{"id":47243,"date":"2022-07-19T23:59:00","date_gmt":"2022-07-19T23:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=47243"},"modified":"2022-12-09T16:42:20","modified_gmt":"2022-12-09T16:42:20","slug":"anomalously-deep-upper-low-brings-snow-to-northwestern-alaska","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/47243","title":{"rendered":"Anomalously-deep upper low brings light snow to northwestern Alaska"},"content":{"rendered":"<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/07\/220718_220719_goes18_waterVapor_surfaceWeatherType_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/07\/G18_WV_WXS_AK_SNOW_18_19JUL2022_B9_2022200_120020_GOES-18_0001PANEL_FRAME00217.GIF\" width=\"640\" height=\"440\"><\/a><p class=\"wp-caption-text\">GOES-18 Mid-level (6.9 \u00b5m) Water Vapor images, with plots of hourly surface weather type [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/07\/220718_220719_goes18_waterVapor_surfaceWeatherType_AK_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p style=\"text-align: center\"><strong>GOES-18 images shown in this blog post are preliminary and non-operational<\/strong><\/p>\n<p>GOES-18 Mid-level Water Vapor (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band09.pdf\"><strong>6.9 \u00b5m<\/strong><\/a>) images during the 18 July &#8211; 19 July 2022 period <em><strong>(above)<\/strong><\/em> showed a series of impulses rotating within the broader circulation of an <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/07\/220718_220719_500hpa_height_anomaly_anim.gif\">anomalously-deep<\/a><\/strong> low pressure system that meandered over the <a href=\"https:\/\/en.wikipedia.org\/wiki\/Bering_Strait\"><strong>Bering Strait<\/strong><\/a> region. <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/07\/220718_220719_850hpa_temperature_anomaly_anim.gif\"><strong>Anomalously-cold<\/strong><\/a> air associated with this deep low helped to produce brief periods of unusual July snow at some locations across the Seward Peninsula and northwestern Alaska.<\/p>\n<p>In GOES-18 <a href=\"https:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/QuickGuide_GOESR_AirMassRGB_final.pdf\"><strong>Air Mass RGB<\/strong><\/a> images created using <a href=\"https:\/\/www.ssec.wisc.edu\/software\/geo2grid\/\"><strong>Geo2Grid<\/strong><\/a> <em><strong>(below)<\/strong><\/em>, brighter shades of red highlighted the core of this broad low pressure system, where high-altitude ozone levels were elevated (due to an unusually low tropopause).<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/07\/220718_220719_goes18_airMassRGB_AK_low_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/07\/GOES-18_ABI_RadF_airmass_2022200_120020Z.png\" width=\"640\" height=\"640\"><\/a><p class=\"wp-caption-text\">GOES-18 Air Mass RGB images [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/07\/220718_220719_goes18_airMassRGB_AK_low_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div><br \/>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/07\/220719_PAOM_RAOBS.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/07\/220719_PAOM_RAOBS.GIF\" width=\"640\" height=\"480\"><\/a><p class=\"wp-caption-text\">Plots of rawinsonde data at Nome, Alaska at 00 UTC and 12 UTC on 19 July 2022 [click to enlarge]<\/p><\/div>In fact, at 12 UTC on 19 July the low 500 hPa geopotential height value of 5269.3 meters from the Nome, Alaska rawinsonde report <em><strong>(above)<\/strong><\/em> established a new July record for that site. The 12 UTC sounding also suggested that the tropopause was located at an unusually low pressure level of 483 hPa &#8212; such a low tropopause height was supported by NOAA-20 Gridded NUCAPS data from the <a href=\"https:\/\/weather.msfc.nasa.gov\/cgi-bin\/sportPublishData.pl?dataset=griddednucaps\"><strong>SPoRT site<\/strong><\/a> <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/07\/220719_1236utc_noaa20_nucaps_AK_tropopause_height.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2022\/07\/220719_1236utc_noaa20_nucaps_AK_tropopause_height.png\" width=\"640\" height=\"360\"><\/a><p class=\"wp-caption-text\">NOAA-20 Gridded NUCAPS Tropopause Height at 1236 UTC on 19 July [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>GOES-18 images shown in this blog post are preliminary and non-operational GOES-18 Mid-level Water Vapor (6.9 \u00b5m) images during the 18 July &#8211; 19 July 2022 period (above) showed a series of impulses rotating within the broader circulation of an anomalously-deep low pressure system that meandered over the Bering Strait region. Anomalously-cold air associated with [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":47293,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[37,132,114,78,83,45,5],"tags":[],"class_list":["post-47243","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-arctic","category-geo2grid","category-goes-18","category-noaa-20","category-nucaps","category-redgreenblue-rgb-images","category-winter-weather"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/47243","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=47243"}],"version-history":[{"count":14,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/47243\/revisions"}],"predecessor-version":[{"id":49090,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/47243\/revisions\/49090"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/47293"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=47243"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=47243"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=47243"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}