{"id":38670,"date":"2020-10-16T23:59:22","date_gmt":"2020-10-16T23:59:22","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=38670"},"modified":"2020-10-24T16:58:49","modified_gmt":"2020-10-24T16:58:49","slug":"early-season-snowfall-across-the-northern-plains","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/38670","title":{"rendered":"Early-season snowfall across the northern Plains"},"content":{"rendered":"<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201016_goes16_visible_dayCloudPhaseDistinction_ND_snowfall_swaths_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/nd_rgb-20201016_150114.png\" alt=\"GOES-16 \" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible<em> (0.64 \u00b5m)<\/em> and Day Cloud Phase Distinction RGB images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201016_goes16_visible_dayCloudPhaseDistinction_ND_snowfall_swaths_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-16 <em>(GOES-East)<\/em> &#8220;Red&#8221; Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>) and <a href=\"http:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/QuickGuide_DayCloudPhaseDistinction_final_v2.pdf\"><strong>Day Cloud Phase Distinction<\/strong><\/a> Red-Green-Blue (RGB) images <em><strong>(above)<\/strong><\/em> showed multiple long, narrow northwest-to-southeast oriented swaths of snow cover extending across much of North Dakota into western Minnesota early in the day on <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20201016.html\"><strong>16 October 2020<\/strong><\/a>. The snow swaths &#8212; which appeared as brighter shades of green in the RGB images &#8212; slowly melted during the late morning and early afternoon hours.<\/p>\n<p>A toggle between NOAA-20 VIIRS Sea Surface Temperature (SST) product and Infrared Window (11.45 \u00b5m) images at 0843 UTC<em><strong> (below)<\/strong><\/em> displayed a northwest-to-southeast cloud band that extended from Lake Sakakawea (which exhibited SST values in the low\/mid 50s F) to the Bismarck (KBIS) \/ Mandan area. Note that Mandan (located just west of KBIS) was reporting &#8220;precipitation of unknown type&#8221; with an air temperature of 32\u00baF &#8212; indicating that this feature was a lake effect cloud band which was producing light precipitation (predominantly snow).<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201016_0843utc_noaa20_seaSurfaceTemperature_infrared_ND_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201016_0843utc_noaa20_seaSurfaceTemperature_infrared_ND_anim.gif\" alt=\"NOAA-20 Sea Surface Temperature product and Infrared Window (11.45 \u00b5m) images at 0843 UTC [click to enlarge]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">NOAA-20 VIIRS Sea Surface Temperature product and Infrared Window<em> (11.45 \u00b5m)<\/em> images at 0843 UTC [click to enlarge]<\/p><\/div><br \/>\n<center><\/p>\n<blockquote class=\"twitter-tweet\">\n<p dir=\"ltr\" lang=\"en\">Yes there was. In fact we had some flakes from that band here at the office in Bismarck too. <a href=\"https:\/\/t.co\/h8h5Aaljlv\">pic.twitter.com\/h8h5Aaljlv<\/a><\/p>\n<p>\u2014 NWS Bismarck (@NWSBismarck) <a href=\"https:\/\/twitter.com\/NWSBismarck\/status\/1317706295642738689?ref_src=twsrc%5Etfw\">October 18, 2020<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<p><\/center><\/p>\n<p style=\"text-align: center;\"><strong>=====17 October Update =====<\/strong><\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201017_goes16_dayCloudPhaseDistinctionRGB_MT_ND_snowfall_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/mt_nd_rgb-20201017_182114.png\" alt=\"GOES-16 Day Cloud Phase Distinction RGB images [click to play animation | MP4]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Day Cloud Phase Distinction RGB images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201017_goes16_dayCloudPhaseDistinctionRGB_MT_ND_snowfall_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>On the following day, GOES-16 Day Cloud Phase Distinction RGB images <em><strong>(above)<\/strong><\/em> showed a new, broader swath of snow cover from southern Saskatchewan and northeastern Montana into North Dakota that was produced by a clipper-type disturbance (<strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201017_surface_analyses_anim.gif\">surface analyses<\/a><\/strong>). For this event, snowfall amounts were as high as 3.5 inches in northeastern Montana and 2.1 inches in North Dakota (<a href=\"https:\/\/www.nohrsc.noaa.gov\/interactive\/html\/map.html?ql=station&amp;zoom=&amp;loc=54.618+N%2C+109.358+W&amp;var=snowfall_obs_24_h&amp;dy=2020&amp;dm=10&amp;dd=17&amp;dh=19&amp;snap=1&amp;o9=1&amp;o12=1&amp;o13=1&amp;lbl=m&amp;mode=pan&amp;extents=us&amp;min_x=-109.39166666667&amp;min_y=39.716666666663&amp;max_x=-94.391666666668&amp;max_y=54.716666666662&amp;coord_x=-101.89166666666901&amp;coord_y=47.216666666662505&amp;zbox_n=&amp;zbox_s=&amp;zbox_e=&amp;zbox_w=&amp;metric=0&amp;bgvar=dem&amp;shdvar=shading&amp;width=1600&amp;height=1600&amp;nw=1600&amp;nh=1600&amp;h_o=0&amp;font=1&amp;js=1&amp;uc=0\"><strong>NOHRSC<\/strong><\/a>) &#8212; so the rate of snow melt was slower than what was seen on the previous day.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>GOES-16 (GOES-East) &#8220;Red&#8221; Visible (0.64 \u00b5m) and Day Cloud Phase Distinction Red-Green-Blue (RGB) images (above) showed multiple long, narrow northwest-to-southeast oriented swaths of snow cover extending across much of North Dakota into western Minnesota early in the day on 16 October 2020. The snow swaths &#8212; which appeared as brighter shades of green in the [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":38672,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[74,78,45,48,5],"tags":[],"class_list":["post-38670","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-16","category-noaa-20","category-redgreenblue-rgb-images","category-viirs","category-winter-weather"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/38670","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=38670"}],"version-history":[{"count":8,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/38670\/revisions"}],"predecessor-version":[{"id":38739,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/38670\/revisions\/38739"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/38672"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=38670"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=38670"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=38670"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}