{"id":38240,"date":"2020-09-09T23:59:13","date_gmt":"2020-09-09T23:59:13","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=38240"},"modified":"2020-09-12T03:00:45","modified_gmt":"2020-09-12T03:00:45","slug":"californias-bear-fire-produces-a-pyrocumulonimbus-cloud","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/38240","title":{"rendered":"Northern California&#8217;s Bear Fire produces a pyrocumulonimbus cloud"},"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\/200909_goes17_visible_shortwaveInfrared_fireTemperatureRGB_glmFlashExtentDensity_infraredWindow_CA_pyroCb_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/norcal_4p-20200909_104425.png\" alt=\"GOES-17 \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-17 \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\/200909_goes17_visible_shortwaveInfrared_fireTemperatureRGB_glmFlashExtentDensity_infraredWindow_CA_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>\u00a0GOES-17\u00a0<em>(GOES-West)\u00a0<\/em>\u201cRed\u201d 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>),\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>\u00a0(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>\u00a0(above)\u00a0<\/strong><\/em>showed the formation of a pyrocumulonimbus (pyroCb) cloud over the Bear Fire (part of the <a href=\"https:\/\/inciweb.nwcg.gov\/incident\/6997\/\"><strong>North Complex<\/strong><\/a>) in Northern California on <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20200909.html\"><strong>09 September 2020<\/strong><\/a>. The coldest cloud-top infrared brightness temperatures were -61.4<span class=\"css-901oao css-16my406 r-1qd0xha r-ad9z0x r-bcqeeo r-qvutc0\">\u00baC; no GLM-detected lightning activity was seen with this pyroCb.\u00a0<\/span><\/p>\n<p>A comparison of Suomi NPP VIIRS Day\/Night Band (0.7 \u00b5m), Shortwave Infrared (3.74 \u00b5m) and Infrared Window (11.45 \u00b5m) images <em><strong>(below)<\/strong> <\/em>displayed the initial 2 pyroCb cloud pulses shortly after their formation. Side-illumination from the Moon (which was in the Waning Gibbous phase, at 59% of Full) allowed for a distinct shadow to be cast northwest of the colder\/taller pyroCb pulse &#8212; and the pyroCb clouds exhibited a darker appearance than the layer of low-altitude smoke to the west, likely due to very high amounts of fresh smoke contained within the rapidly-rising cloud turrets.<\/p>\n<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/200909_1020utc_suomiNPP_viirs_infrared_dayNightBand_shortwaveInfrared_Bear_Fire_CA_pyroCb_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/200909_1020utc_suomiNPP_viirs_infrared_dayNightBand_shortwaveInfrared_Bear_Fire_CA_pyroCb_anim.gif\" alt=\"Suomi NPP VIIRS Day\/Night Band (0.7 \u00b5m), Shortwave Infrared (3.74 \u00b5m) and Infrared Window (11.45 \u00b5m) images [click to enlarge]\" width=\"643\" height=\"300\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS Day\/Night Band <em>(0.7 \u00b5m),<\/em> Shortwave Infrared <em>(3.74 \u00b5m)<\/em> and Infrared Window<em> (11.45 \u00b5m)<\/em> images [click to enlarge]<\/p><\/div><span class=\"css-901oao css-16my406 r-1qd0xha r-ad9z0x r-bcqeeo r-qvutc0\">A toggle between time-matched Infrared Window images of the Bear<\/span><span class=\"r-18u37iz\">\u00a0Fire<\/span>\u00a0<span class=\"r-18u37iz\">pyrocumulonimbus<\/span><span class=\"css-901oao css-16my406 r-1qd0xha r-ad9z0x r-bcqeeo r-qvutc0\">\u00a0cloud from\u00a0<\/span><span class=\"r-18u37iz\">Suomi NPP (SNPP)<\/span><span class=\"css-901oao css-16my406 r-1qd0xha r-ad9z0x r-bcqeeo r-qvutc0\">\u00a0and\u00a0<\/span><span class=\"r-18u37iz\">GOES-17<\/span><span class=\"css-901oao css-16my406 r-1qd0xha r-ad9z0x r-bcqeeo r-qvutc0\"><em><strong>\u00a0(below)<\/strong>\u00a0<\/em>highlighted the differences in spatial resolution \u2014 375-m with SNPP VIIRS, vs 2-km (at satellite sub-point) with GOES-17 ABI \u2014 and the <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/webapps\/parallax\/overview_updated.html\"><strong>parallax displacement<\/strong><\/a>\u00a0inherent with GOES-17 imagery at that location (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/200905_goes17_parallax.png\"><strong>17 km for a 15.2-km tall cloud top<\/strong><\/a>). The c<\/span><span class=\"css-901oao css-16my406 r-1qd0xha r-ad9z0x r-bcqeeo r-qvutc0\">oldest cloud-top infrared brightness temperature was -76.2\u00baC with SNPP, vs -59.9\u00baC with GOES-17 (identical color enhancements were applied to both images).<\/span><\/p>\n<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/200909_1028utc_suomiNPP_goes17_infrared_Bear_Fire_pyroCb_CA_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/200909_1028utc_suomiNPP_goes17_infrared_Bear_Fire_pyroCb_CA_anim.gif\" alt=\"Infrared Window images from Suomi NPP (11.45 \u00b5m) and GOES-17 (11.45 \u00b5m) [click to enlarge]\" width=\"643\" height=\"300\" \/><\/a><p class=\"wp-caption-text\">Infrared Window images from Suomi NPP <em>(11.45 \u00b5m)<\/em> and GOES-17<em> (10.35 \u00b5m)<\/em> [click to enlarge]<\/p><\/div>GOES-17 True Color Red-Green-Blue (RGB) images created using <a href=\"https:\/\/www.ssec.wisc.edu\/software\/geo2grid\/\"><strong>Geo2Grid<\/strong><\/a> <em><strong>(below)<\/strong><\/em> showed the southward drift of the high-altitude pyroCb cloud material during the day, along with widespread dense smoke that covered much of California at lower altitudes.<\/p>\n<div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/200909_goes17_trueColorRGB_CA_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/GOES-17_ABI_RadC_true_color_2020253_150117Z.png\" alt=\"GOES-17 True Color RGB images [click to pay animation | MP4]\" width=\"641\" height=\"641\" \/><\/a><p class=\"wp-caption-text\">GOES-17 True Color RGB images [click to pay animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/09\/200909_goes17_trueColorRGB_CA_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>1-minute\u00a0Mesoscale Domain Sector\u00a0GOES-17\u00a0(GOES-West)\u00a0\u201cRed\u201d Visible (0.64 \u00b5m), Shortwave Infrared (3.9 \u00b5m),\u00a0Fire Temperature\u00a0Red-Green-Blue (RGB) +\u00a0GLM\u00a0Flash Extent Density\u00a0(FED) and \u201cClean\u201d Infrared Window (10.35 \u00b5m) images\u00a0(above)\u00a0showed the formation of a pyrocumulonimbus (pyroCb) cloud over the Bear Fire (part of the North Complex) in Northern California on 09 September 2020. The coldest cloud-top infrared brightness temperatures were -61.4\u00baC; no GLM-detected [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":38247,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[6,80,45,49,48],"tags":[],"class_list":["post-38240","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-fire-detection","category-goes-17","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\/38240","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=38240"}],"version-history":[{"count":8,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/38240\/revisions"}],"predecessor-version":[{"id":38257,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/38240\/revisions\/38257"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/38247"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=38240"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=38240"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=38240"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}