{"id":53733,"date":"2023-07-27T23:59:00","date_gmt":"2023-07-27T23:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=53733"},"modified":"2023-07-29T01:47:13","modified_gmt":"2023-07-29T01:47:13","slug":"spoon-fire-in-arizona-produces-a-pyrocumulonimbus-cloud","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/53733","title":{"rendered":"Spoon Fire in Arizona 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\/07\/230727_goes18_dayLandCloudFireRGB_shortwaveInfrared_infraredWindow_cloudTopTemperature_Spoon_Fire_AZ_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/07\/az_4p-20230728_005725.png\" width=\"1712\" height=\"828\"><\/a><p class=\"wp-caption-text\">GOES-18 Day Land Cloud Fire RGB (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\/07\/230727_goes18_dayLandCloudFireRGB_shortwaveInfrared_infraredWindow_cloudTopTemperature_Spoon_Fire_AZ_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>1-minute&nbsp;<a href=\"https:\/\/www.nco.ncep.noaa.gov\/status\/satellite\/\"><strong>Mesoscale Domain Sector<\/strong><\/a> GOES-18&nbsp;<em>(GOES-West)<\/em>&nbsp;<a href=\"https:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/QuickGuide_GOESR_DayLandCloudFireRGB_final.pdf\"><strong>Day Land Cloud Fire RGB<\/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 <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_BaselineCloudTopTemperature.pdf\"><strong>Cloud Top Temperature<\/strong><\/a> derived product images <em><strong>(above)<\/strong><\/em> showed that the <a href=\"https:\/\/inciweb.nwcg.gov\/incident-information\/azfta-spoon-fire\"><strong>Spoon Fire<\/strong><\/a> in in east-central Arizona 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_20230727.html\"><strong>27 July 2023<\/strong><\/a>. Cloud-top 10.3 \u00b5m brightness temperatures reached the -40\u00baC pyroCb threshold (shades of blue) at 0043 UTC &#8212; and later cooled to a minimum of -50.48\u00baC (with a corresponding Cloud Top Temperature of -54.11\u00baC) at 0057 UTC <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 1543px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/07\/230728_0057utc_goes18_dayLandCloudFireRGB_shortwaveInfrared_infraredWindow_cloudTopTemperature_Spoon_Fire_AZ_pyroCb.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/07\/230728_0057utc_goes18_dayLandCloudFireRGB_shortwaveInfrared_infraredWindow_cloudTopTemperature_Spoon_Fire_AZ_pyroCb.png\" width=\"1533\" height=\"779\"><\/a><p class=\"wp-caption-text\">Cursor-sampled values showing a 10.3 \u00b5m brightness temperature of -50.48\u00baC and a corresponding Cloud Top Temperature of -54.11\u00baC at 0057 UTC [click to enlarge]<\/p><\/div>A plot of rawinsonde data from Flagstaff, Arizona at 0000 UTC on 28 July <em><strong>(below)<\/strong><\/em> indicated that the -50.48\u00baC \/ -54.11\u00baC cloud-top temperature values were close to the height of the Equilibrium Level (EL) of a Most Unstable (MU) air parcel.<\/p>\n<p><div style=\"width: 1707px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/07\/230728_0000utc_kfgz_raob.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/07\/230728_0000utc_kfgz_raob.png\" width=\"1697\" height=\"826\"><\/a><p class=\"wp-caption-text\">Plot of rawinsonde data from Flagstaff, Arizona at 0000 UTC on 28 July [click to enlarge]<\/p><\/div>Prior to producing a pyroCb cloud, the Spoon Fire burned very hot &#8212; 3.9 \u00b5m brightness temperatures reached 137.88\u00baC (which is the saturation temperature of the GOES-18 <a href=\"https:\/\/www.goes-r.gov\/spacesegment\/abi.html\"><strong>ABI<\/strong><\/a> Band 7 detectors) shortly after 2300 UTC, and Fire Power values reached 2842.06 MW at 2334 UTC <em><strong>(below)<\/strong><\/em>. The Fire Power derived product is a component of the GOES Fire Detection and Characterization Algorithm (<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>),<\/p>\n<p><div style=\"width: 1722px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/07\/230727_goes18_dayLandCloudFireRGB_shortwaveInfrared_infraredWindow_firePower_Spoon_Fire_AZ_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/07\/az_firePower_4p-20230727_233425.png\" width=\"1712\" height=\"828\"><\/a><p class=\"wp-caption-text\">GOES-18 Day Land Cloud Fire RGB (top left), Shortwave Infrared (3.9 \u00b5m, top right), \u201cClean\u201d Infrared Window (10.3 \u00b5m, bottom left) and Fire Power derived product (bottom right) [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/07\/230727_goes18_dayLandCloudFireRGB_shortwaveInfrared_infraredWindow_firePower_Spoon_Fire_AZ_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div><br \/>\n<div style=\"width: 1537px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/07\/230727_2334utc_goes18_dayLandCloudFireRGB_shortwaveInfrared_infraredWindow_firePower_Spoon_Fire_AZ.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/07\/230727_2334utc_goes18_dayLandCloudFireRGB_shortwaveInfrared_infraredWindow_firePower_Spoon_Fire_AZ.png\" width=\"1527\" height=\"779\"><\/a><p class=\"wp-caption-text\">Cursor-sampled values showing a 3.9 \u00b5m brightness temperature of 137.88\u00baC along with a corresponding Fire Power value of 2842.06 MW at 2334 UTC [click to enlarge]<\/p><\/div><\/p>\n","protected":false},"excerpt":{"rendered":"<p>1-minute&nbsp;Mesoscale Domain Sector GOES-18&nbsp;(GOES-West)&nbsp;Day Land Cloud Fire RGB, Shortwave Infrared (3.9 \u00b5m), \u201cClean\u201d Infrared Window (10.3 \u00b5m) and Cloud Top Temperature derived product images (above) showed that the Spoon Fire in in east-central Arizona produced a pyrocumulonimbus (pyroCb) cloud late in the day on 27 July 2023. Cloud-top 10.3 \u00b5m brightness temperatures reached the -40\u00baC [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":53739,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[6,114,45],"tags":[],"class_list":["post-53733","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\/53733","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=53733"}],"version-history":[{"count":6,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/53733\/revisions"}],"predecessor-version":[{"id":53740,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/53733\/revisions\/53740"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/53739"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=53733"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=53733"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=53733"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}