{"id":10914,"date":"2012-07-25T23:59:00","date_gmt":"2012-07-25T23:59:00","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=10914"},"modified":"2012-07-28T02:09:35","modified_gmt":"2012-07-28T02:09:35","slug":"saharan-dust-over-the-south-florida-and-the-adjacent-offshore-waters","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/10914","title":{"rendered":"Saharan dust over South Florida and the adjacent offshore waters"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/07\/120725_g13_vis_sal_dust_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-13 0.63 \u00c2\u00b5m visible channel images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/07\/120725_g13_vis_sal_dust_anim.gif\" alt=\"GOES-13 0.63 \u00c2\u00b5m visible channel images\" width=\"480\" height=\"468\" \/><\/a><p class=\"wp-caption-text\">GOES-13 0.63 \u00c2\u00b5m visible channel images<\/p><\/div>\n<p>McIDAS images of GOES-13 0.63 \u00c2\u00b5m visible channel data <em><strong>(above)<\/strong><\/em> showed the hazy signature of a dense veil of airborne Saharan dust over South Florida and the adjacent offshore waters of the Gulf of Mexico and the Atlantic Ocean on <a title=\"25 July 2012 daily weather map\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20120725.html\"><strong>25 July 2012<\/strong><\/a>. This particular major pulse of Saharan dust began to move westward across the Atlantic Ocean <a title=\"Saharan dust outbreak (CIMSS Satellite Blog)\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/10799\"><strong>during mid-July<\/strong><\/a>.<\/p>\n<p>A closer view using an AWIPS image of Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel data<em><strong> (below)<\/strong><\/em> also showed the hazy signature of the dust over the southeastern portion of the satellite scene. A pilot reported flight visibility of 4 to 5 statute miles within the dust layer over the Florida Keys.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/07\/120725_suomi_npp_viirs_vis_FL_SAL_PIREP.png\"><img loading=\"lazy\" decoding=\"async\" title=\"Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel image + Pilot reports\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/07\/120725_suomi_npp_viirs_vis_FL_SAL_PIREP.png\" alt=\"Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel image + Pilot reports\" width=\"480\" height=\"304\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel image + Pilot reports<\/p><\/div>\n<p>A comparison of the VIIRS 0.64 \u00c2\u00b5m visible image with the corresponding VIIRS 11.45 \u00c2\u00b5m IR image <em><strong>(below)<\/strong><\/em> demonstrated that there was no dust signal at that particular IR wavelength, due to the fact tht an elevated dust layer is generally transparent to thermal radiation from the land and ocean surfaces below.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/07\/120725_suomi_npp_viirs_vis_ir_FL_SAL_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel + 11.45 \u00c2\u00b5m IR channel images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/07\/120725_suomi_npp_viirs_vis_ir_FL_SAL_anim.gif\" alt=\"Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel + 11.45 \u00c2\u00b5m IR channel images\" width=\"480\" height=\"304\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel + 11.45 \u00c2\u00b5m IR channel images<\/p><\/div>\n<p>The VIIRS Aerosol Optical Thickness product <em><strong>(below)<\/strong><\/em> showed a strong signal <em>(yellow to red color enhancement)<\/em> over that region due to the presence of the airborne dust. Yet another strong pulse of Saharan dust could be seen exiting\u00c2\u00a0 the coast of Africa and moving westward across the Atlantic Ocean,<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/07\/120725_viirs_aot.png\"><img loading=\"lazy\" decoding=\"async\" title=\"Suomi NPP VIIRS Aerosol Optical Thickness product\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/07\/120725_viirs_aot.png\" alt=\"Suomi NPP VIIRS Aerosol Optical Thickness product\" width=\"480\" height=\"307\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS Aerosol Optical Thickness product<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>McIDAS images of GOES-13 0.63 \u00c2\u00b5m visible channel data (above) showed the hazy signature of a dense veil of airborne Saharan dust over South Florida and the adjacent offshore waters of the Gulf of Mexico and the Atlantic Ocean on 25 July 2012. This particular major pulse of Saharan dust began to move westward across [&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":[7,21,11,49,48],"tags":[],"class_list":["post-10914","post","type-post","status-publish","format-standard","hentry","category-air-quality","category-aviation","category-goes-13","category-suomi_npp","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/10914","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=10914"}],"version-history":[{"count":5,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/10914\/revisions"}],"predecessor-version":[{"id":10917,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/10914\/revisions\/10917"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=10914"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=10914"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=10914"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}