{"id":29654,"date":"2018-09-02T20:41:54","date_gmt":"2018-09-02T20:41:54","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=29654"},"modified":"2018-09-03T18:57:59","modified_gmt":"2018-09-03T18:57:59","slug":"snow-cover-in-the-brooks-range-and-north-slope-in-alaska","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/29654","title":{"rendered":"Snow cover in the Brooks Range and North Slope of Alaska"},"content":{"rendered":"<p><div style=\"width: 649px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180901_180902_suomi_npp_viirs_InfraredWindow_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180901_180902_suomi_npp_viirs_InfraredWindow_AK_anim.gif\" alt=\"Suomi NPP VIIRS Infrared Window (11.45 \u00b5m) images on 01 and 02 September [click to enlarge]\" width=\"639\" height=\"366\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS Infrared Window <em>(11.45 \u00b5m)<\/em> images on 01 and 02 September [click to enlarge]<\/p><\/div>A low moved eastward across the Beaufort Sea on 01 September 2018, bringing a cold front southward across the North Slope and Brooks Range in far northern Alaska (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180901_180902_surface_analyses_AK_anim.gif\"><strong>surface analyses<\/strong><\/a>). A sequence of Suomi NPP VIIRS Infrared Window (11.45 \u00b5m) images<em><strong> (above)<\/strong><\/em> showed the clearing of high\/cold clouds in the wake of the frontal passage.<\/p>\n<p>The upslope flow of cold air helped to generate accumulating snowfall across that region &#8212; prompting a Winter Storm Warning to be issued for the eastern Brooks Range, where 4-8 inches was expected at higher elevations &#8212; and some of the resulting snow cover was seen on a Suomi NPP VIIRS <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/ak_dnb-20180902_141532.png\"><strong>Day\/Night Band<\/strong><\/a> (0.7 \u00b5m) image at 1415 UTC or 6:15 am local time on 02 September <em><strong>(below)<\/strong><\/em>. A comparison with the corresponding VIIRS <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/ak_ir-20180902_141532.png\"><strong>Infrared Window<\/strong><\/a> (11.45 \u00b5m) image and <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/ak_topo-20180902_140000.png\"><strong>Topography<\/strong><\/a> is also shown. The darker shades of brown on the topography image correspond to elevations of 6000-8000 feet in the Brooks Range.<\/p>\n<p><div style=\"width: 649px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180902_1415utc_suomi_npp_viirs_DayNightBand_InfraredWindow_topography_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180902_1415utc_suomi_npp_viirs_DayNightBand_InfraredWindow_topography_AK_anim.gif\" alt=\"Suomi NPP VIIRS Day\/Night Band (0.7 \u00b5m), Infrared Window (11.45 \u00b5m) and Topography images [click to enlarge]\" width=\"639\" height=\"366\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS Day\/Night Band<em> (0.7 \u00b5m),<\/em> Infrared Window <em>(11.45 \u00b5m)<\/em> and Topography images [click to enlarge]<\/p><\/div>Later in the day on 02 September, additional clearing of patchy low clouds revealed more of the snow cover, as seen in a toggle between VIIRS <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/ak_vis-20180902_190824.png\"><strong>Visible<\/strong><\/a> (0.64 \u00b5m), <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/ak_swir-20180902_190000.png\"><strong>Shortwave Infrared<\/strong><\/a> (3.74 \u00b5m) and Topography images <em><strong>(below)<\/strong><\/em>. Supercooled water cloud droplets are efficient reflectors of incoming solar radiation, making patches of low cloud appear <em>darker shades of gray<\/em> on the Shortwave Infrared image (helping to identify low clouds over snow cover).<\/p>\n<p><div style=\"width: 649px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180902_1924utc_suomi_npp_viirs_visible_shortwaveInfrared_topography_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180902_1924utc_suomi_npp_viirs_visible_shortwaveInfrared_topography_AK_anim.gif\" alt=\"Suomi NPP VIIRS Visible (0.64 \u00b5m), Shortwave Infrared (3.74 \u00b5m) and Topography images [click to enlarge]\" width=\"639\" height=\"366\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS Visible <em>(0.64 \u00b5m),<\/em> Shortwave Infrared <em>(3.74 \u00b5m)<\/em> and Topography images [click to enlarge]<\/p><\/div>At 2124 UTC (or 1:24 pm local time), a 30-meter resolution Landsat-8 False Color Red-Green-Blue (RGB) image viewed using <a href=\"https:\/\/re.ssec.wisc.edu\/s\/5Tbzz\"><strong>RealEarth<\/strong><\/a><em><strong> (below)<\/strong><\/em> provided a more detailed view of a portion of the snow cover. Snow and ice appear as shades of cyan in this type of RGB image &#8212; which is created by combining Landsat bands 6 (1.61 \u00b5m), 5 (0.865 \u00b5m), and 4 (0.655 \u00b5m) as Red, Green, and Blue &#8212; and numerous small ice floes can also be seen off the coast.