{"id":36408,"date":"2020-04-26T17:59:59","date_gmt":"2020-04-26T17:59:59","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=36408"},"modified":"2020-04-28T02:26:24","modified_gmt":"2020-04-28T02:26:24","slug":"prolific-lightning-producing-mcs-in-mexico","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/36408","title":{"rendered":"Prolific lightning-producing MCS in eastern Mexico"},"content":{"rendered":"<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200425_200426_goes16_infrared_glmGroups_Mexico_mcs_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/G16_IR_GLM_MEXICO_25APR2020_B13_2020117_042112_GOES-16_0001PANEL_FRAME00101.GIF\" alt=\"GOES-16 \" width=\"642\" height=\"482\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Clean&#8221; Infrared Window <em>(10.35 \u00b5m)<\/em> images, with and without GLM Groups plotted in cyan [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200425_200426_goes16_infrared_glmGroups_Mexico_mcs_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-16 <em>(GOES- East)<\/em> &#8220;Clean&#8221; Infrared Window (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band13.pdf\"><strong>10.35 \u00b5m<\/strong><\/a>) images, with and without plots of <a href=\"https:\/\/www.goes-r.gov\/spacesegment\/glm.html\"><strong>GLM<\/strong><\/a> Groups<em><strong> (above)<\/strong><\/em> showed a Mesoscale Convective System (MCS) that was propagating southward across eastern Mexico (in advance of an approaching <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200425_200426_surface_analyses_Mexico_anim.gif\"><strong>cold front<\/strong><\/a>) from 2001 UTC on 25 April to 1501 UTC on 26 April 2020. The coldest cloud-top infrared brightness temperatures were -90\u00baC <em>(yellow pixels embedded within dark purple regions)<\/em>. This MCS was prolific lightning-producer &#8212; which included numerous anvil streamers that extended well east and northeast of the main convective core <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200426_0421utc_goes16_infrared_glmGroups_Mexico_mcs_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200426_0421utc_goes16_infrared_glmGroups_Mexico_mcs_anim.gif\" alt=\"GOES-16 &quot;Clean&quot; Infrared Window (10.35 \u00b5m) images, with and without GLM Groups plotted in cyan, at 0421 UTC on 26 April [click to enlarge]\" width=\"641\" height=\"481\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Clean&#8221; Infrared Window<em> (10.35 \u00b5m)<\/em> images, with and without GLM Groups plotted in cyan, at 0421 UTC on 26 April [click to enlarge]<\/p><\/div>A toggle between NOAA-20 VIIRS Infrared Window (11.45 \u00b5m) and Day\/Night Band (0.7 \u00b5m) images at 0841 UTC<strong><em> (below)<\/em><\/strong> also revealed isolated pixels in the overshooting top region with brightness temperatures of -90\u00baC <em>(yellow enhancement)<\/em> &#8212; along with numerous bright lightning streaks in the Day\/Night Band image, located well east of the convective core (consistent with the <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200426_0841utc_goes16_infrared_glmGroups_Mexico_mcs_anim.gif\"><strong>GOES&#8211;16 GLM imagery<\/strong><\/a>). At that time, the core of the MCS was located just off the coast of Mexico, between Poza Rica (MMPA) and Veracruz (MMVR).<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200426_0841utc_noaa20_viirs_infrared_dayNightBand_Mexico_mcs_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200426_0841utc_noaa20_viirs_infrared_dayNightBand_Mexico_mcs_anim.gif\" alt=\"NOAA-20 VIIRS Infrared Window (11.45 \u00b5m) and Day\/Night Band (0.7 \u00b5m) images at 0841 UTC [click to enlarge]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">NOAA-20 VIIRS Infrared Window <em>(11.45 \u00b5m)<\/em> and Day\/Night Band <em>(0.7 \u00b5m)<\/em> images at 0841 UTC [click to enlarge]<\/p><\/div>Plots of <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200425_200426_MMVR_RAOB_DATA.TEXT\"><strong>rawinsonde data<\/strong><\/a> from Veracruz, Mexico <em><strong>(below)<\/strong><\/em> showed that the coldest tropopause temperatures were -78.1\u00baC at a pressure level of 103 hPa &#8212; so the coldest GOES-16 and NOAA-20 infrared brightness temperatures of -90\u00baC indicated overshooting tops extending well about the tropopause.