{"id":37655,"date":"2020-07-16T18:59:24","date_gmt":"2020-07-16T18:59:24","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=37655"},"modified":"2020-07-17T19:26:28","modified_gmt":"2020-07-17T19:26:28","slug":"turbulence-associated-with-transverse-banding-2","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/37655","title":{"rendered":"Turbulence associated with transverse banding"},"content":{"rendered":"<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/07\/200716_goes16_infrared_cirrus_pireps_airmets_Midwest_transverse_banding_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/07\/tb_ci-20200716_130122.png\" alt=\"GOES-16 \" width=\"643\" height=\"300\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Clean&#8221; Infrared Window<em> (10.35 \u00b5m)<\/em> and Near-Infrared \u201cCirrus\u201d<em> (1.38 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/07\/200716_goes16_infrared_cirrus_pireps_airmets_Midwest_transverse_banding_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>As a Mesoscale Convective System (MCS) over Kansas and Oklahoma decayed during the morning hours of <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20200716.html\"><strong>16 July 2020<\/strong><\/a>, GOES-16<em> (GOES-East)<\/em> &#8220;Clean&#8221; Infrared Window (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band13.pdf\"><strong>10.35 \u00b5m<\/strong><\/a>) and Near-Infrared \u201cCirrus\u201d (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band04.pdf\"><strong>1.38 \u00b5m<\/strong><\/a>) images <em><strong>(above)<\/strong><\/em> depicted widespread <a href=\"https:\/\/rmets.onlinelibrary.wiley.com\/doi\/abs\/10.1002\/wea.417\"><strong>transverse banding<\/strong><\/a> &#8212; tendrils of cirrus clouds oriented perpendicular to the <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/07\/200716_goes16_cirrus_200hPaWindStreamlines_pireps_airmets_Midwest_transverse_banding_anim.gif\"><strong>upper-tropospheric wind flow<\/strong><\/a> &#8212; along the northern periphery of the MCS. An <a href=\"https:\/\/www.weather.gov\/source\/zhu\/ZHU_Training_Page\/Weather_Keys\/AIRMETs\/AIRMET.htm\"><strong>AIRMET<\/strong><\/a> was issued for that region (advising of moderate turbulence between <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/07\/200716_goes16_cirrus_airmet.png\"><strong>30,000 and 43,000 feet<\/strong><\/a>), and there were numerous Pilot Reports (PIREPs) of light to moderate turbulence in the general vicinity of these transverse banding features.<\/p>\n<p>A GOES-16 <a href=\"https:\/\/cimss.ssec.wisc.edu\/training\/YouTube_TurbulenceTraining.html\"><strong>Turbulence Probability product<\/strong><\/a><em><strong> (below)<\/strong><\/em> did show scattered pockets of 25-35% probability in the transverse banding region. However, this product is designed to diagnose turbulence potential in the vicinity of features such as fronts and fields of convection.<\/p>\n<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/07\/200716_goes16_turbulenceProbability_pireps_airmets_Midwest_transverse_banding_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/07\/200716_1230utc_goes16_turbulenceProbability_pireps_airmets.png\" alt=\"GOES-16 Turbulence Probability product, with plots of PIREPs and AIRMETs [click to play animation | MP4]\" width=\"643\" height=\"300\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Turbulence Probability product, with plots of PIREPs and AIRMETs [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/07\/200716_goes16_turbulenceProbability_pireps_airmets_Midwest_transverse_banding_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Such transverse banding cloud features are frequently observed around the periphery of decaying MCSs (for example, <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/28527\"><strong>June 2018<\/strong><\/a> and <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/21632\"><strong>July 2016<\/strong><\/a>) and in the vicinity of strong upper-tropospheric jet streaks (for example, <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/35566\"><strong>February 2020<\/strong><\/a> and <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/20932\"><strong>March 2016<\/strong><\/a>).<\/p>\n","protected":false},"excerpt":{"rendered":"<p>As a Mesoscale Convective System (MCS) over Kansas and Oklahoma decayed during the morning hours of 16 July 2020, GOES-16 (GOES-East) &#8220;Clean&#8221; Infrared Window (10.35 \u00b5m) and Near-Infrared \u201cCirrus\u201d (1.38 \u00b5m) images (above) depicted widespread transverse banding &#8212; tendrils of cirrus clouds oriented perpendicular to the upper-tropospheric wind flow &#8212; along the northern periphery of [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":37657,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[21,74],"tags":[],"class_list":["post-37655","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-aviation","category-goes-16"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/37655","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=37655"}],"version-history":[{"count":5,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/37655\/revisions"}],"predecessor-version":[{"id":37663,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/37655\/revisions\/37663"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/37657"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=37655"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=37655"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=37655"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}