{"id":31275,"date":"2019-01-06T21:50:10","date_gmt":"2019-01-06T21:50:10","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=31275"},"modified":"2019-01-08T03:09:27","modified_gmt":"2019-01-08T03:09:27","slug":"first-50of-of-the-season-in-alaska","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/31275","title":{"rendered":"First -50\u00baF of the season in Alaska"},"content":{"rendered":"<div style=\"width: 655px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190106_suomiNPP_viirs_infrared_Chicken_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190106_suomiNPP_viirs_infrared_Chicken_AK_anim.gif\" alt=\"Suomi NPP VIIRS Infrared Window (11.45 \u00b5m) images [click to enlarge]\" width=\"645\" height=\"372\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS Infrared Window <em>(11.45 \u00b5m)<\/em> images [click to enlarge]<\/p><\/div>\n<p style=\"text-align: center;\"><em>* GOES-17 images shown here are preliminary and non-operational *<\/em><\/p>\n<p>The first official temperature of -50\u00baF or colder during Alaska&#8217;s 2018\/2019 winter season was reported by the cooperative observer at Chicken on 06 January &#8212; the 24-hour high temperature at that site was -45\u00baF, with a low of -51\u00baF (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190106_pafg_rtp.text\"><strong>NWS Fairbanks summary<\/strong><\/a>). A sequence of Suomi NPP VIIRS Infrared Window (11.45 \u00b5m) images<em><strong> (above)<\/strong><\/em> showed infrared brightness temperatures as cold as -46.5\u00aaC or -51.7\u00baF <em>(lighter green enhancement)<\/em> in the river valleys between Tok and Eagle (Chicken is located about midway between those 2 cities).<\/p>\n<p>A toggle between Infrared Window images from Suomi NPP VIIRS and GOES-17 <em><strong>(below)<\/strong><\/em> highlighted the advantage of polar-orbiting imagery at high latitudes &#8212; improved spatial resolution and a better viewing angle provides more detailed images. However, it should be noted that the Full Disk GOES-17 imagery that is displayed here using AWIPS is degraded from 2-km to 4-km resolution (at satellite sub-point).<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190106_1130utc_suomiNPP_viirs_goes17_infrared_Chicken_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190106_1130utc_suomiNPP_viirs_goes17_infrared_Chicken_AK_anim.gif\" alt=\"Infrared Window images from Suomi NPP VIIRS (11.45 \u00b5m) and GOES-17 (10.3 \u00b5m) [click to enlarge]\" width=\"640\" height=\"369\" \/><\/a><p class=\"wp-caption-text\">Infrared Window images from Suomi NPP VIIRS <em>(11.45 \u00b5m)<\/em> and GOES-17 <em>(10.3 \u00b5m)<\/em> [click to enlarge]<\/p><\/div>A sequence of NOAA-20 VIIRS Infrared images displayed using <a href=\"https:\/\/re.ssec.wisc.edu\/s\/iZWF8\"><strong>RealEarth<\/strong><\/a> is shown below. The majority of the scene was cloud-free &#8212; except for some cyan-enhanced stratiform clouds moving eastward across parts of the Alaska Range &#8212; and although there was some slight diurnal warming seen in the higher terrain, little change was apparent with the signature of colder air <em>(shades of green)<\/em> that was trapped in the lower elevations and river valleys.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190106_noaa20_viirs_infrared_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190106_noaa20_viirs_infrared_AK_anim.gif\" alt=\"NOAA-20 VIIRS Infrared Window (11.45 \u00b5m) images [click to enlarge]\" width=\"641\" height=\"383\" \/><\/a><p class=\"wp-caption-text\">NOAA-20 VIIRS Infrared Window <em>(11.45 \u00b5m)<\/em> images [click to enlarge]<\/p><\/div>Plots of Fairbanks rawinsonde data from 00 UTC on 06 and 07 January <em><strong>(below)<\/strong><\/em> displayed the strong low-level temperature inversion caused by the relatively shallow arctic air.<\/p>\n<div style=\"width: 649px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190106_190107_00utc_pafa_raobs_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190106_190107_00utc_pafa_raobs_anim.gif\" alt=\"Plots of Fairbanks rawinsonde data from 00 UTC on 06 and 07 January [click to enlarge]\" width=\"639\" height=\"425\" \/><\/a><p class=\"wp-caption-text\">Plots of Fairbanks rawinsonde data from 00 UTC on 06 and 07 January [click to enlarge]<\/p><\/div>\n<p style=\"text-align: center;\"><strong>===== 07 January Update =====<\/strong><\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190107_1926utc_goes17_suomiNPP_viirs_infrared_1_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190107_1926utc_goes17_suomiNPP_viirs_infrared_1_AK_anim.gif\" alt=\"Infrared Window images from GOES-17 ABI (10.33 \u00b5m) and Suomi NPP VIIRS (11.45 \u00b5m) [click to enlarge]\" width=\"640\" height=\"369\" \/><\/a><p class=\"wp-caption-text\">Infrared Window images from GOES-17 ABI <em>(10.33 \u00b5m)<\/em> and Suomi NPP VIIRS <em>(11.45 \u00b5m)<\/em> [click to enlarge]<\/p><\/div>Minimum temperatures of -50\u00baF and colder were again reported on 07 January, with lows of -56\u00baF at Chicken and -50\u00baF at North Pole (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/01\/190107_pafg_rtp.text\"><strong>NWS Fairbanks summary<\/strong><\/a>). 1-minute imagery from a GOES-17 <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/23225\"><strong>Mesoscale Domain Sector<\/strong><\/a> allowed for a more direct full-resolution comparison with Suomi NPP VIIRS imagery &#8212; and a toggle between 1926 UTC images <em><strong>(above)<\/strong><\/em> revealed significantly greater detail in terms of the cold air confined to river valleys on the VIIRS image. The enhancements used in this comparison have identical temperature ranges for each of the color segments (there are some color vs. temperature offsets with the GOES\/VIIRS infrared comparison shown on the previous day). The coldest infrared brightness temperature values on the VIIRS image were -46.4\u00baC in the vicinity of Tok, Alaska and -49.4\u00baC across the Canadian border in Yukon &#8212; compared to -44.6\u00baC and -45.1\u00baC for those two locations on the GOES-17 image.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>* GOES-17 images shown here are preliminary and non-operational * The first official temperature of -50\u00baF or colder during Alaska&#8217;s 2018\/2019 winter season was reported by the cooperative observer at Chicken on 06 January &#8212; the 24-hour high temperature at that site was -45\u00baF, with a low of -51\u00baF (NWS Fairbanks summary). A sequence of [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":31277,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[80,78,53,49,48,5],"tags":[],"class_list":["post-31275","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-17","category-noaa-20","category-real-earth","category-suomi_npp","category-viirs","category-winter-weather"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/31275","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=31275"}],"version-history":[{"count":11,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/31275\/revisions"}],"predecessor-version":[{"id":31287,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/31275\/revisions\/31287"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/31277"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=31275"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=31275"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=31275"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}