{"id":48596,"date":"2022-11-03T18:59:00","date_gmt":"2022-11-03T18:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=48596"},"modified":"2022-11-04T15:05:50","modified_gmt":"2022-11-04T15:05:50","slug":"extratropical-transition-of-hurricane-martin","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/48596","title":{"rendered":"Extratropical transition of Hurricane Martin"},"content":{"rendered":"<p><div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/11\/221103_goes16_waterVapor_airMassRGB_Martin_extratropical_transition_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/11\/mar_rgb-20221103_120020.png\" alt=\"\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Mid-Level Water Vapor (6.9 \u00b5m) and Air Mass RGB images [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/11\/221103_goes16_waterVapor_airMassRGB_Martin_extratropical_transition_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-16 <em>(GOES-East)<\/em> Mid-Level Water Vapor (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band09.pdf\"><strong>6.9 \u00b5m<\/strong><\/a>) and <a href=\"https:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/QuickGuide_GOESR_AirMassRGB_final.pdf\"><strong>Air Mass<\/strong><\/a> RGB images <em><strong>(above)<\/strong><\/em> covered the period 0600-1800 UTC on 03 November 2022 &#8212; during which Category 1 <a href=\"https:\/\/www.nhc.noaa.gov\/archive\/2022\/MARTIN.shtml?\"><strong>Hurricane Martin<\/strong><\/a> transitioned to an extratropical cyclone over the North Atlantic Ocean (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/11\/221103_surface_analyses_Martin_anim.gif\"><strong>surface analyses<\/strong><\/a>). West of Martin, the large area of orange-to-red hues on the Air Mass RGB images highlighted an <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/11\/221103_500hPa_geopotentialHeightAnomaly_Martin_anim.gif\"><strong>anomalously-deep<\/strong><\/a> mid-tropospheric trough that was moving eastward (also shown by UKMET model 500 hPa height contours) &#8212; which began to phase with and absorb the mid-tropospheric circulation of Martin as the extratropical transition completed.<\/p>\n<p>DMSP-17 SSMIS Microwave (85 GHz) imagery at 1005 UTC <em><strong>(below)<\/strong><\/em> &#8212; from the <a href=\"http:\/\/tropic.ssec.wisc.edu\"><strong>CIMSS Tropical Cyclones<\/strong><\/a> site &#8212; indicated that a closed eyewall was not present with Martin at that time.<\/p>\n<p><div style=\"width: 1062px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/11\/221103_1005utc_dmsp17_ssmis_microwave_Martin.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/11\/221103_1005utc_dmsp17_ssmis_microwave_Martin.gif\" width=\"1052\" height=\"601\" \/><\/a><p class=\"wp-caption-text\">DMSP-17 SSMIS Microwave (85 GHz) image at 1005 UTC [click to enlarge]<\/p><\/div>VIIRS True Color RGB and Infrared Window (11.45 \u00b5m) images from Suomi-NPP (at 1447 UTC) and NOAA-20 (at 1537 UTC) viewed using <a href=\"http:\/\/realearth.ssec.wisc.edu\"><strong>RealEarth<\/strong><\/a> <em><strong>(below)<\/strong><\/em> showed Martin around the time that extratropical transition was nearly complete.<\/p>\n<p><div style=\"width: 1930px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/11\/221103_1447utc_suomiNPP_1537utc_noaa20_trueColorRGB_infraredWindow_Martin_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/11\/221103_1447utc_suomiNPP_1537utc_noaa20_trueColorRGB_infraredWindow_Martin_anim.gif\" width=\"1920\" height=\"962\" \/><\/a><p class=\"wp-caption-text\">VIIRS True Color RGB and Infrared Window (11.45 \u00b5m) images from Suomi-NPP (at 1447 UTC) and NOAA-20 (at 1537 UTC) [clic to enlarge]<\/p><\/div>GOES-16 Nighttime Microphysics RGB and daytime True Color RGB images from the <a href=\"https:\/\/geosphere.ssec.wisc.edu\/#playing:true;coordinate:0,0;num_frames:30;\"><strong>CSPP GeoSphere<\/strong><\/a> site <em><strong>(below)<\/strong><\/em> displayed the center of Martin moving rapidly north-northeastward (at speeds of 40-50 knots) during the day.<\/p>\n<p><div style=\"width: 1034px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/11\/goeseast_abi_radf_true_color_night_s20221103100020_e20221103181020_f50.mp4\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/11\/goeseast_abi_radf_true_color_night_20221103140020.png\" width=\"1024\" height=\"461\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Nighttime Microphysics RGB and daytime True Color RGB images [click to play MP4 animation]<\/p><\/div>Additional imagery of Martin can be seen in <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/48599\"><strong>this blog post<\/strong><\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>GOES-16 (GOES-East) Mid-Level Water Vapor (6.9 \u00b5m) and Air Mass RGB images (above) covered the period 0600-1800 UTC on 03 November 2022 &#8212; during which Category 1 Hurricane Martin transitioned to an extratropical cyclone over the North Atlantic Ocean (surface analyses). West of Martin, the large area of orange-to-red hues on the Air Mass RGB [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":48623,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[56,74,79,78,53,45,49,2,48],"tags":[],"class_list":["post-48596","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-dmsp","category-goes-16","category-microwave","category-noaa-20","category-real-earth","category-redgreenblue-rgb-images","category-suomi_npp","category-tropical-cyclones","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/48596","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=48596"}],"version-history":[{"count":7,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/48596\/revisions"}],"predecessor-version":[{"id":48627,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/48596\/revisions\/48627"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/48623"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=48596"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=48596"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=48596"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}