{"id":37227,"date":"2020-06-12T23:59:52","date_gmt":"2020-06-12T23:59:52","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=37227"},"modified":"2020-06-14T22:46:31","modified_gmt":"2020-06-14T22:46:31","slug":"cutoff-low-over-northern-alaska","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/37227","title":{"rendered":"Cutoff low over northern Alaska"},"content":{"rendered":"<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/06\/200612_goes17_waterVapor_pv1.5pressure_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/06\/ak_wv-20200612_210032.png\" alt=\"GOES-17 Mid-level Water Vapor (6.9 \u00b5m) images, with contours of PV1.5 Pressure plotted in red [click to play animation | MP4]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Mid-level Water Vapor<em> (6.9 \u00b5m)<\/em> images, with contours of PV1.5 Pressure plotted in red [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/06\/200612_goes17_waterVapor_pv1.5pressure_AK_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-17<em> (GOES-West)<\/em> Mid-level Water Vapor (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band09.pdf\"><strong>6.9 \u00b5m<\/strong><\/a>) images<em><strong> (above)<\/strong> <\/em>showed the circulation of an anomalous middle-tropospheric <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/06\/200612_500hPa_anaomaly_anim.gif\">cutoff low<\/a><\/strong> over the northwestern portion of Alaska on 12 June 2020. A Potential Vorticity (PV) anomaly associated with this low was causing the dynamic tropopause &#8212; represented by the pressure of the PV1.5 surface &#8212; to descend as low as the 500 hPa pressure level.<\/p>\n<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/06\/ak_wv_nucaps-20200612_215031.png\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/06\/ak_wv_nucaps-20200612_215031.png\" alt=\"GOES-17 Mid-level Water Vapor (6.9 \u00b5m) images, with contours of PV1.5 Pressure plotted in red and available NUCAPS sounding profiles denoted by green\/yellow points [click to enlarge]\" width=\"643\" height=\"300\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Mid-level Water Vapor<em> (6.9 \u00b5m)<\/em> images, with contours of PV1.5 Pressure plotted in red and available NUCAPS sounding profiles denoted by green\/yellow points [click to enlarge]<\/p><\/div>Just after 21 UTC, an overpass of the Suomi NPP satellite provided NUCAPS soundings <em><strong>(above)<\/strong><\/em> within much of the core of the cutoff low &#8212; the green NUCAPS sounding profile about 40 miles east\/southeast of the 500 hPa PV1.5 pressure contour <em><strong>(below)<\/strong><\/em> displayed an apparent tropopause near the 400 hPa pressure level.<\/p>\n<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/06\/200612_22utc_nucaps_profile_AK.png\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/06\/200612_22utc_nucaps_profile_AK.png\" alt=\"NUCAPS sounding profile [click to enlarge]\" width=\"642\" height=\"302\" \/><\/a><p class=\"wp-caption-text\">NUCAPS sounding profile [click to enlarge]<\/p><\/div>GOES-17 &#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> (below)<\/strong><\/em> revealed the development of numerous showers and thunderstorms across the Brooks Range and North Slope of Alaska, aided by instability beneath the cutoff low.<\/p>\n<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/06\/200612_goes17_visible_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/06\/ak_vis-20200612_210032.png\" alt=\"GOES-17 &quot;Red&quot; Visible (0.64 \u00b5m) images, with hourly surface reports plotted in red [click to play animation | MP4]\" width=\"643\" height=\"300\" \/><\/a><p class=\"wp-caption-text\">GOES-17 &#8220;Red&#8221; Visible <em>(0.64 \u00b5m)<\/em> images, with hourly surface reports plotted in red [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/06\/200612_goes17_visible_AK_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>A higher spatial resolution view of these showers and thunderstorms was provided by a sequence of VIIRS True Color Red-Green-Blue (RGB) and Infrared Window (11.45 \u00b5m) images from NOAA-20 and Suomi NPP, as viewed using <a href=\"http:\/\/realearth.ssec.wisc.edu\"><strong>RealEarth<\/strong><\/a> <em><strong>(below)<\/strong><\/em>. A few of these thunderstorms moved toward the Arctic Coast, with one fairly impressive storm <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/06\/200612_23z_ir.png\"><strong>just southwest of Katovik<\/strong><\/a> which exhibited cloud-top infrared brightness temperatures near -60\u00baC <em>(red enhancement)<\/em>\u00a0around 23 UTC.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/06\/200612_noaa20_suomiNPP_trueColorRGB_infraredWindow_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/06\/200612_noaa20_suomiNPP_trueColorRGB_infraredWindow_AK_anim.gif\" alt=\"VIIRS True Color (RGB) and Infrared Window (11.45 \u00b5m) images from NOAA-20 and Suomi NPP [click to enlarge]\" width=\"641\" height=\"335\" \/><\/a><p class=\"wp-caption-text\">VIIRS True Color (RGB) and Infrared Window<em> (11.45 \u00b5m)<\/em> images from NOAA-20 and Suomi NPP [click to enlarge]<\/p><\/div><center><\/p>\n<blockquote class=\"twitter-tweet\">\n<p dir=\"ltr\" lang=\"en\">Summer thunderstorms stretched across the North Slope and near the Arctic Coast today. Data from the GLD360 depicted over 800 Cloud-to-Ground lightning events in the area! Here is the scene at Atqasuk, Utqiagvik, Nuiqsut, and Deadhorse this afternoon and evening. <a href=\"https:\/\/twitter.com\/hashtag\/akwx?src=hash&amp;ref_src=twsrc%5Etfw\">#akwx<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/lightning?src=hash&amp;ref_src=twsrc%5Etfw\">#lightning<\/a> <a href=\"https:\/\/t.co\/tGeqswONW5\">pic.twitter.com\/tGeqswONW5<\/a><\/p>\n<p>\u2014 NWS Fairbanks (@NWSFairbanks) <a href=\"https:\/\/twitter.com\/NWSFairbanks\/status\/1271704447031185408?ref_src=twsrc%5Etfw\">June 13, 2020<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><br \/>\n<\/center><\/p>\n","protected":false},"excerpt":{"rendered":"<p>GOES-17 (GOES-West) Mid-level Water Vapor (6.9 \u00b5m) images (above) showed the circulation of an anomalous middle-tropospheric cutoff low over the northwestern portion of Alaska on 12 June 2020. A Potential Vorticity (PV) anomaly associated with this low was causing the dynamic tropopause &#8212; represented by the pressure of the PV1.5 surface &#8212; to descend as [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":37232,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[37,80,78,83,53,45,49,48],"tags":[],"class_list":["post-37227","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-arctic","category-goes-17","category-noaa-20","category-nucaps","category-real-earth","category-redgreenblue-rgb-images","category-suomi_npp","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/37227","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=37227"}],"version-history":[{"count":4,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/37227\/revisions"}],"predecessor-version":[{"id":37233,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/37227\/revisions\/37233"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/37232"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=37227"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=37227"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=37227"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}