{"id":38221,"date":"2020-09-06T23:59:25","date_gmt":"2020-09-06T23:59:25","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=38221"},"modified":"2020-09-12T02:59:24","modified_gmt":"2020-09-12T02:59:24","slug":"pyrocumulonimbus-clouds-produced-by-the-cameron-peak-fire-in-colorado","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/38221","title":{"rendered":"Pyrocumulonimbus clouds produced by the Cameron Peak Fire in Colorado"},"content":{"rendered":"<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/200906_goes16_visible_shortwaveInfrared_fireTemperatureRGB_glmFlashExtentDensity_infraredWindow_CO_pyroCb_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/co_4p-20200906_231053.png\" alt=\"GOES-16 \u201cRed\u201d Visible (0.64 \u00b5m, top left), Shortwave Infrared (3.9 \u00b5m, top right), Fire Temperature RGB + GLM Flash Extent Density (bottom left) and \u201cClean\u201d Infrared Window (10.35 \u00b5m, bottom right) [click to play animation | MP4]\" width=\"643\" height=\"300\" \/><\/a><p class=\"wp-caption-text\">GOES-16 \u201cRed\u201d Visible<em> (0.64 \u00b5m, top left),<\/em> Shortwave Infrared <em>(3.9 \u00b5m, top right),<\/em> Fire Temperature RGB + GLM Flash Extent Density <em>(bottom left)<\/em> and \u201cClean\u201d Infrared Window<em> (10.35 \u00b5m, bottom right)<\/em> [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/200906_goes16_visible_shortwaveInfrared_fireTemperatureRGB_glmFlashExtentDensity_infraredWindow_CO_pyroCb_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>1-minute\u00a0<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/23225\"><strong>Mesoscale Domain Sector<\/strong><\/a> GOES-16 <em>(GOES-East) <\/em>\u201cRed\u201d Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>), GOES-17 Shortwave Infrared (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band07.pdf\"><strong>3.9 \u00b5m<\/strong><\/a>),\u00a0<a href=\"http:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/Fire_Temperature_RGB.pdf\"><strong>Fire Temperature<\/strong><\/a>\u00a0Red-Green-Blue (RGB) +\u00a0<a href=\"https:\/\/www.goes-r.gov\/spacesegment\/glm.html\"><strong>GLM<\/strong><\/a>\u00a0<a href=\"https:\/\/vlab.ncep.noaa.gov\/web\/geostationary-lightning-mapper\/overview\/-\/asset_publisher\/hNLfUix1macb\/blog\/operational-utility-of-glm-flash-extent-density-on-june-1\"><strong>Flash Extent Density<\/strong><\/a> (FED) and \u201cClean\u201d 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 2 distinct pulses of pyrocumulonimbus (pyroCb) cloud emanating from the <a href=\"https:\/\/inciweb.nwcg.gov\/incident\/6964\/\"><strong>Cameron Peak Fire<\/strong><\/a> in north-central Colorado on <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20200906.html\"><strong>06 September 2020<\/strong><\/a>. The coldest cloud-top infrared brightness temperatures were -52.4<span class=\"css-901oao css-16my406 r-1qd0xha r-ad9z0x r-bcqeeo r-qvutc0\">\u00baC. Smoke was occasionally restricting the surface visibility to 2 miles at Boulder (KBJC) and 2.5 miles at Fort Collins (KFNL).<\/span><\/p>\n<p>This fire also produced a brief pyroCb cloud on the previous day <em><strong>(below)<\/strong>, <\/em>as shown by a single blue (-40<span class=\"css-901oao css-16my406 r-1qd0xha r-ad9z0x r-bcqeeo r-qvutc0\">\u00baC) pixel on the 10.35 \u00b5m image at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/co_4p-20200905_230116.png\"><strong>2301 UTC <\/strong><\/a><\/span>&#8212; however, since no Mesoscale Sector was positioned over the area, the fire was only sampled by 5-minute CONUS Sector images. The presence of cloud-top infrared brightness temperatures of -40<span class=\"css-901oao css-16my406 r-1qd0xha r-ad9z0x r-bcqeeo r-qvutc0\">\u00baC<\/span> and colder assures heterogeneous nucleation of all supercooled water droplets to form ice crystals, thereby meeting the criteria of a pyroCb.