{"id":8355,"date":"2011-06-20T23:59:00","date_gmt":"2011-06-20T23:59:00","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=8355"},"modified":"2011-06-23T21:43:46","modified_gmt":"2011-06-23T21:43:46","slug":"pyrocumulus-clouds-and-dense-smoke-from-fires-in-georgia","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/8355","title":{"rendered":"Pyrocumulus clouds and dense smoke from fires in Georgia"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110620_g13_vis_ga_fire_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-13 0.63 \u00c2\u00b5m visible channel images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110620_G13_VIS_GA_FIRE_54.GIF\" alt=\"GOES-13 0.63 \u00c2\u00b5m visible channel images (click image to play animation)\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-13 0.63 \u00c2\u00b5m visible channel images (click image to play animation)<\/p><\/div>\n<p>McIDAS images of GOES-13 0.63 \u00c2\u00b5m visible channel data <strong><em>(above; click image to play animation)<\/em><\/strong> revealed numerous pyrocumulus clouds and large areas of very dense smoke associated with the &#8220;Honey Prairie Fire&#8221; in the Okefenokee Swamp area of southeastern Georgia on <a title=\"20 June 2011 daily weather map\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20110620.html\"><strong>20 June 2011<\/strong><\/a>. The shadows cast by the pyrocumulus towers almost resembled those cast by overshooting tops which are often seen on the anvil tops of severe thunderstorms.<\/p>\n<p>A sequence of 3 AWIPS images of POES AVHRR 0.63 \u00c2\u00b5m visible channel data <strong><em>(below)<\/em><\/strong> offered a larger-scale view of the smoke as it drifted eastward across the adjacent offshore waters of the Atlantic Ocean. The shadow cast by a pyrocumulus tower could be seen on the final 21:22 UTC image. As expected, this dense smoke plume exhibited very high Aerosol Optical Depth (AOD) values (see the <a title=\"US Air Quality Smog Blog\" href=\"http:\/\/alg.umbc.edu\/usaq\/archives\/004214.html\"><strong>US Air Quality &#8220;Smog Blog&#8221;<\/strong><\/a> and the <a title=\"NOAA IDEA\" href=\"http:\/\/www.star.nesdis.noaa.gov\/smcd\/spb\/aq\/index.php?plot_year=2011&amp;plot_month=06&amp;plot_day=20&amp;plot_gmt=0015&amp;product_gmt=0015&amp;plot_type=mod_Region&amp;region=04&amp;product_date=20110619&amp;product_id=0&amp;goto_date=Go\"><strong>NOAA IDEA<\/strong><\/a> sites for AOD imagery).<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110620_poes_avhrr_vis_ga_fire_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"POES AVHRR 0.63 \u00c2\u00b5m visible channel images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110620_poes_avhrr_vis_ga_fire_anim.gif\" alt=\"POES AVHRR 0.63 \u00c2\u00b5m visible channel images\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">POES AVHRR 0.63 \u00c2\u00b5m visible channel images<\/p><\/div>\n<p>The 21:22 UTC POES AVHRR 10.8 \u00c2\u00b5m IR image <strong><em>(below)<\/em><\/strong> showed that the coldest cloud top IR brightness temperatures at that time were -18\u00c2\u00ba C, which corresponded to an altitude of nearly 24,000 feet using the interactive Skew-T diagram with data from the rawinsonde report from Charleston, South Carolina.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110620_avhrr_ir_skewt.jpg\"><img loading=\"lazy\" decoding=\"async\" title=\"POES AVHRR 10.8 \u00c2\u00b5m IR image + interactive Skew-T for Charleston SC rawinsonde\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110620_avhrr_ir_skewt.jpg\" alt=\"POES AVHRR 10.8 \u00c2\u00b5m IR image + interactive Skew-T for Charleston SC rawinsonde\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">POES AVHRR 10.8 \u00c2\u00b5m IR image + interactive Skew-T for Charleston SC rawinsonde<\/p><\/div>\n<p>&nbsp;<\/p>\n<p style=\"text-align: center;\"><strong>=====================================================<\/strong><\/p>\n<p>&nbsp;<\/p>\n<p>On the following day (<a title=\"21 June 2011 daily weather map\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20110621.html\"><strong>21 