinity of a warm front (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/260306_surface_analyses_anim.gif\"><strong>surface analyses<\/strong><\/a>) that was moving northward across the region &#8212; surface plots indicated that air temperatures behind the warm front rose into the low-mid 70s F, with dew points in the 60s F. This supercell produced 4 tornadoes (one rated EF0, one rated EF1, one rated EF2 and one rated EF3) that were responsible for 4 fatalities and numerous injuries (<a href=\"https:\/\/www.weather.gov\/iwx\/03062026_LowerMichiganTornadoes\"><strong>NWS ILX summary<\/strong><\/a>).<\/p>\n<p>Note that surface observations at the Three Rivers Municipal Airport (KHAI) ceased after 2035 UTC <em><strong>(below)<\/strong><\/em> &#8212; apparently due a tornado-related power outage (KHAI surface observations resumed 24 hours later).<\/p>\n<p><div style=\"width: 1290px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/260306_KHAI_SFCMG.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/260306_KHAI_SFCMG.GIF\" width=\"1280\" height=\"960\" \/><\/a><p class=\"wp-caption-text\">Plot of surface observation data from Three Rivers Municipal Airport on 06 March [click to enlarge]<\/p><\/div>The ProbSevere <a href=\"https:\/\/cimss.ssec.wisc.edu\/probsevere\/isn\/\"><strong>IntenseStormNet<\/strong><\/a> product <strong><em>(below)<\/em><\/strong>\u00a0began to depict &gt;50% probabilities of intense convection at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/260306_2011utc_g19_ir_glm_isnSample.png\"><strong>2011 UTC<\/strong><\/a> &#8212; the time when cloud-top infrared brightness temperatures were rapidly cooling, <a href=\"https:\/\/www.goes-r.gov\/spacesegment\/glm.html\"><strong>GLM<\/strong><\/a> Flash Extent Density was increasing, and tornadoes were being reported north and northeast of Edwardsburg (<a href=\"https:\/\/www.spc.noaa.gov\/climo\/reports\/260306_rpts.html\"><strong>SPC Storm Reports<\/strong><\/a>).<\/p>\n<div style=\"width: 3004px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/260306_goes19_infrared_glmFlashExtentDensity_intenseStormNet_MI.mp4\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/260306_2046utc_g19_ir_isn.png\" width=\"2994\" height=\"1704\" \/><\/a><p class=\"wp-caption-text\">5-minute GOES-19 Infrared (10.3 \u00b5m) images (with\/without an overlay of GLM Flash Extent Density) which included contours of IntenseStormNet probability and plots of SPC Storm Reports (red=tornado, green=hail, blue=wind), from 2001-2141 UTC on 06 March [click to play MP4 animation]<\/p><\/div>\n<p style=\"text-align: center;\">_____________________________________<\/p>\n<p>Several hours later, 1-minute Mesoscale Domain Sector GOES-19 infrared images <strong><em>(below)<\/em><\/strong> showed a large cluster of supercell thunderstorms over northeast Oklahoma. One of the tornadoes was responsible for 2 fatalities near Beggs OK around <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/G19_IR_OK_SVR_06MAR2026_B13_2026066_011925_GOES-19_0001PANEL_FRAME00080.GIF\"><strong>0119 UTC<\/strong><\/a>.<\/p>\n<p><div style=\"width: 1290px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/G19_IR_OK_SVR_06MAR2026_loop_GOES-19_2026066_000028_2026066_025925.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/G19_IR_OK_SVR_06MAR2026_B13_2026066_011925_GOES-19_0001PANEL_FRAME00080.GIF\" width=\"1280\" height=\"960\" \/><\/a><p class=\"wp-caption-text\">1-minute GOES-19 Clean Infrared Window (10.3 \u00b5m) images, with time-matched (+\/- 3 minutes) SPC Storm Reports plotted in blue, from 0000-0259 UTC on 07 March [click to play animated GIF]<\/p><\/div>Around the time that the northernmost supercell began to produce tornadoes, it exhibited a notable <a href=\"https:\/\/journals.ametsoc.org\/doi\/10.1175\/WAF1022.1\"><strong>Enhanced-V<\/strong><\/a> storm-top signature along with a subtle <a href=\"https:\/\/journals.ametsoc.org\/doi\/abs\/10.1175\/WAF-D-18-0040.1?journalCode=wefo\"><strong>Above-Anvil Cirrus Plume<\/strong><\/a> in GOES-19 Infrared and Visible images, respectively <strong><em>(below)<\/em><\/strong>.<\/p>\n<p><div style=\"width: 1290px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/260307_0000utc_goes19_visible_infrared_OK_enhancedV_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/260307_0000utc_goes19_visible_infrared_OK_enhancedV_anim.gif\" width=\"1280\" height=\"960\" \/><\/a><p class=\"wp-caption-text\">GOES-19 Infrared (10.3 \u00b5m) and Visible (0.64 \u00b5m) images at 0000 UTC on 07 March, showing Enhanced-V and Above-Anvil Cirrus Plume cloud-top signatures over northeast Oklahoma [click to enlarge]<\/p><\/div>1-minute GOES-19 Infrared images with an overlay of GLM Flash Points <em><strong>(below)<\/strong><\/em>\u00a0depicted abundant lightning activity with these storms.<\/p>\n<p><div style=\"width: 3004px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/260306_goes19_infrared_glmFlashPoints_OK.mp4\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/260307_0123utc_g19_ir_glm.png\" width=\"2994\" height=\"1670\" \/><\/a><p class=\"wp-caption-text\">1-minute GOES-19 Infrared (10.3 \u00b5m) images, with an overlay of 1-minute GLM Flash Points in the left panel, from 0001-0500 UTC on 07 March [click to play MP4 animation]<\/p><\/div>The coldest cloud-top infrared brightness temperature associated with these thunderstorms was -66\u00baC &#8212; according to a plot of rawinsonde data from Oklahoma City <em><strong>(below)<\/strong><\/em> that temperature roughly corresponded to a ~2 km overshoot of the Most Unstable (MU) air parcel&#8217;s Equilibrium Level (EL).<\/p>\n<div style=\"width: 2972px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/260307_0000utc_koun_raob.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/03\/260307_0000utc_koun_raob.png\" width=\"2962\" height=\"1666\" \/><\/a><p class=\"wp-caption-text\">Plot of rawinsonde data from Oklahoma City at 0000 UTC on 07 March [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>5-minute CONUS Sector GOES-19 (GOES-East)\u00a0Visible and Infrared images (above) showed a supercell thunderstorm that developed in northern Indiana and tracked northeast across far southern Lower Michigan on 06 March 2026. This thunderstorm formed in the vicinity of a warm front (surface analyses) that was moving northward across the region &#8212; surface plots indicated that air [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":69363,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[76,159,30,59,3],"tags":[],"class_list":["post-69351","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-glm","category-goes-19","category-lightning","category-probsevere","category-severe-convection"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/69351","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=69351"}],"version-history":[{"count":22,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/69351\/revisions"}],"predecessor-version":[{"id":69376,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/69351\/revisions\/69376"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/69363"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=69351"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=69351"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=69351"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}