{"id":54009,"date":"2023-08-16T23:59:00","date_gmt":"2023-08-16T23:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=54009"},"modified":"2023-08-18T14:38:22","modified_gmt":"2023-08-18T14:38:22","slug":"crater-creek-fire-in-british-columbia-produces-a-pyrocumulonimbus-cloud","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/54009","title":{"rendered":"Crater Creek Fire in British Columbia produces a pyrocumulonimbus cloud"},"content":{"rendered":"<p><div style=\"width: 1722px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/08\/230816_goes18_BC_pyroCb_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/08\/bc_4p-20230817_014226.png\" width=\"1712\" height=\"828\" \/><\/a><p class=\"wp-caption-text\">GOES-18 &#8220;Red&#8221; Visible (0.64 \u00b5m) + Fire Power derived product (top left), Shortwave Infrared (3.9 \u00b5m, top right), \u201cClean\u201d Infrared Window (10.3 \u00b5m, bottom left) and Cloud Top Temperature derived product (bottom right) [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/08\/230816_goes18_BC_pyroCb_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>1-minute\u00a0<a href=\"https:\/\/www.nco.ncep.noaa.gov\/status\/satellite\/\"><strong>Mesoscale Domain Sector<\/strong><\/a>\u00a0GOES-18\u00a0<em>(GOES-West)<\/em> &#8220;Red&#8221; Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>) + Fire Power derived product (a component of the GOES Fire Detection and Characterization Algorithm\u00a0<a href=\"http:\/\/rammb.cira.colostate.edu\/training\/visit\/training_sessions\/goes_r_fire_surface_properties\/video\/presentation_html5.html?lms=1\"><strong>FDCA<\/strong><\/a>), Shortwave Infrared (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band07.pdf\"><strong>3.9 \u00b5m<\/strong><\/a>), \u201cClean\u201d Infrared Window (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>10.3 \u00b5m<\/strong><\/a>) and\u00a0<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_BaselineCloudTopTemperature.pdf\"><strong>Cloud Top Temperature<\/strong><\/a>\u00a0derived product images\u00a0<em><strong>(above)<\/strong><\/em> showed that the Crater Creek Fire &#8212; located in far southern British Columbia, less than 10 miles from the Washington border &#8212; produced a <a href=\"https:\/\/www.nature.com\/articles\/s43247-022-00566-8\"><strong>pyrocumulonimbus<\/strong><\/a> (pyroCb) cloud late in the day on <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20230816.html\"><strong>16 August 2023<\/strong><\/a>.<\/p>\n<p><div style=\"width: 1546px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/08\/230817_0142utc_BC_pyroCb_cursor_sample.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/08\/230817_0142utc_BC_pyroCb_cursor_sample.png\" width=\"1536\" height=\"778\" \/><\/a><p class=\"wp-caption-text\">Cursor sampling of GOES-18 &#8220;Red&#8221; Visible (0.64 \u00b5m) + Fire Power derived product (top left), Shortwave Infrared (3.9 \u00b5m, top right), \u201cClean\u201d Infrared Window (10.3 \u00b5m, bottom left) and Cloud Top Temperature derived product (bottom right) at 0142 UTC [click to enlarge]<\/p><\/div>Beginning at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/08\/230817_0023utc_BC_pyroCb_cursor_sample.png\"><strong>0023 UTC<\/strong><\/a> (prior to pyroCB development), the fire occasionally exhibited 3.9 \u00b5m brightness temperatures of 137.88\u00baC (the saturation temperature of the GOES-18 <a href=\"https:\/\/www.goes-r.gov\/spacesegment\/abi.html\"><strong>ABI<\/strong><\/a> Band 7 detectors) \u2014 and Fire Power values reached 3929.32 MW at 0142 UTC <em><strong>(above)<\/strong><\/em>. Cloud-top 10.3 \u00b5m brightness temperatures first reached the -40\u00baC pyroCb threshold (shades of blue) at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/08\/230817_0035utc_BC_pyroCb_cursor_sample.png\"><strong>0035 UTC<\/strong><\/a> \u2014 and later cooled to a minimum of -42.31\u00baC (with a corresponding Cloud Top Temperature of -57.17\u00baC) at 0157 UTC <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 1545px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/08\/230817_0157utc_BC_pyroCb_cursor_sample.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/08\/230817_0157utc_BC_pyroCb_cursor_sample.png\" width=\"1535\" height=\"780\" \/><\/a><p class=\"wp-caption-text\">Cursor sampling of GOES-18 &#8220;Red&#8221; Visible (0.64 \u00b5m) + Fire Power derived product (top left), Shortwave Infrared (3.9 \u00b5m, top right), \u201cClean\u201d Infrared Window (10.3 \u00b5m, bottom left) and Cloud Top Temperature derived product (bottom right) at 0157 UTC [click to enlarge]<\/p><\/div>1-minute GOES-18 True Color RGB images from the <a href=\"https:\/\/geosphere.ssec.wisc.edu\/#playing:true;coordinate:0,0;satellite:goeswest;num_frames:40;\"><strong>CSPP GeoSphere<\/strong><\/a>\u00a0site\u00a0<em><strong>(below)<\/strong><\/em> showed the abrupt pyroCb pulse as it quickly rose above the wildfire smoke plume, and the pyroCb anvil as it then drifted north-northeastward.<\/p>\n<div style=\"width: 1034px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/08\/goeswest_abi_radm1_true_color_night_s20230817000029_e20230817023029_f151.mp4\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/08\/goeswest_abi_radm1_true_color_night_20230817010926.png\" width=\"1024\" height=\"461\" \/><\/a><p class=\"wp-caption-text\">GOES-18 True Color RGB images [click to play MP4 animation]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>1-minute\u00a0Mesoscale Domain Sector\u00a0GOES-18\u00a0(GOES-West) &#8220;Red&#8221; Visible (0.64 \u00b5m) + Fire Power derived product (a component of the GOES Fire Detection and Characterization Algorithm\u00a0FDCA), Shortwave Infrared (3.9 \u00b5m), \u201cClean\u201d Infrared Window (10.3 \u00b5m) and\u00a0Cloud Top Temperature\u00a0derived product images\u00a0(above) showed that the Crater Creek Fire &#8212; located in far southern British Columbia, less than 10 miles from the [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":54011,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[6,114,45],"tags":[],"class_list":["post-54009","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-fire-detection","category-goes-18","category-redgreenblue-rgb-images"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/54009","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=54009"}],"version-history":[{"count":2,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/54009\/revisions"}],"predecessor-version":[{"id":54017,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/54009\/revisions\/54017"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/54011"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=54009"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=54009"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=54009"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}