{"id":51261,"date":"2023-03-22T23:59:00","date_gmt":"2023-03-22T23:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=51261"},"modified":"2023-03-24T21:48:18","modified_gmt":"2023-03-24T21:48:18","slug":"blowing-dust-across-mongolia-and-china-2","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/51261","title":{"rendered":"Blowing dust across Mongolia and China"},"content":{"rendered":"<p><div style=\"width: 2010px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230320_230322_himawari9_dustRGB_China_Mongolia_blowing_dust_anim.mp4\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/Himawari-9_AHI_FLDK_dust_2023080_180000Z.png\" alt=\"\" width=\"2000\" height=\"1000\" \/><\/a><p class=\"wp-caption-text\">Himawari-9 Dust RGB images, from 2100 UTC on 20 March to 2350 UTC on 22 March [click to play MP4 animation]<\/p><\/div><a href=\"https:\/\/www.jma.go.jp\/jma\/indexe.html\"><strong>JMA<\/strong><\/a> Himawari-9 <a href=\"https:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/Dust_RGB_Quick_Guide.pdf\"><strong>Dust RGB<\/strong><\/a> images created using <a href=\"https:\/\/www.ssec.wisc.edu\/software\/geo2grid\/\"><strong>Geo2Grid<\/strong><\/a> <em><strong>(above)<\/strong><\/em> spanned the period from 2100 UTC on 20 March to 2350 UTC on 22 March 2023 &#8212; and showed a large area of dense blowing dust (brighter shades of magenta to pink) across parts of eastern Mongolia and northern\/northeastern China (eventually crossing the China\/Russia border). This <a href=\"https:\/\/en.wikipedia.org\/wiki\/Gobi_Desert\"><strong>Gobi Desert<\/strong><\/a> dust was lofted by strong winds produced by the tight pressure gradient between high pressure that was moving from Russia into western Mongolia and low pressure that was drifting from eastern Mongolia to northeastern China (<a href=\"https:\/\/www.kma.go.kr\/eng\/index.jsp\"><strong>KMA<\/strong><\/a> surface analyses: <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230321_230322_Asia_surface_analyses_anim.gif\"><strong>GIF<\/strong><\/a> | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230321_230322_Asia_surface_analyses_anim.mp4\"><strong>MP4<\/strong><\/a>).<\/p>\n<p>A <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230319_230322_himawari9_dustRGB_China_Mongolia_blowing_dust_anim.mp4\"><strong>longer Dust RGB animation<\/strong><\/a> showed an additional pulse of blowing dust originating from the <a href=\"https:\/\/en.wikipedia.org\/wiki\/Taklamakan_Desert\"><strong>Taklamakan Desert<\/strong><\/a> on 19 March.<\/p>\n<p>The Himawari-9 <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_SplitWindowDifference.pdf\"><strong>Split Window Difference<\/strong><\/a> product <em><strong>(below)<\/strong><\/em> showed that this blowing dust (brighter shades of yellow to cyan\/blue to red) restricted the surface visibility to 1 mile or less at some sites during the period from 0000 UTC on 21 March to 0000 UTC on 23 March.<\/p>\n<div style=\"width: 2010px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230321_230322_himawari9_splitWindowDifference_Mongolia_China_blowing_dust_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/HIM09_B13_B15_SWD_BLDN_MONGOLIA_CHINA_21_22MAR2023_Bk_2023080_180000_0001PANEL_FRAME00107.GIF\" alt=\"\" width=\"2000\" height=\"1200\" \/><\/a><p class=\"wp-caption-text\">Himawari-9 Split Window Difference product, from 0000 UTC on 21 March to 0000 UTC on 23 March [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230321_230322_himawari9_splitWindowDifference_Mongolia_China_blowing_dust_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p><div style=\"width: 1810px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230320_230321_himawari9_trueColorRGB_Mongolia_China_blowing_dust_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/Himawari-9_AHI_FLDK_true_color_2023080_080000Z.png\" width=\"1800\" height=\"1300\" \/><\/a><p class=\"wp-caption-text\">Himawari-9 True Color RGB images, from 2210 UTC on 20 March to 0950 UTC on 21 March [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230320_230321_himawari9_trueColorRGB_Mongolia_China_blowing_dust_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Himawari-9 True Color RGB images <em><strong>(above)<\/strong><\/em> showed the initial formation of blowing dust plmes (shades of tan) from 2210 UTC on 20 March to 0950 UTC on 21 March &#8212; which later became entrained into the aforementioned low pressure system (as it was centered over far northeastern China) during the period from 2210 UTC on 21 March to 0950 UTC on 22 March <em><strong>(below)<\/strong><\/em>. An animation which combines these 2 daytime periods (20-21 March, and 21-22 March) is available <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230320_230322_himawari9_trueColorRGB_Mongolia_China_blowing_dust_anim.mp4\"><strong>here<\/strong><\/a>.<\/p>\n<p><div style=\"width: 1810px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230321_230322_himawari9_trueColorRGB_Mongolia_China_blowing_dust_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/Himawari-9_AHI_FLDK_true_color_2023081_082000Z.png\" width=\"1800\" height=\"1300\" \/><\/a><p class=\"wp-caption-text\">Himawari-9 True Color RGB images, from 2210 UTC on 21 March to 0950 UTC on 22 March [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/03\/230321_230322_himawari9_trueColorRGB_Mongolia_China_blowing_dust_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Similar cases of dust entrainment into the circulation of a midlatitude cyclone in this region were documented in blog posts from <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/40860\"><strong>May 2021<\/strong><\/a> and <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/33237\"><strong>May 2019<\/strong><\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>JMA Himawari-9 Dust RGB images created using Geo2Grid (above) spanned the period from 2100 UTC on 20 March to 2350 UTC on 22 March 2023 &#8212; and showed a large area of dense blowing dust (brighter shades of magenta to pink) across parts of eastern Mongolia and northern\/northeastern China (eventually crossing the China\/Russia border). This [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":51272,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[7,132,73,45],"tags":[],"class_list":["post-51261","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-air-quality","category-geo2grid","category-himawari-9","category-redgreenblue-rgb-images"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/51261","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=51261"}],"version-history":[{"count":15,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/51261\/revisions"}],"predecessor-version":[{"id":51287,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/51261\/revisions\/51287"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/51272"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=51261"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=51261"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=51261"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}