{"id":34156,"date":"2019-08-22T23:59:21","date_gmt":"2019-08-22T23:59:21","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=34156"},"modified":"2019-08-25T16:49:16","modified_gmt":"2019-08-25T16:49:16","slug":"viirs-imagery-and-nucaps-profiles-near-the-north-pole","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/34156","title":{"rendered":"VIIRS imagery and NUCAPS profiles near the North Pole"},"content":{"rendered":"<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190822_suomiNPP_viirs_visible_shortwaveInfrared_infraredWindow_North_Pole_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190822_suomiNPP_viirs_visible_shortwaveInfrared_infraredWindow_North_Pole_anim.gif\" alt=\"Suomi NPP VIIRS Visible (0.64 \u00b5m), Shortwave Infrared (3.74 \u00b5m) and Infrared Window (11.45 \u00b5m) images [click to enlarge]\" width=\"643\" height=\"300\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS Visible<em> (0.64 \u00b5m),<\/em> Shortwave Infrared <em>(3.74 \u00b5m)<\/em> and Infrared Window <em>(11.45 \u00b5m)<\/em> images [click to enlarge]<\/p><\/div>A sequence of 4 consecutive Suomi NPP <a href=\"https:\/\/www.jpss.noaa.gov\/viirs.html\"><strong>VIIRS<\/strong><\/a> Visible (0.64 \u00b5m), Shortwave Infrared (3.74 \u00b5m) and Infrared Window (11.4 \u00b5m) images <em><strong>(above)<\/strong><\/em> showed a small swirl of clouds associated with a weak area of low pressure near the North Pole &#8212; north of Greenland (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190822_surface_analyses_anim.gif\"><strong>surface analyses<\/strong><\/a>) &#8212; on 22 August 2019.<\/p>\n<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190822_suomiNPP_viirs_visible_noaa20_nucaps_North_Pole_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190822_suomiNPP_viirs_visible_noaa20_nucaps_North_Pole_anim.gif\" alt=\"Suomi NPP VIIRS Visible (0.64 \u00b5m) images, with plots of NUCAPS availability [click to enlarge]\" width=\"643\" height=\"300\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS Visible <em>(0.64 \u00b5m)<\/em> images, with plots of NUCAPS availability [click to enlarge]<\/p><\/div>There were Suomi NPP <a href=\"https:\/\/www.ospo.noaa.gov\/Products\/atmosphere\/soundings\/nucaps\/\"><strong>NUCAPS<\/strong><\/a> soundings\u00a0available in the vicinity of the surface low <em><strong>(above)<\/strong><\/em> &#8212; profiles from the 4 squared green dot locations (green dots indicate successful sounding retrievals from both the <a href=\"https:\/\/www.jpss.noaa.gov\/cris.html\"><strong>CrIS<\/strong><\/a> and <a href=\"https:\/\/www.jpss.noaa.gov\/atms.html\"><strong>ATMS<\/strong><\/a> instruments) which were closest to both the surface low and the North Pole <em><strong>(below)<\/strong><\/em> revealed characteristically-low arctic tropopause heights of around 7-8 km, and surface temperatures dropping to below freezing at the 2 most northerly points of 88.28\u00ba and 88.57\u00ba N latitude. <em><strong>Note:<\/strong> the Suomi NPP (SNPP) CrIS anomaly that began on <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/07\/CrIS_1.png\"><strong>24 March 2019<\/strong><\/a> was resolved via a switch to the redundant Side-2 electronics on <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/07\/CrIS_2.png\"><strong>24 June<\/strong><\/a> &#8212; so CrIS data once again became available for incorporation into SNPP NUCAPS soundings beginning on <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/07\/CrIS_3.png\"><strong>01 August<\/strong><\/a>.<\/em> Training material for NUCAPS in AWIPS is available <a href=\"http:\/\/rammb.cira.colostate.edu\/training\/visit\/training_sessions\/nucaps_soundings_in_awips\/\"><strong>here<\/strong><\/a>.<\/p>\n<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190822_nucaps_profiles_North_Pole_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190822_nucaps_profiles_North_Pole_anim.gif\" alt=\"NUCAPS temperature (red) and dew point (green) profiles [click to enlarge]\" width=\"643\" height=\"284\" \/><\/a><p class=\"wp-caption-text\">NUCAPS temperature <em>(red)<\/em> and dew point <em>(green)<\/em> profiles [click to enlarge]<\/p><\/div>According to GCOM-W1 AMSR2 data (<a href=\"https:\/\/stratus.ssec.wisc.edu\/cgi-bin\/amsr2snow_prod?seaice\"><strong>source<\/strong><\/a>), this weak surface low was over a portion of the Arctic Ocean where sea ice concentration was still high <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190822_seaice_NH.png\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2019\/08\/190822_seaice_NH.png\" alt=\"GCOM-W1 AMSR2 sea ice concentration [click to enlarge]\" width=\"642\" height=\"481\" \/><\/a><p class=\"wp-caption-text\">GCOM-W1 AMSR2 sea ice concentration [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>A sequence of 4 consecutive Suomi NPP VIIRS Visible (0.64 \u00b5m), Shortwave Infrared (3.74 \u00b5m) and Infrared Window (11.4 \u00b5m) images (above) showed a small swirl of clouds associated with a weak area of low pressure near the North Pole &#8212; north of Greenland (surface analyses) &#8212; on 22 August 2019. There were Suomi NPP [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":34159,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[37,81,83,49,48],"tags":[],"class_list":["post-34156","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-arctic","category-gcom-w1","category-nucaps","category-suomi_npp","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/34156","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=34156"}],"version-history":[{"count":13,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/34156\/revisions"}],"predecessor-version":[{"id":34170,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/34156\/revisions\/34170"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/34159"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=34156"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=34156"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=34156"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}