{"id":15100,"date":"2014-03-11T23:59:02","date_gmt":"2014-03-11T23:59:02","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=15100"},"modified":"2014-03-19T23:39:52","modified_gmt":"2014-03-19T23:39:52","slug":"dust-storm-over-the-central-and-southern-high-plains-region","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/15100","title":{"rendered":"Dust storm over the central and southern High Plains region"},"content":{"rendered":"<div style=\"width: 493px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140311_goes13_visible_blowing_dust_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-13 0.63 \u00c2\u00b5m visible channel images (click to play animation)\" alt=\"GOES-13 0.63 \u00c2\u00b5m visible channel images (click to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/Reg_Vis_Sat_20140311_2345.png\" width=\"483\" height=\"314\" \/><\/a><p class=\"wp-caption-text\">GOES-13 0.63 \u00c2\u00b5m visible channel images (click to play animation)<\/p><\/div>\n<p>AWIPS images of GOES-13 0.63 \u00c2\u00b5m visible channel data <em><strong>(above; click image to play animation)<\/strong><\/em> show the hazy signature of an intense dust storm (sometimes locally referred to as a &#8220;haboob&#8221;) created by strong winds in the wake of a <a title=\"southward-moving cold front\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140311_g13_vis_surface_fronts_anim.gif\"><strong>southward-moving cold front<\/strong><\/a> on <a title=\"11 March 2014 daily weather map\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20140311.html\"><strong>11 March 2014<\/strong><\/a>. This blowing dust reduced surface visibility to zero in parts of southwestern Kansas <em>(where there were wind gusts of 59 mph),<\/em> causing several traffic accidents. At Amarillo, Texas (KAMA) the wind gusted to 60 mph, and visibility was reduced to 0.25 mile at times. A <a title=\"pilot report of blowing dust top\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140311_2015z_g13_vis_pirep_dust_top_fl110.jpg\"><strong>pilot report<\/strong><\/a> indicated that the top of the blowing dust was as high as 11,000 feet over the Oklahoma panhandle region.<\/p>\n<p>A sequence of Terra\/Aqua MODIS and Suomi NPP VIIRS true-color Red\/Green\/Blue (RGB) images visualized using the <a title=\"SSEC RealEarth web map server\" href=\"http:\/\/wms.ssec.wisc.edu\/\"><strong>SSEC RealEarth<\/strong><\/a> web map server <em><strong>(below)<\/strong><\/em> showed the southward advancement of the lighter tan colored areas of blowing dust.<\/p>\n<div style=\"width: 489px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140311_modis_viirs_truecolor_blowing_dust_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"Terra\/Aqua MODIS and Suomi NPP VIIRS true-color RGB images\" alt=\"Terra\/Aqua MODIS and Suomi NPP VIIRS true-color RGB images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140311_modis_viirs_truecolor_blowing_dust_anim.gif\" width=\"479\" height=\"303\" \/><\/a><p class=\"wp-caption-text\">Terra\/Aqua MODIS and Suomi NPP VIIRS true-color RGB images<\/p><\/div>\n<p>A signal of the airborne dust <em>(cyan color enhancement)<\/em> was also seen on Terra\/Aqua MODIS images of the 11-12 \u00c2\u00b5m &#8220;<a title=\"&quot;reverse absorption&quot;\" href=\"http:\/\/journals.ametsoc.org\/doi\/full\/10.1175\/JTECH1926.1\"><strong>reverse absorption<\/strong><\/a>&#8221; IR difference product <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 489px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140311_modis_11-12_ir_difference_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"MODIS 11-12 \u00c2\u00b5m &quot;reverse absorption&quot; IR difference product\" alt=\"MODIS 11-12 \u00c2\u00b5m &quot;reverse absorption&quot; IR difference product\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140311_modis_11-12_ir_difference_anim.gif\" width=\"479\" height=\"312\" \/><\/a><p class=\"wp-caption-text\">MODIS 11-12 \u00c2\u00b5m &#8220;reverse absorption&#8221; IR difference product<\/p><\/div>\n<p>GOES-13 6.5 \u00c2\u00b5m water vapor channel images <em><strong>(below; click image to play animation)<\/strong><\/em> showed the development of a &#8220;cirrus bloom&#8221; over far northeastern New Mexico as the surface cold front and blowing dust moved through that region. It is interesting to note that there was a <a title=\"pilot report of severe turbulence at 45,000 feet\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140311_2231z_g13_vis_pirep_sev_turb_fl450.jpg\"><strong>pilot report<\/strong><\/a>\u00c2\u00a0of severe turbulence at an altitude of 45,000 feet around that time (reportedly due to a mountain wave) &#8212; this raises the question as to whether a vertically-propagating wave generated by the strong cold front might have caused that high-altitude turbulence.