{"id":51052,"date":"2023-03-11T23:59:00","date_gmt":"2023-03-11T23:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=51052"},"modified":"2023-03-14T01:35:49","modified_gmt":"2023-03-14T01:35:49","slug":"severe-thunderstorms-in-the-central-valley-of-california","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/51052","title":{"rendered":"Severe thunderstorms in the Central Valley of California"},"content":{"rendered":"<div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230311_goes18_visible_infrared_glmFlashExtentDensity_warnings_CA_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/ca_2p-20230311_225925.png\" width=\"1715\" height=\"828\" \/><\/a><p class=\"wp-caption-text\">GOES-18 \u201cRed\u201d Visible (0.64 \u00b5m, top) and \u201cClean\u201d Infrared Window (10.3 \u00b5m, bottom) images, with and without an overlay of GOES-18 GLM Flash Extent Density [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230311_goes18_visible_infrared_glmFlashExtentDensity_warnings_CA_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p>1-minute Mesoscale Domain Sector GOES-18 <em>(GOES-West)<\/em>\u00a0\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<strong><em>(above)<\/em><\/strong> included an overlay of <a href=\"https:\/\/www.goes-r.gov\/spacesegment\/glm.htmlhttps:\/\/www.goes-r.gov\/spacesegment\/glm.html\"><strong>GLM<\/strong><\/a> Flash Extent Density &#8212; which showed thunderstorms that produced flash flooding, hail and an EF-1 tornado (<a href=\"https:\/\/www.spc.noaa.gov\/climo\/reports\/230311_rpts.html\"><strong>SPC Storm Reports<\/strong><\/a>) in the Central Valley of California on <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20230311.html\"><strong>11 March 2023<\/strong><\/a>. At <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/ca_2p-20230311_223625.png\"><strong>2236 UTC<\/strong><\/a> (1 minute prior to the Tornado Warning being issued), an overshooting top along the Calaveras\/Tuolumne County line exhibited an infrared brightness temperature of -53.3\u00baC &#8212; which roughly corresponded to the altitude of a Most Unstable Maximum Parcel Level (MU MPL) as analyzed from the <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230312_00utc_koak_raob.png\"><strong>0000 UTC Oakland rawinsonde<\/strong><\/a> (<a href=\"https:\/\/www.spc.noaa.gov\/exper\/soundings\/\"><strong>source<\/strong><\/a>).\u00a0 Note that for the relatively low-topped convection over California on this day, the coldest value of the default infrared enhancement was modified to -70\u00baC, to aid in the identification of colder overshooting tops (shades of white embedded within dark black regions). <\/p>\n<p>The corresponding GOES-18 <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_BaselineCloudTopHeight.pdf\"><strong>Cloud Top Height<\/strong><\/a> derived product at 2236 UTC &#8212; just before the issuance of the Tornado Warning &#8212; was around 32,482 feet <em><strong>(below)<\/strong><\/em>. For this storm, the maximum value of the default Cloud Top Height enhancement was set to 35,000 feet.<\/p>\n<div style=\"width: 1550px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230311_2236utc_goes18_cloudTopHeight_infrared_cursor_sample.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230311_2236utc_goes18_cloudTopHeight_infrared_cursor_sample.png\" width=\"1540\" height=\"771\" \/><\/a><p class=\"wp-caption-text\">GOES-18 \u201cRed\u201d Visible image (0.64 \u00b5m, top) and Cloud Top Height derived product (bottom), with cursor sampling of the coldest 10.3 \u00b5m pixel along the Calaveras\/Tuolumne County line at 2336 UTC [click to enlarge]<\/p><\/div>\n<p>During the period leading up to convective initiation of the hail\/tornado-producing thunderstorm, 1-minute GOES-18 Visible and Infrared images <em><strong>(below)<\/strong><\/em>\u00a0include contours of\u00a0<a href=\"https:\/\/cimss.ssec.wisc.edu\/severe_conv\/pltg.html\"><strong>LightningCast<\/strong><\/a> Probability &#8212; a &gt;50% LightningCast Probability (green contour) over western San Joaquin County at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/ca_2p_lcast-20230311_200925.png\"><strong>2009 UTC<\/strong><\/a> provided a 17-minute lead time to the start of a prolonged period of GLM-indicated lightning activity for that storm, which commenced at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/ca_2p_lcast-20230311_202625.png\"><strong>2026 UTC<\/strong><\/a> (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230311_goes18_visible_infrared_glmFlashExtentDensity_CA_anim.gif\"><strong>2000 &#8211; 0100 UTC animation<\/strong><\/a>).