<\/p>\n<div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/200905_goes16_visible_shortwaveInfrared_fireTemperatureRGB_glmFlashExtentDensity_infraredWindow_CO_pyroCb_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/co_4p-20200905_230116.png\" alt=\"GOES-16 \u201cRed\u201d Visible (0.64 \u00b5m, top left), Shortwave Infrared (3.9 \u00b5m, top right), Fire Temperature RGB + GLM Flash Extent Density (bottom left) and \u201cClean\u201d Infrared Window (10.35 \u00b5m, bottom right) [click to play animation | MP4]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">GOES-16 \u201cRed\u201d Visible<em> (0.64 \u00b5m, top left),<\/em> Shortwave Infrared<em> (3.9 \u00b5m, top right),<\/em> Fire Temperature RGB + GLM Flash Extent Density<em> (bottom left)<\/em> and \u201cClean\u201d Infrared Window<em> (10.35 \u00b5m, bottom right)<\/em> [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/200905_goes16_visible_shortwaveInfrared_fireTemperatureRGB_glmFlashExtentDensity_infraredWindow_CO_pyroCb_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p style=\"text-align: center;\"><strong>===== 07 September Update =====<\/strong><\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/200907_0916utc_suomiNPP_viirs_shortwaveInfrared_dayNightBand_Cameron_Peak_Fire_CO_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/200907_0916utc_suomiNPP_viirs_shortwaveInfrared_dayNightBand_Cameron_Peak_Fire_CO_anim.gif\" alt=\"Suomi NPP VIIRS Shortwave Infrared (3.74 \u00b5m) and Day\/Night Band (0.7 \u00b5m) images, with plots of METAR surface reports [click to enlarge]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS Shortwave Infrared <em>(3.74 \u00b5m)<\/em> and Day\/Night Band <em>(0.7 \u00b5m)<\/em> images, with plots of METAR surface reports [click to enlarge]<\/p><\/div>As the fire continued burning into the nighttime hours, Suomi NPP VIIRS Shortwave Infrared (3.74 \u00b5m) and Day\/Night Band (0.7 \u00b5m) images<em><strong> (above)<\/strong><\/em> displayed the fire around 0916 UTC or 2:16 am PDT on 07 September. Reflected illumination from the Moon &#8212; in the Waning Gibbous phase, at 76% of Full &#8212; allowed some of the eastward-drifting smoke to be seen.<\/p>\n<p>A toggle between Shortwave Infrared images from Suomi NPP VIIRS (3.74 \u00b5m) and GOES-16 ABI (3.9 \u00b5m) is shown below &#8212; the shape of the Cameron Peak Fire thermal anomaly as well as locations of ongoing hot fires along its perimeter were more accurately seen in the 375-m resolution <a href=\"https:\/\/www.jpss.noaa.gov\/viirs.html\"><strong>VIIRS<\/strong><\/a> image, compared to the 2-km resolution (at satellite sub-point) <a href=\"https:\/\/www.goes-r.gov\/spacesegment\/abi.html\"><strong>ABI<\/strong><\/a> image. The 2 images are time-matched to correspond to the 0922 UTC time of the Suomi NPP satellite&#8217;s <a href=\"https:\/\/www.ssec.wisc.edu\/datacenter\/polar_orbit_tracks\/data\/NPP\/2020\/2020_09_07_251\/NA.gif\"><strong>overpass<\/strong><\/a>.<\/p>\n<div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/200907_0916utc_suomiNPP_goes16_shortwaveInfrared_Cameron_Peak_Fire_CO_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/200907_0916utc_suomiNPP_goes16_shortwaveInfrared_Cameron_Peak_Fire_CO_anim.gif\" alt=\"Shortwave Infrared images from Suomi NPP (3.74 \u00b5m) and GOES-16 (3.9 \u00b5m), with plots of METAR surface reports [click to enlarge]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">Shortwave Infrared images from Suomi NPP <em>(3.74 \u00b5m)<\/em> and GOES-16<em> (3.9 \u00b5m),<\/em> with plots of METAR surface reports [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>1-minute\u00a0Mesoscale Domain Sector GOES-16 (GOES-East) \u201cRed\u201d Visible (0.64 \u00b5m), GOES-17 Shortwave Infrared (3.9 \u00b5m),\u00a0Fire Temperature\u00a0Red-Green-Blue (RGB) +\u00a0GLM\u00a0Flash Extent Density (FED) and \u201cClean\u201d Infrared Window (10.35 \u00b5m) images (above) showed 2 distinct pulses of pyrocumulonimbus (pyroCb) cloud emanating from the Cameron Peak Fire in north-central Colorado on 06 September 2020. The coldest cloud-top infrared brightness temperatures [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":38226,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[7,6,74,49,48],"tags":[],"class_list":["post-38221","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-air-quality","category-fire-detection","category-goes-16","category-suomi_npp","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/38221","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=38221"}],"version-history":[{"count":9,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/38221\/revisions"}],"predecessor-version":[{"id":38256,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/38221\/revisions\/38256"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/38226"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=38221"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=38221"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=38221"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}