{"id":59859,"date":"2024-06-11T23:59:00","date_gmt":"2024-06-11T23:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=59859"},"modified":"2024-06-14T17:45:48","modified_gmt":"2024-06-14T17:45:48","slug":"record-1-hour-rainfall-accumulation-at-sarasota-florida","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/59859","title":{"rendered":"Record 1-hour rainfall accumulation at Sarasota, Florida"},"content":{"rendered":"<p><div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/240611_goes16_infrared_FL_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/fl_ir-20240611_231117.png\" alt=\"\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">5-minute GOES-16 \u201cClean\u201d Infrared Window (10.3 \u00b5m) images, from 2001 UTC on 11 June to 0101 UTC on 12 June; KSRQ denotes the location of Sarasota\/Bradenton International Airport [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/240611_goes16_infrared_FL_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>5-minute CONUS Sector GOES-16 <em>(GOES-East)<\/em>\u00a0\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> displayed areas of convection that moved inland along the west coast of Florida on <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20240611.html\"><strong>11 June 2024<\/strong><\/a>. Sarasota\/Bradenton International Airport received very heavy rainfall (3.93 inches) during the 1-hour period ending at 2353 UTC or 7:53 PM local time (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/240611_ksrq_metars.png\"><strong>METARs<\/strong><\/a>\u00a0|\u00a0<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/240611_ksrq_obs.png\"><strong>decoded surface reports<\/strong><\/a> | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/240611_KSRQ_SFCMG.GIF\"><strong>plot of surface report data<\/strong><\/a>) &#8212; which was a new record maximum 1-hour rainfall accumulation for that location (contributing to their <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/240611_ktbw_rer.text\"><strong>record daily rainfall of 6.26 inches<\/strong><\/a>).<\/p>\n<p>A GOES-16 Infrared image showing a cold thunderstorm overshooting top at 2311 UTC <strong><em>(below)<\/em><\/strong> included a cursor sample of the associated GOES-16 <a href=\"https:\/\/weather.ndc.nasa.gov\/sport\/training\/nesdisGoesrQpe\/QPE%20Quick%20Guide%20-%20NASA%20SPoRT.pdf\"><strong>Rain Rate<\/strong><\/a> derived product &#8212; which was 3.17 in\/hr, compared to the 3.93 in observed at Sarasota\/Bradenton for the hour ending at 2353 UTC. Note that the cold overshooting top and high rain rate were displaced about 6 mi northwest of KSRQ &#8212; for a <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/240611_2311utc_goes16_infrared_cloudTopHeight_rainRate_FL.png\"><strong>Cloud Top Height<\/strong><\/a> around 50 kft, this is consistent with the <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/webapps\/parallax\/overview.html\"><strong>parallax<\/strong><\/a> adjustment of <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/parallax_goes16_50kft_FL.png\"><strong>~10 km<\/strong><\/a> with GOES-East imagery over Florida.<\/p>\n<p><div style=\"width: 1926px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/240611_2311utc_goes16_infrared_rainRate_FL.png\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/240611_2311utc_goes16_infrared_rainRate_FL.png\" alt=\"\" width=\"1916\" height=\"968\" \/><\/a><p class=\"wp-caption-text\">GOES-16 \u201cClean\u201d Infrared Window (10.3 \u00b5m) image showing a cold thunderstorm overshooting top at 2311 UTC on 11 June, which included a cursor sample of the associated GOES-16 Rain Rate (cyan) derived product [click to enlarge]<\/p><\/div>GOES-16 Infrared images with 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 the lightning activity associated with these thunderstorms, which included a few brief lightning jumps (most notably near Bradenton at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/fl_ir_glm-20240611_231617.png\"><strong>2316 UTC<\/strong><\/a>, 5 minutes after the peak GOES-16 Rain Rate).<\/p>\n<p><div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/240611_goes16_infrared_glmFlashExtentDensity_FL_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/fl_ir_glm-20240611_231617.png\" alt=\"\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">5-minute GOES-16 \u201cClean\u201d Infrared Window (10.3 \u00b5m) images, with an overlay of GLM Flash Extent Density, from 2001 UTC on 11 June to 0101 UTC on 12 June [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/240611_goes16_infrared_glmFlashExtentDensity_FL_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>5-minute GOES-16 Visible images <em><strong>(below)<\/strong><\/em> also depicted many of the thunderstorm overshooting tops &#8212; but also showed the offshore cyclonic circulation of low-level clouds associated with Tropical Invest 90L (what role 90L may have played in helping to force the development of the heavy-rainfall-producing thunderstorms is not known).<\/p>\n<div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/240611_goes16_visible_FL_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/fl_vis-20240611_231117.png\" alt=\"\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">5-minute GOES-16 \u201cRed\u201d Visible (0.64 \u00b5m) images, from 2001 UTC on 11 June to 0011 UTC on 12 June; KSRQ denotes the location of Sarasota\/Bradenton International Airport [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/06\/240611_goes16_visible_FL_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>5-minute CONUS Sector GOES-16 (GOES-East)\u00a0\u201cClean\u201d Infrared Window (10.3 \u00b5m) images\u00a0(above) displayed areas of convection that moved inland along the west coast of Florida on 11 June 2024. Sarasota\/Bradenton International Airport received very heavy rainfall (3.93 inches) during the 1-hour period ending at 2353 UTC or 7:53 PM local time (METARs\u00a0|\u00a0decoded surface reports | plot of [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":59884,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[76,74,16,151,30],"tags":[],"class_list":["post-59859","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-glm","category-goes-16","category-heavy-rain-flooding","category-l2_readouts","category-lightning"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/59859","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=59859"}],"version-history":[{"count":31,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/59859\/revisions"}],"predecessor-version":[{"id":59893,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/59859\/revisions\/59893"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/59884"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=59859"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=59859"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=59859"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}