{"id":36122,"date":"2020-04-04T21:59:23","date_gmt":"2020-04-04T21:59:23","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=36122"},"modified":"2020-04-05T04:12:15","modified_gmt":"2020-04-05T04:12:15","slug":"signature-of-ice-accrual-across-the-upper-midwest","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/36122","title":{"rendered":"Signature of ice accrual across the Upper Midwest"},"content":{"rendered":"<p><div style=\"width: 654px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200402_200403_goes16_waterVapor_precipitationType_Upper_Midwest_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/G16_WV_MIDWEST_ICE_02_03APR2020_B9_2020094_060117_GOES-16_0001PANEL_FRAME00361.GIF\" alt=\"GOES-16 Mid-level Water Vapor (6.9 \u00b5m) images, with hourly precipitation type plotted in red [click to play animation | MP4]\" width=\"644\" height=\"479\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Mid-level Water Vapor<em> (6.9 \u00b5m)<\/em> images, with hourly precipitation type plotted in red [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200402_200403_goes16_waterVapor_precipitationType_Upper_Midwest_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-16 <em>(GOES-East)<\/em> Mid-level Water Vapor (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band09.pdf\"><strong>6.9 \u00b5m<\/strong><\/a>) images <em><strong>(above)<\/strong> <\/em>showed a variety of precipitation types as a strong cold front moved slowly eastward across the Upper Midwest during the <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20200402.html\"><strong>02 April<\/strong><\/a> &#8211; <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20200403.html\"><strong>03 April 2020<\/strong><\/a> period &#8212; including thundersnow snow at Aberdeen, South Dakota and Oakes, North Dakota (at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/G16_WV_MIDWEST_ICE_02_03APR2020_B9_2020093_180117_GOES-16_0001PANEL_FRAME00217.GIF\"><strong>18 UTC on 02 April<\/strong><\/a>) and <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200403_ice_lsr.text\"><strong>freezing rain<\/strong><\/a> at a few sites in northern Iowa, the eastern Dakotas and western Minnesota.<\/p>\n<p>On the following day, in a comparison of GOES-16 &#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_DaySnowFog.pdf\"><strong>Day Snow Fog<\/strong><\/a> Red-Green-Blue (RGB) images <em><strong>(below)<\/strong>,<\/em> the RGB images revealed darker red swaths across southeastern South Dakota, northwestern Iowa and western Minnesota (at the 1.61 \u00b5m wavelength, ice absorbs radiation more strongly than snow &#8212; which contributed to the darker appearance of those swaths). Note that these ice accrual swaths exhibited no signature in the Visible imagery.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200404_goes16_visible_daySnowFogRGB_Upper_Midwest_ice_acretion_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/uwm_rgb-20200404_142117.png\" alt=\"GOES-16 &quot;Red&quot; Visible (0.64 \u00b5m) and Day Snow Fog RGB images [click to play animation | MP4]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible <em>(0.64 \u00b5m)<\/em> and Day Snow Fog RGB images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/04\/200404_goes16_visible_daySnowFogRGB_Upper_Midwest_ice_acretion_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Props to Carl Jones (NWS Grand Forks) for pointing this feature out.<br \/>\n<center><\/p>\n<blockquote class=\"twitter-tweet\">\n<p dir=\"ltr\" lang=\"en\">Dark red swath extending through Minnesota is <a href=\"https:\/\/twitter.com\/hashtag\/ice?src=hash&amp;ref_src=twsrc%5Etfw\">#ice<\/a> accretion from April 2-3 winter storm. Strong infrared absorption in the 1.61 component of the Day Snow-Fog RGB makes it darker compared to snow. Clearly shows where ice accretion occurred whereas visible cannot. <a href=\"https:\/\/twitter.com\/hashtag\/ndwx?src=hash&amp;ref_src=twsrc%5Etfw\">#ndwx<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/mnwx?src=hash&amp;ref_src=twsrc%5Etfw\">#mnwx<\/a> <a href=\"https:\/\/t.co\/L1rs7EskLa\">pic.twitter.com\/L1rs7EskLa<\/a><\/p>\n<p>\u2014 Carl Jones (@northflwx) <a href=\"https:\/\/twitter.com\/northflwx\/status\/1246442118811394048?ref_src=twsrc%5Etfw\">April 4, 2020<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/center><\/p>\n","protected":false},"excerpt":{"rendered":"<p>GOES-16 (GOES-East) Mid-level Water Vapor (6.9 \u00b5m) images (above) showed a variety of precipitation types as a strong cold front moved slowly eastward across the Upper Midwest during the 02 April &#8211; 03 April 2020 period &#8212; including thundersnow snow at Aberdeen, South Dakota and Oakes, North Dakota (at 18 UTC on 02 April) and [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":36124,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[74,45,5],"tags":[],"class_list":["post-36122","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-16","category-redgreenblue-rgb-images","category-winter-weather"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/36122","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=36122"}],"version-history":[{"count":9,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/36122\/revisions"}],"predecessor-version":[{"id":36132,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/36122\/revisions\/36132"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/36124"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=36122"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=36122"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=36122"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}