<\/p>\n<div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230311_goes18_visible_infrared_glmFlashExtentDensty_lightningCastProbability_CA_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/ca_2p_lcast-20230311_202925.png\" width=\"1715\" height=\"828\" \/><\/a><p class=\"wp-caption-text\">GOES-18 \u201cRed\u201d Visible (0.64 \u00b5m, top) and \u201cClean\u201d Infrared Window (10.3 \u00b5m, bottom) images, with an overlay of GLM Flash Extent Density and contours of LightningCast Probability [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230311_goes18_visible_infrared_glmFlashExtentDensty_lightningCastProbability_CA_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p>These thunderstorms developed in an environment of modest moisture and instability, as shown by 1-minute GOES-18 Visible and Infrared images combined with Total Preciptitable Water (TPW) and Convective Available Potential Energy (CAPE) derived products in cloud-free areas <em><strong>(below)<\/strong><\/em>. Satellite-derived TPW values up to 0.90 inch and CAPE values as high as 400 J\/kg were observed in the general vicinity of the strongest convection. Note that the default enhancements for TPW and CAPE were also modified for use with these particular storms &#8212; the maximum TPW value was set at 1.1 inches, while the maximum CAPE value was set at 500 J\/kg. <\/p>\n<div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230311_goes18_visible_infrared_totalPrecipitableWater_convectiveAvailablePotentialEnergy_CA_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/ca_2p_cape-20230311_225125.png\" alt=\"\" width=\"1715\" height=\"828\" \/><\/a><p class=\"wp-caption-text\">GOES-18 \u201cRed\u201d Visible (0.64 \u00b5m, top) and \u201cClean\u201d Infrared Window (10.3 \u00b5m, bottom) images, combined with Total Preciptitable Water and Convective Available Potential Energy (CAPE) derived products in cloud-free areas [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230311_goes18_visible_infrared_totalPrecipitableWater_convectiveAvailablePotentialEnergy_CA_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n\n\n<figure class=\"wp-block-embed is-type-rich is-provider-twitter wp-block-embed-twitter\"><div class=\"wp-block-embed__wrapper\">\n<blockquote class=\"twitter-tweet\" data-width=\"500\" data-dnt=\"true\"><p lang=\"en\" dir=\"ltr\">We have determined a brief EF-1 tornado touched down 6SW of Tuttletown in Tuolumne County during yesterday&#39;s severe thunderstorms that also produced 1&quot; hail and significant flash flooding.  See map and press release for more info.  <a href=\"https:\/\/twitter.com\/hashtag\/CAwx?src=hash&amp;ref_src=twsrc%5Etfw\">#CAwx<\/a> <a href=\"https:\/\/t.co\/bEHYHzolI4\">pic.twitter.com\/bEHYHzolI4<\/a><\/p>&mdash; NWS Sacramento (@NWSSacramento) <a href=\"https:\/\/twitter.com\/NWSSacramento\/status\/1635014705168416770?ref_src=twsrc%5Etfw\">March 12, 2023<\/a><\/blockquote><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script>\n<\/div><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>1-minute Mesoscale Domain Sector GOES-18 (GOES-West)\u00a0\u201cRed\u201d Visible (0.64 \u00b5m) and \u201cClean\u201d Infrared Window (10.3 \u00b5m) images\u00a0(above) included an overlay of GLM Flash Extent Density &#8212; which showed thunderstorms that produced flash flooding, hail and an EF-1 tornado (SPC Storm Reports) in the Central Valley of California on 11 March 2023. At 2236 UTC (1 minute [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":51055,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[76,114,30,115,3],"tags":[],"class_list":["post-51052","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-glm","category-goes-18","category-lightning","category-lightningcast","category-severe-convection"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/51052","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=51052"}],"version-history":[{"count":20,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/51052\/revisions"}],"predecessor-version":[{"id":51074,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/51052\/revisions\/51074"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/51055"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=51052"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=51052"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=51052"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}