{"id":14861,"date":"2014-01-29T21:59:36","date_gmt":"2014-01-29T21:59:36","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=14861"},"modified":"2014-02-02T21:03:09","modified_gmt":"2014-02-02T21:03:09","slug":"great-lakes-ice","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/14861","title":{"rendered":"Great Lakes ice"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/01\/140129_1806z_suomi_npp_viirs_visible_rgb_great_lakes_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel and Snow\/cloud discrimination RGB images\" alt=\"Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel and Snow\/cloud discrimination RGB images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/01\/140129_1806z_suomi_npp_viirs_visible_rgb_great_lakes_anim.gif\" width=\"480\" height=\"287\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel and Snow\/cloud discrimination RGB images<\/p><\/div>\n<p>An AWIPS II image comparison of Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel data and the corresponding &#8220;Snow\/cloud discrimination&#8221; Red\/Green\/Blue (RGB) product <em><strong>(above)<\/strong><\/em> provided a glimpse of many of the areas of ice coverage on the Great Lakes at 18:06 UTC on <a title=\"29 January 2014 daily weather map\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20080116.html\"><strong>29 January 2014<\/strong><\/a>. Ice began to increase (especially across the western Great Lakes) in late January following one of the more significant arctic outbreaks of the 2013\/2014 winter season. On the RGB image, snow and ice appear as varying shades of red, in contrast to supercooled water droplet clouds which appear as shades of white.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/01\/140128_modis_truecolor_lake_ice_motion_MQT_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"TerTerra and Aqua MODIS true-color images (28 January)\" alt=\"Terra and Aqua MODIS true-color images (28 January)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/01\/140128_modis_truecolor_lake_ice_motion_MQT_anim.gif\" width=\"480\" height=\"312\" \/><\/a><p class=\"wp-caption-text\">Terra and Aqua MODIS true-color images (28 January)<\/p><\/div>\n<p>On the previous day (28 January), comparisons between 17:28 UTC Terra and 19:12 UTC Aqua MODIS true-color RGB images from the <a title=\"SSEC MODIS Today site\" href=\"http:\/\/ge.ssec.wisc.edu\/modis-today\/index.php?satellite=t1&amp;product=true_color&amp;date=2014_01_28_028&amp;overlay_sector=false&amp;overlay_state=true&amp;overlay_coastline=true\"><strong>SSEC MODIS Today<\/strong><\/a> site revealed the amount of sea ice motion in the relatively short time (approximately 100 minutes) between the 2 images, a result of fairly strong winds blowing over the nearshore waters. The MODIS image comparisons are centered over the Upper Peninsula of Michigan <em><strong>(above),<\/strong><\/em> and over southern Lake Michigan <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/01\/140128_modis_truecolor_lake_ice_motion_CHI_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"Terra and Aqua MODIS true-color images (28 January)\" alt=\"Terra and Aqua MODIS true-color images (28 January)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/01\/140128_modis_truecolor_lake_ice_motion_CHI_anim.gif\" width=\"480\" height=\"312\" \/><\/a><p class=\"wp-caption-text\">Terra and Aqua MODIS true-color images (28 January)<\/p><\/div>\n<p style=\"text-align: center;\">&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8211;<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/01\/140129_modis_truecolor_lake_ice_MQT_GRB_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"Terra and Aqua MODIS true-color images (29 January)\" alt=\"Terra and Aqua MODIS true-color images (29 January)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/01\/140129_modis_truecolor_lake_ice_MQT_GRB_anim.gif\" width=\"480\" height=\"311\" \/><\/a><p class=\"wp-caption-text\">Terra and Aqua MODIS true-color images (29 January)<\/p><\/div>\n<p>On 29 January, similar comparisons of the 16:34 UTC Terra and 18:16 UTC Aqua MODIS true-color RGB images showed a better view of the multiple long and narrow ice floes in northern lake Michigan <em><strong>(above),<\/strong><\/em> and showed how much ice in southern Lake Michigan had been blown across the lake and against the southeastern shore <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 489px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/01\/140129_modis_truecolor_lake_ice_CHI_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"Terra and Aqua MODIS true-color images (29 January)\" alt=\"Terra and Aqua MODIS true-color images (29 January)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/01\/140129_modis_truecolor_lake_ice_CHI_anim.gif\" width=\"479\" height=\"310\" \/><\/a><p class=\"wp-caption-text\">Terra and Aqua MODIS true-color images (29 January)<\/p><\/div>\n<p style=\"text-align: center;\"><strong>===== 31 January Update =====<\/strong><\/p>\n<div style=\"width: 489px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/01\/140131_1653z_landsat8_band8_lake_superior_ice_DLH_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"Landsat 8 Panochromatic (0.59 \u00c2\u00b5m Band 8) image\" alt=\"Landsat 8 Panochromatic (0.59 \u00c2\u00b5m Band 8) image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/01\/140131_1653z_landsat8_band8_lake_superior_ice_DLH_anim.gif\" width=\"479\" height=\"267\" \/><\/a><p class=\"wp-caption-text\">Landsat 8 Panochromatic (0.59 \u00c2\u00b5m Band 8) image<\/p><\/div>\n<p>A 15-meter resolution Landsat 8 Panochromatic (0.59 \u00c2\u00b5m Band 8) image from the <a title=\"SSEC RealEarth web map server\" href=\"http:\/\/wms.ssec.wisc.edu\/\"><strong>SSEC RealEarth<\/strong><\/a> web map server <em><strong>(above)<\/strong><\/em> showed the ice coverage in the far western portion of Lake Superior on 31 January. Land-fast ice in the Apostle Islands area of Wisconsin <em>(located in the eastern part of the image)<\/em> was thicker and snow-covered, giving it a brighter white appearance.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>An AWIPS II image comparison of Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel data and the corresponding &#8220;Snow\/cloud discrimination&#8221; Red\/Green\/Blue (RGB) product (above) provided a glimpse of many of the areas of ice coverage on the Great Lakes at 18:06 UTC on 29 January 2014. Ice began to increase (especially across the western Great Lakes) [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":14864,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[44,55,12,45,49,48,5],"tags":[],"class_list":["post-14861","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-awips-ii","category-landsat","category-modis","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\/14861","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=14861"}],"version-history":[{"count":8,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/14861\/revisions"}],"predecessor-version":[{"id":14870,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/14861\/revisions\/14870"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/14864"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=14861"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=14861"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=14861"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}