{"id":70526,"date":"2026-05-19T17:59:00","date_gmt":"2026-05-19T17:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=70526"},"modified":"2026-05-22T16:21:09","modified_gmt":"2026-05-22T16:21:09","slug":"leeside-cold-frontal-gravity-wave-as-viewed-by-goes-18-16-19","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/70526","title":{"rendered":"Leeside cold frontal gravity wave as viewed by GOES-18\/16\/19"},"content":{"rendered":"<p><div style=\"width: 2564px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/05\/260519_goes18_goes16_goes19_waterVapor_leesideColdFrontalGravityWave_Plains_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/05\/G18_G16_G19_WATER_VAPOR_CDFNT_NOWINDS_19MAY2026_B999_2026139_090021_0003PANELS_FRAME00145.GIF\" width=\"2554\" height=\"1082\" \/><\/a><p class=\"wp-caption-text\">10-minute GOES-18\/GOES-West (left), 5-minute GOES-16 (center) and 5-minute GOES-19\/GOES-East (right) Mid-level Water Vapor (6.9 \u00b5m) images, with\/without hourly plots of surface wind barbs and gusts (knots), from 2100 UTC on 18 May to 1701 UTC on 19 May [click to play animated GIF]<\/p><\/div>The GOES-16 satellite was temporarily brought out of storage for annual testing (<a href=\"https:\/\/www.ospo.noaa.gov\/data\/messages\/2026\/05\/MSG_20260508_1915.html\"><strong>details<\/strong><\/a>) &#8212; which allowed for a 3-GOES (GOES-18\/GOES-West positioned at 137.0 W longitude, GOES-16 at 104.7 W longitude and GOES-19\/GOES-East at 75.2 W longitude) Water Vapor image comparison of the signature of a leeside cold frontal gravity wave (<a href=\"https:\/\/journals.ametsoc.org\/doi\/full\/10.1175\/1520-0469%281999%29056%3C2986%3ADTGWCB%3E2.0.CO%3B2\"><strong>reference<\/strong><\/a>) that propagated southward across the High Plains during the <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20260518.html\"><strong>18 May<\/strong><\/a> &#8211; <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20260519.html\"><strong>19 May 2026<\/strong><\/a> period <em><strong>(above)<\/strong><\/em>. The images are displayed in the native projection of each satellite.<\/p>\n<p>In the immediate wake of the cold frontal passage there were northerly\/northeasterly wind gusts of 40-42 kts in the Panhandles of Oklahoma and Texas, as well as in northeastern New Mexico &#8212; and the highest peak wind gust at post-frontal METAR sites was 44 kts at Tucumcari, New Mexico (KTCC), which occurred at 0537 UTC <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><div style=\"width: 3002px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/05\/260519_0601utc_)goes19_watewrVapor_ktccMETAR.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/05\/260519_0601utc_)goes19_watewrVapor_ktccMETAR.png\" width=\"2992\" height=\"1672\" \/><\/a><p class=\"wp-caption-text\">GOES-19 Mid-level Water Vapor (6.9 \u00b5m) image at 0601 UTC on 19 May, with a cursor sample of the METAR report at Tucumcari, New Mexico [click to enlarge]<\/p><\/div><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/05\/260518_KDDC_SFCMG.GIF\"><strong>Surface observations<\/strong><\/a> showed that the cold front moved through Dodge City in southwest Kansas just before 2100 UTC on 18 May &#8212; and data from the Dodge City rawinsonde launch a few hours later at 0000 UTC on 19 May <em><strong>(below)<\/strong><\/em> depicted the shallow post-frontal cold air that extended from the surface to the 850 hPa pressure level, as well as dry air throughout much of the middle\/upper troposphere.<\/p>\n<p><div style=\"width: 3002px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/05\/260519_0000utc_kddc_raob.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/05\/260519_0000utc_kddc_raob.png\" width=\"2992\" height=\"1672\" \/><\/a><p class=\"wp-caption-text\">Plot of rawinsonde data from Dodge City, Kansas at 0000 UTC on 19 May [click to enlarge]<\/p><\/div>A plot of the GOES-19 Band 9 <a href=\"https:\/\/cimss.ssec.wisc.edu\/goes-wf\/\"><strong>weighting function<\/strong><\/a> &#8212; calculated using rawinsonde data from Dodge City at 0000 UTC on 19 May <em><strong>(below)<\/strong><\/em> showed that the peak of upwelling 6.9 \u00b5m radiation occurred at the 500 hPa pressure level, with no contribution from the surface. This helped to underscore the vertically-propagating nature of the leeside cold frontal gravity wave, which allowed its unambiguous mid-tropospheric signature to be evident in 6.9 \u00b5m Band 9 water vapor imagery.<\/p>\n<div style=\"width: 3258px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/05\/260519_0000utc_kddc_band09_weightingFunction.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2026\/05\/260519_0000utc_kddc_band09_weightingFunction.png\" width=\"3248\" height=\"2122\" \/><\/a><p class=\"wp-caption-text\">Plot of the GOES-19 Band 9 (6.9 \u00b5m) weighting function, calculated using Dodge City, Kansas rawinsonde data at 0000 UTC on 19 May [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>The GOES-16 satellite was temporarily brought out of storage for annual testing (details) &#8212; which allowed for a 3-GOES (GOES-18\/GOES-West positioned at 137.0 W longitude, GOES-16 at 104.7 W longitude and GOES-19\/GOES-East at 75.2 W longitude) Water Vapor image comparison of the signature of a leeside cold frontal gravity wave (reference) that propagated southward across [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":70527,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[74,114,159],"tags":[],"class_list":["post-70526","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-16","category-goes-18","category-goes-19"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/70526","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=70526"}],"version-history":[{"count":19,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/70526\/revisions"}],"predecessor-version":[{"id":70592,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/70526\/revisions\/70592"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/70527"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=70526"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=70526"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=70526"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}