<\/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\/2014\/03\/140311_g13_wv_blowing_dust_pirep_sev_turb_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-13 6.5 \u00c2\u00b5m water vapor channel images, with pilot reports of turbulence (click to play animation)\" alt=\"GOES-13 6.5 \u00c2\u00b5m water vapor channel images, with pilot reports of turbulence (click to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/Reg_Water_Vapor_20140311_2231.png\" width=\"480\" height=\"312\" \/><\/a><p class=\"wp-caption-text\">GOES-13 6.5 \u00c2\u00b5m water vapor channel images, with pilot reports of turbulence (click to play animation)<\/p><\/div>\n<p>Additional satellite images of this event can be found on the <a title=\"Wide World of SPoRT blog\" href=\"http:\/\/nasasport.wordpress.com\/2014\/03\/11\/dust-storm-shown-by-viirs-and-modis-in-southwest-2014\/\"><strong>Wide World of SPoRT<\/strong><\/a> blog.<\/p>\n<p style=\"text-align: center;\"><strong>===== 12 March Update =====<\/strong><\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140312_0835z_suomi_npp_viirs_dnb_blowing_dust_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band image, with surface observations and frontal analysis\" alt=\"Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band image, with surface observations and frontal analysis\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140312_0835z_suomi_npp_viirs_dnb_blowing_dust_anim.gif\" width=\"480\" height=\"288\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band image, with surface observations and frontal analysis<\/p><\/div>\n<p>During the subsequent night-time hours, a Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band image at 08:35 UTC or 2:35 AM local time <em><strong>(above)<\/strong><\/em> displayed a signature of the airborne dust over far southwestern Texas &#8212; the glow of the city lights below the dust layer was more diffuse than in dust-free areas farther to the east in central Texas. Also note that an <a title=\"undular bore\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/VIIRS_DNB__REF_20140312_0835_undular_bore.png\"><strong>undular bore<\/strong><\/a> had formed along the cold frontal boundary near the coast of southeast Texas.<\/p>\n<p>A comparison of the VIIRS Day\/Night Band image with a MODIS 11-12 \u00c2\u00b5m image <em><strong>(below)<\/strong><\/em> confirmed the presence of airborne dust over southwestern Texas. As in the MODIS example above, the brighter cyan color enhancement was a signal of dust.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140312_09z_viirs_modis_blowing_dust_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band and MODIS 11-12 \u00c2\u00b5m IR difference product images\" alt=\"Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band and MODIS 11-12 \u00c2\u00b5m IR difference product images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140312_09z_viirs_modis_blowing_dust_anim.gif\" width=\"480\" height=\"288\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band and MODIS 11-12 \u00c2\u00b5m IR difference product images<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>AWIPS images of GOES-13 0.63 \u00c2\u00b5m visible channel data (above; click image to play animation) show the hazy signature of an intense dust storm (sometimes locally referred to as a &#8220;haboob&#8221;) created by strong winds in the wake of a southward-moving cold front on 11 March 2014. This blowing dust reduced surface visibility to zero [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":15101,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[7,21,11,12,53,45,49,48],"tags":[],"class_list":["post-15100","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-air-quality","category-aviation","category-goes-13","category-modis","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\/15100","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=15100"}],"version-history":[{"count":19,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/15100\/revisions"}],"predecessor-version":[{"id":15181,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/15100\/revisions\/15181"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/15101"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=15100"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=15100"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=15100"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}