{"id":62038,"date":"2024-12-10T23:59:00","date_gmt":"2024-12-10T23:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=62038"},"modified":"2024-12-13T01:19:25","modified_gmt":"2024-12-13T01:19:25","slug":"franklin-fire-near-malibu-california","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/62038","title":{"rendered":"Franklin Fire near Malibu, California"},"content":{"rendered":"<p><div style=\"width: 2720px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/12\/241210_g18_swir_Franklin_Fire_CA.mp4\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/12\/241210_0855utc_g18_swir_CA_fire.png\" width=\"2710\" height=\"1674\" \/><\/a><p class=\"wp-caption-text\">1-minute GOES-18 Shortwave Infrared (3.9 \u00b5m) images, from 0631-2130 UTC on 10th December [click to play MP4 animation]<\/p><\/div>1-minute <a href=\"https:\/\/www.nco.ncep.noaa.gov\/status\/satellite\/\"><strong>Mesoscale Domain Sector<\/strong><\/a> GOES-18 <em>(GOES-West)<\/em> Shortwave Infrared (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band07.pdf\"><strong>3.9 \u00b5m<\/strong><\/a>) images <em><strong>(above)<\/strong><\/em> displayed a pronounced thermal signature associated with the <a href=\"https:\/\/www.fire.ca.gov\/incidents\/2024\/12\/9\/franklin-fire\"><strong>Franklin Fire<\/strong><\/a>, which began burning just north-northwest Malibu, California around <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/12\/241210_0644utc_g18_swir_FF_initial_detect.png\"><strong>0644 UTC<\/strong><\/a> on <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20241210.html\"><strong>10th December 2024<\/strong><\/a> (or 10:24 PM PST on 9th December). This wildfire was driven by strong <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/12\/241210_klox_pns_wind.text\"><strong>Santa Ana winds<\/strong><\/a>, which helped it to increase rapidly in size and intensity &#8212; in fact, the Franklin Fire began to exhibit 3.9 \u00b5m brightness temperatures of 137.88\u00baC (the saturation temperature of GOES-18 <a href=\"https:\/\/www.goes-r.gov\/spacesegment\/abi.html\"><strong>ABI<\/strong><\/a> Band 7 detectors) beginning at 0855 UTC <em><strong>(below)<\/strong><\/em>, which persisted until 0947 UTC.<\/p>\n<p><div style=\"width: 2720px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/12\/241210_0855utc_g18_swir_cursor_sample.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/12\/241210_0855utc_g18_swir_cursor_sample.png\" width=\"2710\" height=\"1674\" \/><\/a><p class=\"wp-caption-text\">Sample of GOES-18 Shortwave Infrared (3.9 \u00b5m) brightness temperature NW of Malibu at 0855 UTC on 10th December [click to enlarge]<\/p><\/div>About 12 minutes after the Franklin Fire began to exhibit a thermal signature on GOES-18 Shortwave Infrared imagery, a <a href=\"https:\/\/www.nifc.gov\/about-us\/what-is-nifc\/remote-automatic-weather-stations\"><strong>RAWS<\/strong><\/a> site just east of the wildfire reported a wind gust of 52 mph at 0656 UTC <em><strong>(below)<\/strong><\/em>. About 2.5 hours later, a RAWS site just northwest of the fire reported a wind gust of <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/12\/241210_0931utc_g18_swir_RAWS.png\"><strong>50 mph at 0931 UTC<\/strong><\/a>. In addition to the strong winds, relative humidity values at those nearby RAWS sites were generally 10% or less.<\/p>\n<p><div style=\"width: 2720px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/12\/241210_0656utc_g18_swir_RAWS.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/12\/241210_0656utc_g18_swir_RAWS.png\" width=\"2710\" height=\"1674\" \/><\/a><p class=\"wp-caption-text\">GOES-18 Shortwave Infrared image at 0656 UTC, with a sample of RAWS site observation data just east of the Franklin Fire [click to enlarge]<\/p><\/div>Since the Franklin Fire began and rapidly intensified during the nighttime hours, its thermal signature was also apparent in the Near-Infrared <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band05.pdf\"><strong>1.61 \u00b5m<\/strong><\/a> and <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band06.pdf\"><strong>2.24 \u00b5m<\/strong><\/a> spectral bands <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 1292px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/12\/241210_goes18_nearInfrared_shortwaveInfrared_Franklin_Fire_CA_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/12\/G18_NIR_SWIR_FRANKLIN_FIRE_CA_10DEC2024_B567_2024345_085524_0003PANELS_FRAME00141.GIF\" width=\"1282\" height=\"964\" \/><\/a><p class=\"wp-caption-text\">1-minute GOES-18 Near-Infrared (1.61 \u00b5m and 2.24 \u00b5m, top and middle) and Shortwave Infrared (3.9 \u00b5m, bottom) images, from 0635-1430 UTC on 10th December [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/12\/241210_goes18_nearInfrared_shortwaveInfrared_Franklin_Fire_CA_anim.mp4\"><strong>MP4]<\/strong><\/a><\/p><\/div>1-minute GOES-18 True Color RGB images from the <a href=\"https:\/\/geosphere.ssec.wisc.edu\/#playing:true;coordinate:-30792,182544;zoom:1.5;satellite:goeswest;num_frames:61;\"><strong>CSPP GeoSphere<\/strong><\/a> site <em><strong>(below)<\/strong><\/em> revealed several pyrocumulus jumps over the Franklin Fire, in addition to a dense smoke plume drifting offshore.<\/p>\n<div style=\"width: 1506px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/12\/goeswest_abi_radm1_true_color_night_s20241210153027_e20241210235925_f510.mp4\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/12\/goeswest_abi_radm1_true_color_night_20241210162027.png\" width=\"1496\" height=\"848\" \/><\/a><p class=\"wp-caption-text\">1-minute GOES-18 True Color RGB images, from 1530-2359 UTC on 10th December [click to play MP4 animation]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>1-minute Mesoscale Domain Sector GOES-18 (GOES-West) Shortwave Infrared (3.9 \u00b5m) images (above) displayed a pronounced thermal signature associated with the Franklin Fire, which began burning just north-northwest Malibu, California around 0644 UTC on 10th December 2024 (or 10:24 PM PST on 9th December). This wildfire was driven by strong Santa Ana winds, which helped it [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":62042,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[6,114,45],"tags":[],"class_list":["post-62038","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\/62038","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=62038"}],"version-history":[{"count":32,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/62038\/revisions"}],"predecessor-version":[{"id":62075,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/62038\/revisions\/62075"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/62042"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=62038"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=62038"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=62038"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}