{"id":34107,"date":"2019-08-18T21:51:47","date_gmt":"2019-08-18T21:51:47","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=34107"},"modified":"2019-08-27T02:07:25","modified_gmt":"2019-08-27T02:07:25","slug":"pyrocumulonimbus-cloud-in-bolivia","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/34107","title":{"rendered":"Pyrocumulonimbus cloud in Bolivia"},"content":{"rendered":"<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190818_goes16_visible_shortwaveInfrared_longwaveInfraredWindow_Bolivia_pyrocb_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/G16_VIS_SWIR_IR_BOLIVIA_PYROCB_V2_18AUG2019_2019230_180019_GOES-16_0003PANELS.GIF\" alt=\"GOES-16 \" width=\"640\" height=\"571\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible <em>(0.64 \u00b5m, top),<\/em> Shortwave Infrared <em>(3.9 \u00b5m, middle)<\/em> and &#8220;Clean&#8221; Infrared Window <em>(10.35 \u00b5m, bottom)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190818_goes16_visible_shortwaveInfrared_longwaveInfraredWindow_Bolivia_pyrocb_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-16 <em>(GOES-East)<\/em> &#8220;Red&#8221; Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>), Shortwave Infrared (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band07.pdf\"><strong>3.9 \u00b5m<\/strong><\/a>) and &#8220;Clean&#8221; Infrared Window (10.35 \u00b5m) images <em><strong>(above)<\/strong><\/em> showed the formation of a pyrocumulonimbus (pyroCb) cloud over far southeastern Bolivia on 18 August 2019. The small anvil cloud briefly surpassed the -40\u00baC pyroCb threshold from 1800-1820 UTC, attaining a minimum cloud-top infrared brightness temperature of -45.2\u00baC along the Bolivia\/Paraguay border at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/G16_VIS_SWIR_IR_BOLIVIA_PYROCB_V2_18AUG2019_2019230_180019_GOES-16_0003PANELS.GIF\"><strong>1800 UTC<\/strong><\/a>. This pyroCb formed over the hottest southern portion of an elongated fire line, as seen in the Shortwave Infrared imagery.<\/p>\n<p>A 1.5-day animation of GOES-16 Shortwave Infrared images (from 12 UTC on 17 August to 2350 UTC on 18 August) revealed the rapid southeastward run of the fire to the Bolivia\/Paraguay border on 17 August, followed by the eastward expansion of the fire line on 18 August <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190817_190818_goes16_shortwaveInfrared_Bolivia_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/G16_SWIR_18_19AUG2019_2019229_232100_GOES-16_0001PANEL.GIF\" alt=\"GOES-16 Shortwave Infrared (3.9 \u00b5m) images [click to play animation | MP4]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Shortwave Infrared <em>(3.9 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190817_190818_goes16_shortwaveInfrared_Bolivia_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>A toggle between Suomi NPP VIIRS True Color Red-Green-Blue (RGB) and Infrared Window (11.45 \u00b5m) images as viewed using <a href=\"http:\/\/realearth.ssec.wisc.edu\"><strong>RealEarth<\/strong><\/a> <em><strong>(below)<\/strong><\/em> showed the large and dense smoke plume streaming southeastward, with the small pyroCb along the Bolivia\/Paraguay border at 1745 UTC &#8212; the brighter white tops of the pyrocumulus and pyrocumulonimbus clouds reached higher altitudes than the tan-colored smoke plume. The coldest cloud-top infrared brightness temperature was about -55\u00baC <em>(orange enhancement)<\/em>, which corresponded to an altitude around 9 km according to <a href=\"http:\/\/weather.uwyo.edu\/cgi-bin\/sounding?region=samer&amp;TYPE=TEXT%3ALIST&amp;YEAR=2019&amp;MONTH=08&amp;FROM=1812&amp;TO=1900&amp;STNM=83554\"><strong>rawinsonde data<\/strong><\/a> from Corumb\u00e1, Bolivia.<\/p>\n<div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190818_17utc_suomiNPP_viirs_trueColor_infraredWindow_Bolivia_pyrocb_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190818_17utc_suomiNPP_viirs_trueColor_infraredWindow_Bolivia_pyrocb_anim.gif\" alt=\"Suomi NPP VIIRS True Color Red-Green-Blue (RGB) and Infrared Window (11.45 \u00b5m) images [click to enlarge]\" width=\"642\" height=\"385\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS True Color Red-Green-Blue (RGB) and Infrared Window <em>(11.45 \u00b5m)<\/em> images [click to enlarge]<\/p><\/div>\n<p>&nbsp;<\/p>\n<blockquote class=\"twitter-tweet\">\n<p dir=\"ltr\" lang=\"en\">Looking more closely at yesterday&#8217;s smoke over South America, the aerosol index from <a href=\"https:\/\/twitter.com\/hashtag\/NOAA20?src=hash&amp;ref_src=twsrc%5Etfw\">#NOAA20<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/OMPS?src=hash&amp;ref_src=twsrc%5Etfw\">#OMPS<\/a> was in double digits! Values on the right refer to the UTC of the measurements. <a href=\"https:\/\/t.co\/3XBqoEVs4M\">pic.twitter.com\/3XBqoEVs4M<\/a><\/p>\n<p>\u2014 Colin Seftor (@colin_seftor) <a href=\"https:\/\/twitter.com\/colin_seftor\/status\/1163416907933986819?ref_src=twsrc%5Etfw\">August 19, 2019<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<p>Strong northerly to northwesterly surface winds were blowing across the region, in advance of an approaching cold front (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190818_18utc_190819_00utc_surface_analyses_Bolivia_anim.gif\"><strong>surface analyses<\/strong><\/a>) &#8212; at Robore, Bolivia (located just north-northwest of the fires), winds were gusting to 25-28 knots during much of the day <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190818_SLRB_SFCMG.