{"id":35517,"date":"2020-01-24T23:59:25","date_gmt":"2020-01-24T23:59:25","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=35517"},"modified":"2020-02-01T02:23:20","modified_gmt":"2020-02-01T02:23:20","slug":"stratospheric-smoke-from-australian-bushfires","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/35517","title":{"rendered":"Stratospheric smoke from Australian bushfires"},"content":{"rendered":"<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200119_200124_goes16_nearInfraredCirrus_Australian_fire_smoke_South_Pacific_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/G16_CIRRUS_SH_SMOKE_AUS_FIRES_24JAN2020_B4_2020021_110017_GOES-16_0001PANEL_FRAME00355.GIF\" alt=\"GOES-16 Near-Infrared \" width=\"641\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Near-Infrared &#8220;Cirrus&#8221;<em> (1.37 \u00b5m)<\/em> images, 19-24 January 2019 [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200119_200124_goes16_nearInfraredCirrus_Australian_fire_smoke_South_Pacific_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-16<em> (GOES-East)<\/em> Near-Infrared &#8220;Cirrus&#8221; (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band04.pdf\"><strong>1.37 \u00b5m<\/strong><\/a>) images during the 19-24 January 2019 period <em><strong>(above)<\/strong><\/em> showed a semi-circular pall of smoke that originated from Australian bushfires\u00a0 &#8212; outbreaks of pyrocumulonimbus clouds that occurred in <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/35283\"><strong>late December 2019<\/strong><\/a> and <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/35342\"><strong>early January 2020<\/strong><\/a> injected large amounts of smoke into the lower stratosphere, and this smoke drifted eastward across the South Pacific Ocean. The 1.37 \u00b5m spectral band does a good job at detecting light scattered by airborne particles such as ice crystals, smoke, volcanic ash, dust, etc.; the areal extent of the smoke was most apparent approaching sunset on each day, due to enhanced forward scattering.<\/p>\n<p>CALIPSO satellite CALIOP lidar data indicated that this smoke often resided at altitudes in the 18-24 km range &#8212; one example from 21 January can be seen <a href=\"https:\/\/www-calipso.larc.nasa.gov\/products\/lidar\/browse_images\/show_detail.php?s=expedited&amp;v=V3-30&amp;browse_date=2020-01-21&amp;orbit_time=06-00-00&amp;page=3&amp;granule_name=CAL_LID_L1_Exp-Prov-V3-40.2020-01-21T06-00-00Z.hdf\"><strong>here<\/strong><\/a>. 12-hourly GOES-16 Cirrus images with plots of GFS model 70 hPa wind barbs during the 20-24 January 2019 period <em><strong>(below)<\/strong><\/em> showed that winds at the 70 hPa pressure level were generally light.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200124_12UTC_SCCI_RAOB_DATA.TEXT\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200120_200124_goes16_nearInfrared_cirrus_70hPa_winds_anim.gif\" alt=\"GOES-16 Near-Infrared &quot;Cirrus&quot; (1.37 \u00b5m) images, with plots of GFS model 70 hPa wind barbs (knots), 20-24 January 2019 [click to enlarge]\" width=\"641\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Near-Infrared &#8220;Cirrus&#8221; <em>(1.37 \u00b5m)<\/em> images, with plots of GFS model 70 hPa wind barbs <em>(knots),<\/em> 20-24 January 2019 [click to enlarge]<\/p><\/div>As the stratospheric smoke feature was beginning to move over the Punta Arena, Chile area <em>(station identifier SCCI),<\/em> <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200124_12UTC_SCCI_RAOB_DATA.TEXT\"><strong>rawinsonde data<\/strong><\/a> from that site indicated that the wind speed at 70 hPa (18.5 km) was 18 knots<em><strong> (below)<\/strong><\/em>.<\/p>\n<div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200124_SCCI_RAOB.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/01\/200124_SCCI_RAOB.GIF\" alt=\"Plot of rawinsonde data from Punta Arenas, Chile at 12 UTC on 24 January [click to enlarge]\" width=\"642\" height=\"482\" \/><\/a><p class=\"wp-caption-text\">Plot of rawinsonde data from Punta Arenas, Chile at 12 UTC on 24 January [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>GOES-16 (GOES-East) Near-Infrared &#8220;Cirrus&#8221; (1.37 \u00b5m) images during the 19-24 January 2019 period (above) showed a semi-circular pall of smoke that originated from Australian bushfires\u00a0 &#8212; outbreaks of pyrocumulonimbus clouds that occurred in late December 2019 and early January 2020 injected large amounts of smoke into the lower stratosphere, and this smoke drifted eastward across [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":35519,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[74],"tags":[],"class_list":["post-35517","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-16"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/35517","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=35517"}],"version-history":[{"count":5,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/35517\/revisions"}],"predecessor-version":[{"id":35525,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/35517\/revisions\/35525"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/35519"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=35517"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=35517"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=35517"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}