<\/p>\n<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200425_20426_MMVR_RAOBS.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200425_20426_MMVR_RAOBS.GIF\" alt=\"Plots of rawinsonde data from Veracruz, Mexico [click to enlarge]\" width=\"643\" height=\"483\" \/><\/a><p class=\"wp-caption-text\">Plots of rawinsonde data from Veracruz, Mexico [click to enlarge]<\/p><\/div>On 25 April, GOES-16 True Color Red-Green-Blue (RGB) images created using <a href=\"http:\/\/cimss.ssec.wisc.edu\/csppgeo\/geo2grid_v1.0.0.html\"><strong>Geo2Grid<\/strong><\/a> <em><strong>(below)<\/strong><\/em> portrayed a well-defined rope cloud with an undular bore along the cold frontal boundary. Also evident was widespread dense smoke across much of the Gulf of Mexico, a result of prolonged <strong><a href=\"https:\/\/yucatanexpatlife.com\/fires-consume-7062-hectares-of-green-areas-in-yucatan\/\">fire activity<\/a><\/strong> in the Yucatan Peninsula of Mexico and parts of Central America.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200425_goes16_trueColorRGB_Gulf_of_Mexico_frontal_bore_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/GOES-16_ABI_RadF_true_color_2020116_132016Z.png\" alt=\"GOES-16 True Color RGB images [click to play animation | MP4]\" width=\"641\" height=\"641\" \/><\/a><p class=\"wp-caption-text\">GOES-16 True Color RGB images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200425_goes16_trueColorRGB_Gulf_of_Mexico_frontal_bore_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div><center><\/p>\n<blockquote class=\"twitter-tweet\">\n<p dir=\"ltr\" lang=\"en\">So after breaking the <a href=\"https:\/\/twitter.com\/hashtag\/lightning?src=hash&amp;ref_src=twsrc%5Etfw\">#lightning<\/a> archive tool a few times (because of searching a time period with too much lightning)&#8230;I&#8217;ve counted up the dots between 2000 UTC 25 April and 1500 UTC 26 April. 1.1 million! <a href=\"https:\/\/t.co\/yQrmbONPQ0\">https:\/\/t.co\/yQrmbONPQ0<\/a> <a href=\"https:\/\/t.co\/K0eedrOAdC\">pic.twitter.com\/K0eedrOAdC<\/a><\/p>\n<p>\u2014 Ch?is Vagas|?y (@COweatherman) <a href=\"https:\/\/twitter.com\/COweatherman\/status\/1254444705011523585?ref_src=twsrc%5Etfw\">April 26, 2020<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><br \/>\n<\/center><\/p>\n","protected":false},"excerpt":{"rendered":"<p>GOES-16 (GOES- East) &#8220;Clean&#8221; Infrared Window (10.35 \u00b5m) images, with and without plots of GLM Groups (above) showed a Mesoscale Convective System (MCS) that was propagating southward across eastern Mexico (in advance of an approaching cold front) from 2001 UTC on 25 April to 1501 UTC on 26 April 2020. The coldest cloud-top infrared brightness [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":36411,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[76,74,30,78,45,48],"tags":[],"class_list":["post-36408","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-glm","category-goes-16","category-lightning","category-noaa-20","category-redgreenblue-rgb-images","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/36408","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=36408"}],"version-history":[{"count":8,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/36408\/revisions"}],"predecessor-version":[{"id":36429,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/36408\/revisions\/36429"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/36411"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=36408"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=36408"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=36408"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}