{"id":28992,"date":"2018-07-15T23:59:10","date_gmt":"2018-07-15T23:59:10","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=28992"},"modified":"2018-07-17T12:59:42","modified_gmt":"2018-07-17T12:59:42","slug":"ferguson-fire-in-california-forms-a-pyrocumulonimbus-cloud","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/28992","title":{"rendered":"Ferguson Fire in California forms a pyrocumulonimbus cloud"},"content":{"rendered":"<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/07\/180715_goes16_visible_shortwaveInfrared_infraredWindow_Ferguson_Fire_CA_pyrocb_anim.mp4\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/07\/G16_VIS_SWIR_IR_CA_PYROCB_15JUL2018_960x427_B2713_2018196_224334_0003PANELS_00029.GIF\" alt=\"GOES-16 \" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible<em> (0.64 \u00b5m, left),<\/em> Shortwave Infrared<em> (3.9 \u00b5m, center)<\/em> and &#8220;Clean&#8221; Infrared Window <em>(10.3 \u00b5m, right)<\/em> images [click to play MP4 animation]<\/p><\/div>\n<p style=\"text-align: center;\"><strong>* GOES-17 images shown here are preliminary and non-operational *<\/strong><\/p>\n<p>The <a href=\"https:\/\/inciweb.nwcg.gov\/incident\/5927\/\"><strong>Ferguson Fire<\/strong><\/a> in central California produced a pyrocumulonimbus (pyroCb) cloud during the afternoon hours on <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20180715.html\"><strong>15 July 2018<\/strong><\/a>.\u00a0GOES-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 (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band13.pdf\"><strong>10.3 \u00b5m<\/strong><\/a>) images<em><strong> (above)<\/strong><\/em> showed that the high-altitude portion of the pyroCb cloud then drifted northeastward toward the California\/Nevada border, where cloud-top infrared brightness temperatures cooled to near -55\u00baC<em> (orange enhancement)<\/em> as it crossed the border around <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/07\/G16_VIS_SWIR_IR_CA_PYROCB_15JUL2018_960x427_B2713_2018197_000534_0003PANELS_00111.GIF\"><strong>0005 UTC<\/strong><\/a> on 16 July.<\/p>\n<p>A comparison of Visible images from GOES-15 (0.63 \u00b5m), GOES-17 (0.64 \u00b5m) and GOES-16 (0.64 \u00b5m) is shown below &#8212; with the imagery displayed in the native projection of each satellite. Images from GOES-16\/17 are at 5-minute intervals, while images from GOES-15 are every 5-15 minutes depending on the operational scan schedule of that GOES-West satellite. GOES-17 was at its post-launch checkout position of 89.5\u00baW longitude, so it offered a more direct view of the pyroCb cloud.<\/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\/2018\/07\/180715_goes15_goes17_goes16_visible_Ferguson_Fire_CA_pyrocb_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/07\/180715_G15_G17_G16_VIS_CA_PYROCB_08.GIF\" alt=\"Visible images from GOES-15 (0.63 \u00b5m, left), GOES-17 (0.64 \u00b5m, center) and GOES-16 (0.64 \u00b5m, right) [click to play animation]\" width=\"640\" height=\"424\" \/><\/a><p class=\"wp-caption-text\">Visible images from <strong>GOES-15<\/strong><em> (0.63 \u00b5m, left),<\/em> <strong>GOES-17<\/strong> <em>(0.64 \u00b5m, center)<\/em> and <strong>GOES-16<\/strong> <em>(0.64 \u00b5m, right)<\/em> [click to play animation]<\/p><\/div>A toggle between NOAA-19 Visible (0.63 \u00b5m), Shortwave Infrared (3.7 \u00b5m) and Infrared Window (10.8 \u00b5m) images <em><strong>(below)<\/strong><\/em> showed the pyroCb cloud southwest of the California\/Nevada border (between Bridgeport KBAN and Mammoth KMMH) at 2327 UTC. In spite of a minimum cloud-top 10.8 \u00b5m infrared brightness temperature of -59\u00baC<em> (red enhancement),<\/em> note the darker<em> (warmer)<\/em> appearance of the cloud on the 3.7 \u00b5m image &#8212; this is due to reflection of solar radiation off the smaller ice particles of the pyroCb anvil. The -59\u00baC temperature roughly corresponded to an altitude of 13 km or 42.6 kft on the 00 UTC Reno, Nevada rawinsonde report (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/07\/180716_00UTC_KREV_RAOB.GIF\"><strong>plot<\/strong><\/a> | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/07\/180716_00UTC_KREV_RAOB.TEXT\"><strong>data<\/strong><\/a>)<\/p>\n<p><div style=\"width: 649px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/07\/180715_2327utc_noaa19_visible_shortwaveIR_IRwindow_Ferguson_Fire_CA_pyrocb_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/07\/180715_2327utc_noaa19_visible_shortwaveIR_IRwindow_Ferguson_Fire_CA_pyrocb_anim.gif\" alt=\"NOAA-19 Visible (0.63 \u00b5m), Shortwave Infrared (3.7 \u00b5m) and Infrared Window (10.8 \u00b5m) images [click to enlarge]\" width=\"639\" height=\"424\" \/><\/a><p class=\"wp-caption-text\">NOAA-19 Visible <em>(0.63 \u00b5m),<\/em> Shortwave Infrared <em>(3.7 \u00b5m)<\/em> and Infrared Window <em>(10.8 \u00b5m)<\/em> images [click to enlarge]<\/p><\/div>A time lapse of the pyroCb was created by Sierra Fire Watch <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 648px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/www.youtube.com\/watch?v=dwcUCeucQ9Y&amp;feature=youtu.be\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/07\/180715_Ferguson_Fire_time_lapse_capture.jpeg\" alt=\"Time lapse [click to play YouTube video]\" width=\"638\" height=\"359\" \/><\/a><p class=\"wp-caption-text\">Time lapse [click to play YouTube video]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>* GOES-17 images shown here are preliminary and non-operational * The Ferguson Fire in central California produced a pyrocumulonimbus (pyroCb) cloud during the afternoon hours on 15 July 2018.\u00a0GOES-16 (GOES-East) &#8220;Red&#8221; Visible (0.64 \u00b5m), Shortwave Infrared (3.9 \u00b5m) and &#8220;Clean&#8221; Infrared Window (10.3 \u00b5m) images (above) showed that the high-altitude portion of the pyroCb cloud [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":28994,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[22,6,43,74,80,26],"tags":[],"class_list":["post-28992","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-avhrr","category-fire-detection","category-goes-15","category-goes-16","category-goes-17","category-poes"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/28992","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=28992"}],"version-history":[{"count":7,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/28992\/revisions"}],"predecessor-version":[{"id":29000,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/28992\/revisions\/29000"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/28994"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=28992"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=28992"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=28992"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}