June 2011<\/strong><\/a>) the winds were much lighter across the region, so the smoke was not being transported as far eastward over the Atlantic Ocean. In fact, GOES-13 0.63 \u00c2\u00b5m visible channel images <em><strong>(below; click image to play animation)<\/strong><\/em> showed that significant amounts of the smoke remained just offshore &#8212; so when a sea breeze front began to move inland during the afternoon hours, much of this smoke was brought back inland. For example, at St. Augustine, Florida <em>(surface identifier KSGJ),<\/em> the surface visibility dropped from 10 miles to 0.75 mile after the surface winds shifted to easterly behind the sea breeze front.<\/p>\n<p style=\"text-align: center;\">&nbsp;<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110621_g13_vis_ga_smoke_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"GOES-13 0.63 \u00c2\u00b5m visible channel images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110621_G13_VIS_GA_SMOKE_35.GIF\" alt=\"GOES-13 0.63 \u00c2\u00b5m visible channel images (click image to play animation)\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-13 0.63 \u00c2\u00b5m visible channel images (click image to play animation)<\/p><\/div>\n<p style=\"text-align: center;\">&nbsp;<\/p>\n<p style=\"text-align: center;\"><strong>=====================================================<\/strong><\/p>\n<p>&nbsp;<\/p>\n<p>A sequence of 250-meter resolution MODIS <a title=\"true color Red\/Green\/Blue (RGB) images\" href=\"http:\/\/lance.nasa.gov\/imagery\/rapid-response\/frequently-asked-questions\/#faq04\"><strong>true color<\/strong><\/a> Red\/Green\/Blue (RGB) images from the <a title=\"SSEC MODIS Today site\" href=\"http:\/\/ge.ssec.wisc.edu\/modis-today\/index.php?satellite=a1&amp;product=true_color&amp;date=2011_06_22_173&amp;overlay_sector=false&amp;overlay_state=true&amp;overlay_coastline=true\"><strong>SSEC MODIS Today<\/strong><\/a> site <em><strong>(below; displayed using Google Earth)<\/strong><\/em> showed varying regimes of transport of the thick smoke on 19 June, 20 June, 21 June, and 22 June 2011.<\/p>\n<p>&nbsp;<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110619-22_modis_truecolor_ga_smoke_google_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"MODIS true color RGB images (displayed using Google Earth)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/06\/110619-22_modis_truecolor_ga_smoke_google_anim.gif\" alt=\"MODIS true color RGB images (displayed using Google Earth)\" width=\"480\" height=\"332\" \/><\/a><p class=\"wp-caption-text\">MODIS true color RGB images (displayed using Google Earth)<\/p><\/div>\n<p><strong> <\/strong><\/p>\n<p><strong> <\/strong><\/p>\n<p><strong><br \/>\n<\/strong><\/p>\n","protected":false},"excerpt":{"rendered":"<p>McIDAS images of GOES-13 0.63 \u00c2\u00b5m visible channel data (above; click image to play animation) revealed numerous pyrocumulus clouds and large areas of very dense smoke associated with the &#8220;Honey Prairie Fire&#8221; in the Okefenokee Swamp area of southeastern Georgia on 20 June 2011. The shadows cast by the pyrocumulus towers almost resembled those cast [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[7,22,6,11,32,12,26,45],"tags":[],"class_list":["post-8355","post","type-post","status-publish","format-standard","hentry","category-air-quality","category-avhrr","category-fire-detection","category-goes-13","category-google-earth","category-modis","category-poes","category-redgreenblue-rgb-images"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/8355","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=8355"}],"version-history":[{"count":13,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/8355\/revisions"}],"predecessor-version":[{"id":8357,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/8355\/revisions\/8357"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=8355"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=8355"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=8355"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}