{"id":39407,"date":"2020-12-24T22:59:45","date_gmt":"2020-12-24T22:59:45","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=39407"},"modified":"2020-12-27T21:20:24","modified_gmt":"2020-12-27T21:20:24","slug":"tehuano-wind-event-5","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/39407","title":{"rendered":"Tehuano wind event"},"content":{"rendered":"<p><div style=\"width: 655px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/12\/201224_goes16_visible_Tehuano_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/12\/tehuano_vis-20201224_210117.png\" alt=\"GOES-16 \" width=\"645\" height=\"301\" \/><\/a><p class=\"wp-caption-text\">Topography + 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\/images\/2020\/12\/201224_goes16_visible_Tehuano_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-16 <em>(GOES-East)<\/em> &#8220;Red&#8221; Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>) images<em><strong> (above)<\/strong><\/em> indicated that a strong arctic cold front (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/12\/201224_surface_analyses_anim.gif\"><strong>surface analyses<\/strong><\/a>) had plunged southward across Mexico, through the Chivela Pass, and emerged as a Tehuano (or &#8220;<a href=\"https:\/\/en.wikipedia.org\/wiki\/Tehuantepecer\"><strong>Tehuantepecer<\/strong><\/a>&#8220;) gap wind into the Gulf of Tehuantepec on 24 December 2020. Along the Gulf of Mexico coast, a few sites in Mexico reported blowing dust and\/or blowing sand with onshore winds gusting to 40 knots.<\/p>\n<p>GOES-16 True Color RGB images created using\u00a0<a href=\"https:\/\/www.ssec.wisc.edu\/software\/geo2grid\/\"><strong>Geo2Grid<\/strong><\/a>\u00a0<em><strong>(below)<\/strong>\u00a0<\/em>showed the hazy signature of blowing dust\/sand as it was transported off the south coast of Mexico and spread out across the Gulf of Tehuantepec.<\/p>\n<div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/12\/201224_goes16_trueColorGB_Tehuano_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/12\/GOES-16_ABI_RadC_true_color_2020359_220117Z.png\" alt=\"GOES-16 True Color RGB images [click to play animation | MP4]\" width=\"642\" height=\"714\" \/><\/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\/images\/2020\/12\/201224_goes16_trueColorGB_Tehuano_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p style=\"text-align: center;\"><strong>===== 25 December Update =====<\/strong><\/p>\n<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/12\/201225_goes16_visible_Tehuano_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/12\/tehuano_vis-20201225_160021.png\" alt=\"GOES-16 &quot;Red&quot; Visible (0.64 \u00b5m) images [click to play animation | MP4]\" width=\"643\" height=\"300\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible (0.64 \u00b5m) images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/12\/201225_goes16_visible_Tehuano_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>On the following day, GOES-16 Visible images <em><strong>(above)<\/strong><\/em> showed that the leading edge of the gap wind flow &#8212; marked by a broad arc cloud &#8212; was approaching the ITCZ \/ Monsoon Trough in the Pacific Ocean. Ship reports of 30-35 knot winds were seen within the offshore flow &#8212; and <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/12\/tehuano_vis_ascat_44kts-20201225_151021.png\"><strong>ASCAT surface scatterometer winds<\/strong><\/a> revealed speeds as high as 44 knots.<\/p>\n<p>GOES-16 True Color RGB images <em><strong>(below)<\/strong>\u00a0<\/em>showed the hazy signature of blowing dust from Mexico as it spread out across the Pacific Ocean.<\/p>\n<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/12\/201225_goes16_trueColorRGB_Tehuano_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/12\/GOES-16_ABI_RadF_true_color_2020360_180021Z.png\" 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\/images\/2020\/12\/201225_goes16_trueColorRGB_Tehuano_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div><span class=\"css-901oao css-16my406 r-1qd0xha r-ad9z0x r-bcqeeo r-qvutc0\">Aided by enhanced forward scattering during the morning hours, True Color RGB images from <\/span><span class=\"r-18u37iz\">GOES-17 <em>(<\/em><\/span><em><span class=\"r-18u37iz\">GOES-West)<\/span><\/em><span class=\"css-901oao css-16my406 r-1qd0xha r-ad9z0x r-bcqeeo r-qvutc0\"> showed the hazy signature of airborne dust from Mexico a bit better <em><strong>(below)<\/strong><\/em>.<\/span><\/p>\n<div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/12\/201225_goes17_trueColorRGB_Tehuano_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/12\/GOES-17_ABI_RadF_true_color_2020360_150032Z.png\" alt=\"GOES-17 True Color RGB images [click to play animation | MP4]\" width=\"641\" height=\"641\" \/><\/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\/images\/2020\/12\/201225_goes17_trueColorRGB_Tehuano_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>GOES-16 (GOES-East) &#8220;Red&#8221; Visible (0.64 \u00b5m) images (above) indicated that a strong arctic cold front (surface analyses) had plunged southward across Mexico, through the Chivela Pass, and emerged as a Tehuano (or &#8220;Tehuantepecer&#8220;) gap wind into the Gulf of Tehuantepec on 24 December 2020. Along the Gulf of Mexico coast, a few sites in Mexico [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":39409,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[7,74,80,45,25],"tags":[],"class_list":["post-39407","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-air-quality","category-goes-16","category-goes-17","category-redgreenblue-rgb-images","category-satellite-winds"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/39407","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=39407"}],"version-history":[{"count":5,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/39407\/revisions"}],"predecessor-version":[{"id":39413,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/39407\/revisions\/39413"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/39409"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=39407"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=39407"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=39407"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}