{"id":32816,"date":"2019-04-09T23:59:57","date_gmt":"2019-04-09T23:59:57","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=32816"},"modified":"2019-04-11T17:37:47","modified_gmt":"2019-04-11T17:37:47","slug":"blowing-dust-in-southern-nevada","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/32816","title":{"rendered":"Blowing dust in southern Nevada"},"content":{"rendered":"<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190409_goes17_splitWindowDifference_cloudTopPhase_visible_LAS_blowing_dust_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/las_ctp-20190409_234619.png\" alt=\"GOES-17 Split Window (10.3-12.3 \u00b5m), Split Cloud Top Phase (11.2-8.4 \u00b5m) and \" width=\"640\" height=\"370\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Split Window <em>(10.3-12.3 \u00b5m),<\/em> Split Cloud Top Phase<em> (11.2-8.4 \u00b5m)<\/em> and &#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\/04\/190409_goes17_splitWindowDifference_cloudTopPhase_visible_LAS_blowing_dust_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-17 <em>(GOES-West)<\/em> Split Window (<strong><a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_SplitWindowDifference.pdf\">10.3-12.3 \u00b5m<\/a><\/strong>), Split Cloud Top Phase (<strong><a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_G16_CloudPhaseBTD.pdf\">11.2-8.4 \u00b5m<\/a><\/strong>) and &#8220;Red&#8221; Visible (<strong><a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\">0.64 \u00b5m<\/a><\/strong>) images <em><strong>(above)<\/strong><\/em> displayed a plume of blowing dust &#8212; whose source region was a dry lake bed along the California-Nevada border &#8212; which developed in advance of an approaching cold front (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190409_surface_analyses_LAS_anim.gif\"><strong>surface analyses<\/strong><\/a>) and moved northeastward across far southern Nevada on 09 April 2019. <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190410_klas_pns.text\"><strong>Wind gusts<\/strong><\/a> of 50-65 mph were reported across the region.<\/p>\n<p>This dust plume was also apparent over far southern Nevada in GOES-17 True Color Red-Green-Blue (RGB) images from the <a href=\"https:\/\/www.aos.wisc.edu\/weather\/wx_obs\/GOES17.html\"><strong>AOS<\/strong><\/a> site <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190409_goes17_truecolor_LAS_blowing_dust_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/201904100016_sw.jpg\" alt=\"GOES-17 True Color RGB images [click to play animation | MP4]\" width=\"640\" height=\"435\" \/><\/a><p class=\"wp-caption-text\">GOES-17 True Color RGB images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190409_goes17_truecolor_LAS_blowing_dust_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>There are 5 airports located in the Las Vegas Valley, and GOES-17 images showed that the dust plume passed directly over Henderson (KHND) &#8212; time series plots of surface data from these sites <em><strong>(below)<\/strong><\/em> indicated that visibility was reduced to 3 miles at Henderson, with visibilities dropping to 8-9 miles at McCarran International Airport (KLAS) and Nellis Air Force Base (KLSV). The visibility was not impacted at the North Las Vegas Airport (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190409_KVGT_SFCMG.GIF\"><strong>KVGT<\/strong><\/a>), with its more northwest location being farther from the dust plume.<\/p>\n<p><div style=\"width: 649px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190409_KHND_SFCMG.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190409_KHND_SFCMG.GIF\" alt=\"Time series plot of surface data at Henderson [click to enlarge]\" width=\"639\" height=\"424\" \/><\/a><p class=\"wp-caption-text\">Time series plot of surface data at Henderson [click to enlarge]<\/p><\/div><div style=\"width: 649px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190409_KLAS_SFCMG.GIF\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190409_KLAS_SFCMG.GIF\" alt=\"Time series plot of surface data at McCarran International Airport [click to enlarge]\" width=\"639\" height=\"424\" \/><\/a><p class=\"wp-caption-text\">Time series plot of surface data at McCarran International Airport [click to enlarge]<\/p><\/div><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190409_KLSV_SFCMG.GIF\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190409_KLSV_SFCMG.GIF\" alt=\"Time series plot of surface data at Nellis Air Force Base [click to enlarge]\" width=\"643\" height=\"427\" \/><\/a><p class=\"wp-caption-text\">Time series plot of surface data at Nellis Air Force Base [click to enlarge]<\/p><\/div>A notable exception was the Boulder City Municipal Airport (KBVU), which was downwind of a smaller local point source of blowing dust (<strong><a href=\"https:\/\/www.google.com\/maps\/place\/Mursha+Reservoir\/@35.8722199,-114.9523522,3105m\/data=!3m2!1e3!4b1!4m5!3m4!1s0x80cf2a293b26ade7:0xf0da9d57908bd180!8m2!3d35.8722033!4d-114.9435974\">Mursha Reservoir<\/a><\/strong>, another dry lake bed to the southwest) &#8212; the visibility at KBVU was restricted to 2 miles at times. With the 2-km spatial resolution (at satellite nadir) of the GOES-17 Infrared spectral bands, there was not a signature of this smaller-scale Boulder City dust plume in the 10.3-12.3 \u00b5m and 11.2-8.4 \u00b5m Brightness Temperature Difference products &#8212; however, this hazy plume was evident in the 0.5-km resolution (at satellite nadir) <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190409_goes17_visible_LAS_blowing_dust_anim.gif\"><strong>Visible imagery<\/strong><\/a>.