{"id":63196,"date":"2025-02-24T22:59:00","date_gmt":"2025-02-24T22:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=63196"},"modified":"2025-02-28T21:40:12","modified_gmt":"2025-02-28T21:40:12","slug":"south-dakotas-first-february-tornado-on-record","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/63196","title":{"rendered":"South Dakota&#8217;s first February tornado on record"},"content":{"rendered":"<p><div style=\"width: 2710px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/02\/250224_g16_vis_ir_fed_SD.mp4\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/02\/250224_2206utc_g16_vis_ir_SD.png\" width=\"2700\" height=\"1664\" \/><\/a><p class=\"wp-caption-text\">5-minute GOES-16 Red Visible (0.64 \u00b5m, left) and Clean Infrared Window (10.3 \u00b5m, right) images, with\/without an overlay of GLM Flash Extent Density, from 2031-2221 UTC on 24 February [click to play MP4 animation]<\/p><\/div>5-minute CONUS Sector GOES-16 <em>(GOES-East)<\/em> Visible and Infrared images <strong><em>(above)<\/em><\/strong> displayed a thunderstorm that was moving southeast from Aberdeen (KABR) to Watertown (KATY) in northeastern South Dakota on <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20250224.html\"><strong>24 February 2025<\/strong><\/a>. While overall <a href=\"https:\/\/www.goes-r.gov\/spacesegment\/glm.html\"><strong>GLM<\/strong><\/a>-detected lightning activity was relatively modest, periodic increases in Flash Extent Density (orange to red pixels) were evident.<\/p>\n<p>A Special Weather Statement was issued for this thunderstorm at 2058 UTC <em><strong>(below)<\/strong><\/em>, advising on its potential to produce 50 mph winds and nickel-size hail. Note the slight northwest displacement of the Flash Extent Density pixels, compared to the thunderstorm overshooting top as seen in GOES-16 Visible and Infrared imagery \u2014 this is because the commonly-used Gridded GLM products (such as Flash Extent Density, Minimum Flash Area and Total Optical Energy) are not corrected for <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/webapps\/parallax\/overview_updated.html\"><strong>parallax<\/strong><\/a>. With this particular low-topped storm, the magnitude of GOES-16 parallax correction would be about <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/02\/goes16_parallax_30kft.png\"><strong>15 km<\/strong><\/a> (9 miles) to the southeast.<\/p>\n<p><div style=\"width: 2710px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/02\/250224_2101z_g16_vis_ir_glm_sps_SD_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/02\/250224_2101z_g16_vis_ir_glm_sps_SD_anim.gif\" width=\"2700\" height=\"1664\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Red Visible (0.64 \u00b5m, left) and Clean Infrared Window (10.3 \u00b5m, right) images at 2101 UTC, with\/without an overlay of a Special Weather Statement polygon and GLM Flash Extent Density [click to enlarge]<\/p><\/div>GOES-19 (Preliminary\/Non-operational) Visible and Infrared images <em><strong>(below)<\/strong><\/em> included a red &#8220;T&#8221; denoting the location of a brief tornado that occurred at 2211 UTC, southeast of Watertown (<a href=\"https:\/\/www.weather.gov\/abr\/FirstFebTornado\"><strong>NWS Aberdeen<\/strong><\/a> | <a href=\"https:\/\/www.spc.noaa.gov\/climo\/reports\/250224_rpts.html\"><strong>SPC Storm Reports<\/strong><\/a>).<\/p>\n<div style=\"width: 1294px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/02\/G19_VIS_IR_SD_SVR_24FEB2025_loop_GOES-19_2025055_210117_2025055_221117.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/02\/G19_VIS_IR_SD_SVR_24FEB2025_B213_2025055_221117_0002PANELS_FRAME00015.GIF\" width=\"1284\" height=\"962\" \/><\/a><p class=\"wp-caption-text\">5-minute GOES-19 Red Visible (0.64 \u00b5m, left) and Clean Infrared Window (10.3 \u00b5m, right) images, from 2101-2211 UTC on 24 February. The location of the 2211 UTC tornado is plotted in red [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/02\/G19_VIS_IR_SD_SVR_24FEB2025_loop_GOES-19_2025055_210117_2025055_221117.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p style=\"text-align: center;\"><strong>_________<\/strong><\/p>\n<p>LightningCast probabilities (<a href=\"https:\/\/cimss.ssec.wisc.edu\/severe_conv\/pltg.html\">source<\/a>), below, from 2042 &#8211; 2232 UTC, showed high probabilities confined to the storm that produced the tornado; those probabilities diminished quickly after the tornado occurred.<\/p>\n<div style=\"width: 580px;\" class=\"wp-video\"><video class=\"wp-video-shortcode\" id=\"video-63196-1\" width=\"580\" height=\"338\" loop preload=\"metadata\" controls=\"controls\"><source type=\"video\/mp4\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/02\/LightningCastRE_SouthDakota24February2024.mp4?_=1\" \/><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/02\/LightningCastRE_SouthDakota24February2024.mp4\">https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2025\/02\/LightningCastRE_SouthDakota24February2024.mp4<\/a><\/video><\/div>\n","protected":false},"excerpt":{"rendered":"<p>5-minute CONUS Sector GOES-16 (GOES-East) Visible and Infrared images (above) displayed a thunderstorm that was moving southeast from Aberdeen (KABR) to Watertown (KATY) in northeastern South Dakota on 24 February 2025. While overall GLM-detected lightning activity was relatively modest, periodic increases in Flash Extent Density (orange to red pixels) were evident. A Special Weather Statement [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":63229,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[76,74,159,30,115,3],"tags":[],"class_list":["post-63196","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-glm","category-goes-16","category-goes-19","category-lightning","category-lightningcast","category-severe-convection"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/63196","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=63196"}],"version-history":[{"count":21,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/63196\/revisions"}],"predecessor-version":[{"id":63271,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/63196\/revisions\/63271"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/63229"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=63196"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=63196"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=63196"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}