<\/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\/2018\/09\/180902_2124utc_landsat8_falsecolor_AK.jpeg\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180902_2124utc_landsat8_falsecolor_AK.jpeg\" alt=\"Landsat-8 False Color RGB image [click to enlarge]\" width=\"641\" height=\"365\" \/><\/a><p class=\"wp-caption-text\">Landsat-8 False Color RGB image [click to enlarge]<\/p><\/div>On a side note, farther to the west an interesting pattern of contrails was seen in VIIRS <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/ak_vis_zoom-20180902_204757.png\"><strong>Visible<\/strong><\/a> and <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/ak_ir_zoom-20180902_204757.png\"><strong>Infrared Window<\/strong><\/a> images at 2046 UTC <em><strong>(below)<\/strong><\/em>. On the Visible image, note that the darker contrail shadows cast onto the surface are displaced about 15 miles to the north (due to the low sun angle); the contrail features exhibited Infrared brightness temperatures of -10 to -15\u00baC. These contrail patterns were generated by military aircraft performing training exercises: similar features have been noted over <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/27856\">California<\/a><\/strong> and <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/26165\">North Dakota<\/a><\/strong>. <\/p>\n<p><div style=\"width: 649px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180902_suomiNPP_viirs_visible_infrared_contrails_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180902_suomiNPP_viirs_visible_infrared_contrails_AK_anim.gif\" alt=\"Suomi NPP VIIRS Visible (0.64 \u00b5m) and Infrared Window (11.45 \u00b5m) images [click to enlarge]\" width=\"639\" height=\"366\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS Visible (0.64 \u00b5m) and Infrared Window (11.45 \u00b5m) images [click to enlarge]<\/p><\/div>A curved portion of one of these contrails was seen on web camera images looking south from Atqasuk <em><strong>(below)<\/strong><\/em>.<\/p>\n<p><center><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p dir=\"ltr\" lang=\"en\">Webcam from Atqasuk earlier. <a href=\"https:\/\/twitter.com\/AlaskaWx?ref_src=twsrc%5Etfw\">@AlaskaWx<\/a> <a href=\"https:\/\/t.co\/VJbbLaqtJm\">pic.twitter.com\/VJbbLaqtJm<\/a><\/p>\n<p>\u2014 Brian Brettschneider (@Climatologist49) <a href=\"https:\/\/twitter.com\/Climatologist49\/status\/1036450351086370817?ref_src=twsrc%5Etfw\">September 3, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<p>&nbsp;<\/p>\n<p><\/center><\/p>\n","protected":false},"excerpt":{"rendered":"<p>A low moved eastward across the Beaufort Sea on 01 September 2018, bringing a cold front southward across the North Slope and Brooks Range in far northern Alaska (surface analyses). A sequence of Suomi NPP VIIRS Infrared Window (11.45 \u00b5m) images (above) showed the clearing of high\/cold clouds in the wake of the frontal passage. [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":29656,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[37,55,45,49,48,5],"tags":[],"class_list":["post-29654","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-arctic","category-landsat","category-redgreenblue-rgb-images","category-suomi_npp","category-viirs","category-winter-weather"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/29654","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=29654"}],"version-history":[{"count":20,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/29654\/revisions"}],"predecessor-version":[{"id":29679,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/29654\/revisions\/29679"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/29656"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=29654"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=29654"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=29654"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}