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190409_KBVU_SFCMG.GIF\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190409_KBVU_SFCMG.GIF\" alt=\"Time series plot of surface data at Boulder City Municipal Airport [click to enlarge]\" width=\"640\" height=\"425\" \/><\/a><p class=\"wp-caption-text\">Time series plot of surface data at Boulder City Municipal Airport [click to enlarge]<\/p><\/div>A comparison of 1-km resolution NOAA-19 AVHRR Visible (0.63 \u00b5m), Shortwave Infrared (3.8 \u00b5m) and Split Window (10.8-12.0 \u00b5m) images<em><strong> (below)<\/strong><\/em> provided a detailed view of the primary dust plume &#8212; and also exhibited a subtle signature of the smaller plume that reduced visibility at Boulder City KBVU. The small dust aerosols act as efficient reflectors of incoming solar radiation, therefore appearing warmer <em>(darker)<\/em> on the Shortwave Infrared image.<\/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\/04\/190409_2335utc_noaa19_visible_shortwaveInfrared_splitWindowDifference_LAS_blowing_dust_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/04\/190409_2335utc_noaa19_visible_shortwaveInfrared_splitWindowDifference_LAS_blowing_dust_anim.gif\" alt=\"NOAA-19 AVHRR Visible (0.63 \u00b5m), Shortwave Infrared (3.8 \u00b5m) and Split Window (10.8-12.0 \u00b5m) images, with plots of 23 UTC surface reports [click to enlarge]\" width=\"642\" height=\"426\" \/><\/a><p class=\"wp-caption-text\">NOAA-19 AVHRR Visible <em>(0.63 \u00b5m),<\/em> Shortwave Infrared<em> (3.8 \u00b5m)<\/em> and Split Window <em>(10.8-12.0 \u00b5m)<\/em> images, with plots of 23 UTC surface reports [click to enlarge]<\/p><\/div>The GOES-17 and NOAA-19 images also showed that the larger dust plume moved across a section of Interstate 15 between Sloan and Jean; traffic cameras showed significant reductions in visibility along I-15 near Primm (along the California\/Nevada border).<\/p>\n<p><center><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p dir=\"ltr\" lang=\"en\">Dust plume visible on <a href=\"https:\/\/twitter.com\/nevadadot?ref_src=twsrc%5Etfw\">@nevadadot<\/a> cam blowing across I-15 near the NV\/CA border! Be prepared for reduced visibility! <a href=\"https:\/\/twitter.com\/hashtag\/NVwx?src=hash&amp;ref_src=twsrc%5Etfw\">#NVwx<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/CAwx?src=hash&amp;ref_src=twsrc%5Etfw\">#CAwx<\/a> <a href=\"https:\/\/t.co\/hkwlgp9IzJ\">pic.twitter.com\/hkwlgp9IzJ<\/a><\/p>\n<p>\u2014 NWS Las Vegas (@NWSVegas) <a href=\"https:\/\/twitter.com\/NWSVegas\/status\/1115742882474885120?ref_src=twsrc%5Etfw\">April 9, 2019<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p dir=\"ltr\" lang=\"en\"><a href=\"https:\/\/twitter.com\/hashtag\/VegasWeather?src=hash&amp;ref_src=twsrc%5Etfw\">#VegasWeather<\/a> &#8211; it&#8217;s pretty bad out there in some areas. <a href=\"https:\/\/t.co\/mdzeGNnMSL\">https:\/\/t.co\/mdzeGNnMSL<\/a><\/p>\n<p>\u2014 Clark County Nevada (@ClarkCountyNV) <a href=\"https:\/\/twitter.com\/ClarkCountyNV\/status\/1115747975836225536?ref_src=twsrc%5Etfw\">April 9, 2019<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<p><\/center><\/p>\n","protected":false},"excerpt":{"rendered":"<p>GOES-17 (GOES-West) Split Window (10.3-12.3 \u00b5m), Split Cloud Top Phase (11.2-8.4 \u00b5m) and &#8220;Red&#8221; Visible (0.64 \u00b5m) images (above) displayed a plume of blowing dust &#8212; whose source region was a dry lake bed along the California-Nevada border &#8212; which developed in advance of an approaching cold front (surface analyses) and moved northeastward across far [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":32826,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[7,22,80,26,45],"tags":[],"class_list":["post-32816","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-air-quality","category-avhrr","category-goes-17","category-poes","category-redgreenblue-rgb-images"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/32816","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=32816"}],"version-history":[{"count":16,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/32816\/revisions"}],"predecessor-version":[{"id":32867,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/32816\/revisions\/32867"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/32826"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=32816"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=32816"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=32816"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}