{"id":34081,"date":"2019-08-17T23:59:01","date_gmt":"2019-08-17T23:59:01","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=34081"},"modified":"2019-08-18T20:57:26","modified_gmt":"2019-08-18T20:57:26","slug":"swan-lake-fire-in-alaska","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/34081","title":{"rendered":"Swan Lake Fire in Alaska"},"content":{"rendered":"<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190817_goes17_visible_shortwaveInfrared_SwanLakeFire_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/ak_swir-20190817_232757.png\" alt=\"GOES-17 \" width=\"642\" height=\"367\" \/><\/a><p class=\"wp-caption-text\">GOES-17 &#8220;Red&#8221; Visible <em>(0.64 \u00b5m)<\/em> and Shortwave Infrared <em>(3.9 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190817_goes17_visible_shortwaveInfrared_SwanLakeFire_AK_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>1-minute <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/23225\"><strong>Mesoscale Domain Sector<\/strong><\/a> GOES-17 <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> and 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> revealed thick smoke and a pronounced thermal anomaly <em>(hot pixels, darker black)<\/em> associated with the <a href=\"https:\/\/inciweb.nwcg.gov\/incident\/6387\/\"><strong>Swan Lake Fire<\/strong><\/a> on the Kenai Peninsula in south-central Alaska on 17 August 2019. Later in the day, a few pyrocumulus jumps could be seen in Visible imagery over the fire source region, as fire behavior increased (another day when pyrocumulus jumps were apparent with this fire was <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/06\/190630_goes17_visible_shortwaveInfrared_Swan_Lake_Fire_AK_anim.gif\"><strong>30 June<\/strong><\/a>, during a period when southerly winds were transporting dense smoke to the <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/06\/190628_190630_PANC_SFCMG.GIF\"><strong>Anchorage area<\/strong><\/a>).<\/p>\n<p>Strong northerly-northwesterly winds were transporting smoke from the Swan Lake Fire southward across the Kenai Peninsula and the Seward area &#8212; a time series of surface report data from Seward <em><strong>(below)<\/strong> <\/em>showed that this smoke had reduced the visibility to less than 1 mile by 03 UTC (7 PM local time). South-central Alaska was experiencing <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190813_droughtMonitor_AK.png\"><strong>drought conditions<\/strong><\/a>, which had <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190806_190813_AK_drought_monitor.png\"><strong>worsened<\/strong><\/a> from the preceding week; the strong winds on this day acted to dry fuels even further, leading to a re-invigoration of the long-lived fire.<\/p>\n<div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190817_PAWD_SFCMG.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190817_PAWD_SFCMG.GIF\" alt=\"Time series of surface reports from Seward, Alaska [click to enlarge]\" width=\"642\" height=\"481\" \/><\/a><p class=\"wp-caption-text\">Time series of surface report data from Seward, Alaska [click to enlarge]<\/p><\/div>\n<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190817_2358utc_Seward_airport_webcam.png\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190817_2358utc_Seward_airport_webcam.png\" alt=\"Seward Airport webcam image at 2358 UTC [click to enlarge]\" width=\"642\" height=\"482\" \/><\/a><p class=\"wp-caption-text\">Seward Airport webcam image at 2358 UTC [click to enlarge]<\/p><\/div>The PM2.5 Air Quality Index reached 427 at Cooper Landing, and 358 farther downwind at Seward<em><strong> (below)<\/strong><\/em>.<\/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\/2019\/08\/190817_Seward_AK_airQalityIndex.png\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190817_Seward_AK_airQalityIndex.png\" alt=\"Air Quality Index at Copper Landing and Seward [click to enlarge]\" width=\"639\" height=\"374\" \/><\/a><p class=\"wp-caption-text\">Air Quality Index at Copper Landing and Seward [click to enlarge]<\/p><\/div>The southward transport of smoke across the Seward area and out over the adjacent offshore waters of the Gulf of Alaska was evident in VIIRS True Color Red-Green-Blue (RGB) images from NOAA-20 and Suomi NPP, as viewed using <a href=\"http:\/\/realearth.ssec.wisc.edu\"><strong>RealEarth<\/strong><\/a> <em><strong>(below).<\/strong><\/em><\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190817_noaa20_suomiNPP_viirs_trueColor_SwanLakeFire_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190817_noaa20_suomiNPP_viirs_trueColor_SwanLakeFire_AK_anim.gif\" alt=\"VIIRS True Color RGB images from NOAA-20 and Suomi NPP [click to enlarge]\" width=\"640\" height=\"355\" \/><\/a><p class=\"wp-caption-text\">VIIRS True Color RGB images from NOAA-20 and Suomi NPP [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>1-minute Mesoscale Domain Sector GOES-17 (GOES-West) &#8220;Red&#8221; Visible (0.64 \u00b5m) and Shortwave Infrared (3.9 \u00b5m) images (above) revealed thick smoke and a pronounced thermal anomaly (hot pixels, darker black) associated with the Swan Lake Fire on the Kenai Peninsula in south-central Alaska on 17 August 2019. Later in the day, a few pyrocumulus jumps could [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":34085,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[7,6,80,45,3],"tags":[],"class_list":["post-34081","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-air-quality","category-fire-detection","category-goes-17","category-redgreenblue-rgb-images","category-severe-convection"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/34081","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=34081"}],"version-history":[{"count":24,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/34081\/revisions"}],"predecessor-version":[{"id":34106,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/34081\/revisions\/34106"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/34085"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=34081"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=34081"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=34081"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}