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190818_SLRB_SFCMG.GIF\" alt=\"Time series of surface report data from Robore, Bolivia [click to enlarge]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">Time series of surface report data from Robore, Bolivia [click to enlarge]<\/p><\/div>This is likely the second confirmed case of a South American pyroCb (the first being on <a href=\"http:\/\/pyrocb.ssec.wisc.edu\/archives\/2213\"><strong>29 January 2018<\/strong><\/a>) &#8212; in addition, it&#8217;s the second pyroCb documented in the tropics and the first pyroCb documented during a winter season. Thanks to Mike Fromm (NRL) for bringing this case to our attention!<\/p>\n<p style=\"text-align: center;\"><strong>===== 25 August Update =====<\/strong><\/p>\n<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190825_goes16_visible_shortwaveInfrared_longwaveInfraredWindow_Bolivia_pyrocb_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/G16_VIS_SWIR_IR_BOLIVIA_PYROCB_25AUG2019_2019237_181021_GOES-16_0003PANELS.GIF\" alt=\"GOES-16 \u201cRed\u201d Visible (0.64 \u00b5m, top), Shortwave Infrared (3.9 \u00b5m, middle) and \u201cClean\u201d Infrared Window (10.35 \u00b5m, bottom) images [click to play animation | MP4]\" width=\"642\" height=\"573\" \/><\/a><p class=\"wp-caption-text\">GOES-16 \u201cRed\u201d Visible <em>(0.64 \u00b5m, top),<\/em> Shortwave Infrared<em> (3.9 \u00b5m, middle)<\/em> and \u201cClean\u201d Infrared Window <em>(10.35 \u00b5m, bottom)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190825_goes16_visible_shortwaveInfrared_longwaveInfraredWindow_Bolivia_pyrocb_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-16 Visible, Shortwave Infrared and \u201cClean\u201d Infrared Window images <em><strong>(above)<\/strong><\/em> showed that another pyroCb developed from that same general fire complex, southwest of Robore, Bolivia (SLRB), on 25 August.<\/p>\n<p>A toggle between Suomi NPP and NOAA-20 VIIRS True Color RGB and Infrared Window images as viewed using <a href=\"http:\/\/realearth.ssec.wisc.edu\"><strong>RealEarth<\/strong><\/a> <em><strong>(below)<\/strong><\/em> showed the large and dense smoke plume streaming southeastward, with the small pyroCb just north of the Bolivia\/Paraguay border \u2014 the brighter white tops of the pyrocumulus and pyrocumulonimbus clouds reached higher altitudes than the tan-colored smoke-rich clouds at lower altitudes.<\/p>\n<div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190825_1712utc_suomiNPP_1802utc_noaa20_trueColor_infraredWindow_Bolivia_pyroCb_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190825_1712utc_suomiNPP_1802utc_noaa20_trueColor_infraredWindow_Bolivia_pyroCb_anim.gif\" alt=\"Suomi NPP and NOAA-20 VIIRS True Color RGB and Infrared Window (11.45 \u00b5m) images [click to enlarge]\" width=\"642\" height=\"354\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP and NOAA-20 VIIRS True Color RGB and Infrared Window <em>(11.45 \u00b5m)<\/em> images [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>GOES-16 (GOES-East) &#8220;Red&#8221; Visible (0.64 \u00b5m), Shortwave Infrared (3.9 \u00b5m) and &#8220;Clean&#8221; Infrared Window (10.35 \u00b5m) images (above) showed the formation of a pyrocumulonimbus (pyroCb) cloud over far southeastern Bolivia on 18 August 2019. The small anvil cloud briefly surpassed the -40\u00baC pyroCb threshold from 1800-1820 UTC, attaining a minimum cloud-top infrared brightness temperature of [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":34110,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[6,74,78,53,45,49,48],"tags":[],"class_list":["post-34107","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-fire-detection","category-goes-16","category-noaa-20","category-real-earth","category-redgreenblue-rgb-images","category-suomi_npp","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/34107","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=34107"}],"version-history":[{"count":13,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/34107\/revisions"}],"predecessor-version":[{"id":34176,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/34107\/revisions\/34176"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/34110"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=34107"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=34107"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=34107"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}