{"id":34387,"date":"2019-09-20T23:59:40","date_gmt":"2019-09-20T23:59:40","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=34387"},"modified":"2020-12-15T16:44:43","modified_gmt":"2020-12-15T16:44:43","slug":"saharan-air-layer-plume-over-the-atlantic-ocean","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/34387","title":{"rendered":"Saharan Air Layer plume over the Atlantic Ocean"},"content":{"rendered":"<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/09\/190915_190920_Atlantic_SaharanAirLayer_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/09\/20190920_18z_SAL.jpg\" alt=\"Saharan Air Layer product [click to play animation | MP4]\" width=\"641\" height=\"341\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Split Window&#8221; Saharan Air Layer product [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/09\/190915_190920_Atlantic_SaharanAirLayer_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-16<em> (GOES-East)<\/em> <a href=\"http:\/\/tropic.ssec.wisc.edu\/misc\/sal\/info.sal.g16split.html\"><strong>Split Window<\/strong><\/a> images <em><strong>(above)<\/strong><\/em> showed a large plume of the Saharan Air Layer (SAL) that moved westward off the coast of Africa then westward and northwestward across the eastern and central Atlantic Ocean during the 15-20 September 2019 period.<\/p>\n<p>On 20 September, the hazy SAL plume could be easily seen in Full Disk GOES-16 True Color Red-Green-Blue (RGB) images from the <a href=\"http:\/\/www.aos.wisc.edu\/weather\/wx_obs\/GOES16.html\"><strong>AOS<\/strong><\/a> site <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/09\/190920_goes16_truecolor_fulldisk_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/09\/201909201500_fulldisk.jpg\" alt=\"GOES-16 True Color images [click to play animation | MP4]\" width=\"641\" height=\"641\" \/><\/a><p class=\"wp-caption-text\">GOES-16 True Color RGB images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/09\/190920_goes16_truecolor_fulldisk_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>The SAL plume was also apparent in True Color RGB images from Suomi NPP and NOAA-20 as viewed using <a href=\"http:\/\/realearth.ssec.wisc.edu\"><strong>RealEarth<\/strong><\/a> <em><strong>(below)<\/strong><\/em>.<\/p>\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\/09\/190920_15utc_suomiNPP_16utc_noaa20_viirs_trueColor_SAL_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/09\/190920_15utc_suomiNPP_16utc_noaa20_viirs_trueColor_SAL_anim.gif\" width=\"642\" height=\"375\" \/><\/a><p class=\"wp-caption-text\">VIIRS True Color RGB images from Suomi NPP and NOAA-20 [click to enlarge]<\/p><\/div>A comparison of GOES-16 <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_CIMSSRGB_v2.pdf\"><strong>CIMSS Natural Color RGB<\/strong><\/a>, <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_BaselineAerosolDetection.pdf\"><strong>Aerosol Optical Depth<\/strong><\/a> and <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_BaselineAerosolDetection.pdf\"><strong>Dust Detection<\/strong><\/a> product images from 1500-1900 UTC on 20 September <em><strong>(below)<\/strong><\/em> revealed AOD values as high as 0.5 within the hazy dust-laden SAL plume; the Dust Detection product indicated large areas of Low- to Medium-Confidence dust (with isolated pockets of High Confidence).<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/09\/190920_goes16_naturalColor_aerosolOpticalDepth_dustDetection_Atlantic_SAL_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/09\/sal_natcolor-20190920_180019.png\" alt=\"GOES-16 CIMSS Natural Color RGB, Aerosol Optical Depth, and Dust Detection product [click to play animation | MP4]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">GOES-16 CIMSS Natural Color RGB, Aerosol Optical Depth, and Dust Detection product [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/09\/190920_goes16_naturalColor_aerosolOpticalDepth_dustDetection_Atlantic_SAL_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div><center><\/p>\n<blockquote class=\"twitter-tweet\">\n<p dir=\"ltr\" lang=\"en\">Yes, that&#8217;s quite a plume. Here&#8217;s the <a href=\"https:\/\/twitter.com\/hashtag\/SNPP?src=hash&amp;ref_src=twsrc%5Etfw\">#SNPP<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/OMPS?src=hash&amp;ref_src=twsrc%5Etfw\">#OMPS<\/a> aerosol index from yesterday that shows how big it is. <a href=\"https:\/\/t.co\/WrQjRMZwRK\">pic.twitter.com\/WrQjRMZwRK<\/a><\/p>\n<p>\u2014 Colin Seftor (@colin_seftor) <a href=\"https:\/\/twitter.com\/colin_seftor\/status\/1175331110693330944?ref_src=twsrc%5Etfw\">September 21, 2019<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/center><br \/>\nOn a side note, the Full Disk True Color shown above images revealed 3 different types of solar backscatter: a small spot of very bright sun glint off the water of the Amazon River and its tributaries, which moved from east to west &#8212; similar to this example from October 2018\u00a0 <em><strong>(below)<\/strong><\/em><\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/09\/190920_goes16_visible_Amazon_sun_glint_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/09\/G16_FD_VIS_SOAM_SUNGLINT_20SEP2018_B2_2018274_143022_GOES-16_0001PANEL_FRAME00031.GIF\" alt=\"GOES-16 \" width=\"641\" height=\"481\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible <em>(0.64 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/09\/190920_goes16_visible_Amazon_sun_glint_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>along with 2 separate (and larger) areas of more diffuse solar backscatter, which propagated from west to east: the first (possibly a 180\u00ba-42\u00ba=138\u00ba or &#8220;rainbow&#8221; backscatter) appeared about midway between the Equator and the southern tip of South America &#8212; and the second\u00a0 (a 180\u00ba backscatter) appeared farther north, closer to the Equator, slightly later in time (this type of solar backscatter was previously discussed <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/27238\"><strong>here<\/strong><\/a>). These 3 solar backscatter features can also be seen in a rocking animation below.<\/p>\n<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\/09\/190920_goes16_truecolor_fulldisk_backscatter_rock_v2_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/09\/201909201500_fulldisk.jpg\" alt=\"GOES-16 True Color RGB images [click to play animation | MP4]\" width=\"642\" height=\"642\" \/><\/a><p class=\"wp-caption-text\">GOES-16 True Color RGB images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/09\/190920_goes16_truecolor_fulldisk_backscatter_rock_v2_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Thanks to Fred Wu (NOAA\/NESDIS) and Steve Miller (CIRA) for providing further insight regarding the nature of the 2 larger types of solar backscatter.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>GOES-16 (GOES-East) Split Window images (above) showed a large plume of the Saharan Air Layer (SAL) that moved westward off the coast of Africa then westward and northwestward across the eastern and central Atlantic Ocean during the 15-20 September 2019 period. On 20 September, the hazy SAL plume could be easily seen in Full Disk [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":34389,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[74,78,53,45,49,48],"tags":[],"class_list":["post-34387","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-16","category-noaa-20","category-real-earth","category-redgreenblue-rgb-images","category-suomi_npp","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/34387","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=34387"}],"version-history":[{"count":19,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/34387\/revisions"}],"predecessor-version":[{"id":39250,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/34387\/revisions\/39250"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/34389"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=34387"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=34387"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=34387"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}