{"id":586,"date":"2007-12-13T23:55:33","date_gmt":"2007-12-13T23:55:33","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/586"},"modified":"2010-05-20T20:44:26","modified_gmt":"2010-05-20T20:44:26","slug":"ice-in-the-upper-midwest","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/586","title":{"rendered":"Ice in the Upper Midwest"},"content":{"rendered":"<p><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/12\/071213_modis_vis_ice_2_anim.gif\" title=\"MODIS visible + snow\/ice images (Animated GIF)\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/12\/071213_modis_vis_ice_2_anim.gif\" title=\"MODIS visible + snow\/ice images (Animated GIF)\" alt=\"MODIS visible + snow\/ice images (Animated GIF)\" align=\"middle\" height=\"464\" width=\"480\" \/><\/a><\/p>\n<p>AWIPS images of the MODIS visible and &#8220;snow\/ice&#8221; channels from <a href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20071213.html\" title=\"13 December 2007 daily weather map\" target=\"_blank\"><strong>13 December 2007<\/strong><\/a> <em><strong>(above; <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/12\/071213_modis_vis_ice_anim.gif\" title=\"MODIS visible + snow\/ice images (Animated GIF)\" target=\"_blank\">closer view<\/a>)<\/strong><\/em> reveal that much of the southeastern half of Iowa received a significant glazing of ice <em>(0.25 to 1.0 inch)<\/em> during a <a href=\"http:\/\/www.crh.noaa.gov\/crnews\/display_story.php?wfo=dvn&amp;storyid=11517&amp;source=0\" title=\"ice storm accumulation map\" target=\"_blank\"><strong>freezing drizzle\/freezing rain event on 10-11 December<\/strong><\/a>. Snow and ice particles are very <em>strong absorbers<\/em> at the 1.6 \u00c2\u00b5m wavelength of the MODIS snow\/ice channel <em>[Baum et al., 2000],<\/em> so the thick coating of ice on top of existing snow cover shows up as a very <em>dark<\/em> feature on those images <em>(even darker than adjacent areas to the north which had <strong><a href=\"http:\/\/www.nohrsc.nws.gov\/interactive\/html\/map.html?mode=pan&amp;zoom=&amp;center_x=++-95.654&amp;center_y=+++45.443&amp;ql=station&amp;var=snow_depth_obs_24_h&amp;dy=2007&amp;dm=12&amp;dd=13&amp;dh=12&amp;snap=1&amp;o9=1&amp;o12=1&amp;o13=1&amp;lbl=m&amp;min_x=-95.683749999991&amp;min_y=37.463334019974&amp;max_x=-87.367083333325&amp;max_y=45.78000068664&amp;coord_x=-91.525416666658&amp;coord_y=41.621667353307004&amp;zbox_n=&amp;zbox_s=&amp;zbox_e=&amp;zbox_w=&amp;metric=0&amp;bgvar=dem&amp;width=1000&amp;height=1000&amp;nw=1000&amp;nh=1000&amp;type=0&amp;js=1&amp;uc=0\" title=\"NOHRSC snow depth\" target=\"_blank\">more snow cover<\/a><\/strong> but did <strong>not<\/strong> receive significant amounts of freezing rain).<\/em>  In contrast, supercooled water droplet clouds show up as much <em>brighter<\/em> features on the MODIS snow\/ice channel image.<\/p>\n<p>A  false-color RGB composite using the MODIS visible and 1.6 \u00c2\u00b5m images  <em><strong>(below)<\/strong><\/em>  shows the region of significant ice glazing as the transition to deeper red colors.<\/p>\n<p><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/12\/071213_MODIS_CH010707_RGB.JPG\" title=\"MODIS false color composite image\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/12\/071213_MODIS_CH010707_RGB.JPG\" title=\"MODIS false color composite image\" alt=\"MODIS false color composite image\" align=\"middle\" height=\"360\" width=\"480\" \/><br \/>\n<\/a><\/p>\n<p>A comparison with the MODIS snow\/ice channel image from the previous day  <em><strong>(below)<\/strong><\/em> shows that the significant ice accumulation <em>(darker black enhancement)<\/em> also extended to the northeast, covering parts of northern Illinois and extreme southern\/southeastern Wisconsin. It is interesting to compare this event with another case of significant ice glazing that was seen on MODIS imagery in the <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/misc\/modis\/ice_storm\/020201.html\" title=\"southern Plains ice storm (February 2002)\" target=\"_blank\"><strong>southern Plains back in February 2002<\/strong><\/a>.<\/p>\n<p><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/12\/071212-13_modis_ice_anim.gif\" title=\"MODIS snow\/ice images (Animated GIF)\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/12\/071212-13_modis_ice_anim.gif\" title=\"MODIS snow\/ice images (Animated GIF)\" alt=\"MODIS snow\/ice images (Animated GIF)\" align=\"middle\" height=\"466\" width=\"482\" \/><\/a><\/p>\n<p>For photos of the ice accumulation in extreme northwestern  Missouri, see the <a href=\"http:\/\/www.extremeinstability.com\/07-12-10.htm\" title=\"ice storm photos\" target=\"_blank\"><strong>website from storm chaser Mike Hollingshead<\/strong><\/a>.<\/p>\n<p><strong>Reference:<\/strong> Baum, B.A., P.F. Soulen, K.I. Strabala, M.D. King, S.A. Ackerman, W. P. Menzel, and P. Yang: <em>Remote sensing of cloud properties using MODIS airborne simulator imagery during SUCCESS,<\/em>  J. Geophys. Res., <strong>105<\/strong>, 11781-11792, 2000.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>AWIPS images of the MODIS visible and &#8220;snow\/ice&#8221; channels from 13 December 2007 (above; closer view) reveal that much of the southeastern half of Iowa received a significant glazing of ice (0.25 to 1.0 inch) during a freezing drizzle\/freezing rain event on 10-11 December. Snow and ice particles are very strong absorbers at the 1.6 [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[12,45,5],"tags":[],"class_list":["post-586","post","type-post","status-publish","format-standard","hentry","category-modis","category-redgreenblue-rgb-images","category-winter-weather"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/586","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=586"}],"version-history":[{"count":1,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/586\/revisions"}],"predecessor-version":[{"id":5743,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/586\/revisions\/5743"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=586"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=586"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=586"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}