{"id":35710,"date":"2020-02-14T14:59:04","date_gmt":"2020-02-14T14:59:04","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=35710"},"modified":"2020-02-15T19:16:19","modified_gmt":"2020-02-15T19:16:19","slug":"mesoscale-convective-system-in-argentina-2","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/35710","title":{"rendered":"Mesoscale Convective System in Argentina"},"content":{"rendered":"<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/200214_goes16_infrared_Argentina_mcs_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/G16_IR_ARGENTINA_MCS_14FEB2020_B13_2020045_075002_GOES-16_0001PANEL_FRAME00048.GIF\" alt=\"GOES-16 \" width=\"641\" height=\"481\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Clean&#8221; Infrared Window<em> (10.35 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/200214_goes16_infrared_Argentina_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<em><strong> (above)<\/strong> <\/em>showed a large Mesoscale Convective System (MCS) west of Resistencia (station identifier SARE) in far northern Argentina on 14 February 2020 &#8212; this MCS developed southeast of an area of low pressure that was situated well north of a slow-moving cold front (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/200214_surface_analyses_Argentina_anim.gif\"><strong>surface analyses<\/strong><\/a>). The coldest GOES-16 cloud-top infrared brightness temperature was -94.1\u00baC on the <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/G16_IR_ARGENTINA_MCS_14FEB2020_B13_2020045_075002_GOES-16_0001PANEL_FRAME00048.GIF\"><strong>0750 UTC image<\/strong><\/a>.<\/p>\n<p>VIIRS Infrared Window (11.45 \u00b5m) images from NOAA-20 (at 0452 UTC) and Suomi NPP (at 0541 UTC) as viewed using <a href=\"http:\/\/realearth.ssec.wisc.edu\"><strong>RealEarth<\/strong><\/a><em><strong> (below)<\/strong><\/em> revealed intricate patterns of cloud-top waves and radial banding.<\/p>\n<p><div style=\"width: 654px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/200214_noaa20_suomiNPP_viirs_infrared_Argentina_mcs_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/200214_noaa20_suomiNPP_viirs_infrared_Argentina_mcs_anim.gif\" alt=\"VIIRS Infrared Window (11.45 \u00b5m) images from NOAA-20 (at 0452 UTC) and Suomi NPP (at 0541 UTC) [click to enlarge]\" width=\"644\" height=\"376\" \/><\/a><p class=\"wp-caption-text\">VIIRS Infrared Window<em> (11.45 \u00b5m)<\/em> images from NOAA-20 (at 0452 UTC) and Suomi NPP (at 0541 UTC) [click to enlarge]<\/p><\/div>Plots of available NOAA-20 NUCAPS sounding points are shown below. NUCAPS profiles immediately north and south of the MCS revealed a very moist and unstable atmosphere, with Total Precipitable Water values around 2.4 inches and Most Unstable air parcel Convective Available Potential Energy (CAPE) values of 4500-5200 J\/kg. The red NUCAPS profile dots indicate points where both the infrared and microwave retrievals failed &#8212; these are located within the core of the MCS.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/nucaps_arg-20200214_034135_sounding_points.png\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/nucaps_arg-20200214_034135_sounding_points.png\" alt=\"Plots of available NUCAPS sounding points at 0341 UTC [click to enlarge]\" width=\"641\" height=\"380\" \/><\/a><p class=\"wp-caption-text\">Plots of available NOAA-20 NUCAPS sounding points [click to enlarge]<\/p><\/div><div style=\"width: 654px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/200214_04utc_nucaps_profile_north.png\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/200214_04utc_nucaps_profile_north.png\" alt=\"NUCAPS profile north of the MCS [click to enlarge]\" width=\"644\" height=\"385\" \/><\/a><p class=\"wp-caption-text\">NOAA-20 NUCAPS profile just north of the MCS [click to enlarge]<\/p><\/div><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/200214_0341utc_nucaps_profile_south.png\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/200214_0341utc_nucaps_profile_south.png\" alt=\"NUCAPS profile south of the MCS [click to enlarge]\" width=\"642\" height=\"384\" \/><\/a><p class=\"wp-caption-text\">NOAA-20 NUCAPS profile just south of the MCS [click to enlarge]<\/p><\/div><br \/>\nPlots of <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/200213_200214_SACO_RAOB_DATA.TEXT\"><strong>rawinsonde data<\/strong><\/a> from C\u00f3rdoba, Argentina<em><strong> (below)<\/strong><\/em> &#8212; located not far <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/200214_noaa20_infrared_mcs_Cordoba.png\">southwest of the MCS<\/a><\/strong> &#8212; indicated a tropopause temperature of -74.7\u00baC at an altitude of 16.4 km on 14 February at 12 UTC.<\/p>\n<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/200213_200214_SACO_RAOBS.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/02\/200213_200214_SACO_RAOBS.GIF\" alt=\"Plots of rawinsonde data from C\u00f3rdoba, Argentina [click to enlarge]\" width=\"642\" height=\"482\" \/><\/a><p class=\"wp-caption-text\">Plots of rawinsonde data from C\u00f3rdoba, Argentina [click to enlarge]<\/p><\/div>&nbsp;<br \/>\n<center><\/p>\n<blockquote class=\"twitter-tweet\">\n<p dir=\"ltr\" lang=\"en\">You&#8217;ll have to add one <a href=\"https:\/\/twitter.com\/70_dbz?ref_src=twsrc%5Etfw\">@70_dbz<\/a>&#8230; Here is a MCS over Argentina early this morn (0748 UTC). 18 km deep (according to GPM-DPR), with a -92 degC brightness temperature (according to GOES-16, on NASA Worldview). What. A. Beast. <a href=\"https:\/\/t.co\/KkSVpETkuk\">https:\/\/t.co\/KkSVpETkuk<\/a> <a href=\"https:\/\/t.co\/KJU3jieuCp\">pic.twitter.com\/KJU3jieuCp<\/a><\/p>\n<p>\u2014 Randy Chase (@DopplerChase) <a href=\"https:\/\/twitter.com\/DopplerChase\/status\/1228335285307617281?ref_src=twsrc%5Etfw\">February 14, 2020<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/center><\/p>\n","protected":false},"excerpt":{"rendered":"<p>GOES-16 (GOES-East) &#8220;Clean&#8221; Infrared Window (10.35 \u00b5m) images (above) showed a large Mesoscale Convective System (MCS) west of Resistencia (station identifier SARE) in far northern Argentina on 14 February 2020 &#8212; this MCS developed southeast of an area of low pressure that was situated well north of a slow-moving cold front (surface analyses). The coldest [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":35716,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[74,78,83,53,49,48],"tags":[],"class_list":["post-35710","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-16","category-noaa-20","category-nucaps","category-real-earth","category-suomi_npp","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/35710","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=35710"}],"version-history":[{"count":10,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/35710\/revisions"}],"predecessor-version":[{"id":35721,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/35710\/revisions\/35721"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/35716"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=35710"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=35710"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=35710"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}