{"id":58,"date":"2006-09-06T22:08:15","date_gmt":"2006-09-06T22:08:15","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/2006\/09\/06\/valley-fog-smoke-aloft-and-lake-breeze-boundaries\/"},"modified":"2008-08-27T21:53:03","modified_gmt":"2008-08-27T21:53:03","slug":"valley-fog-smoke-aloft-and-lake-breeze-boundaries","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/58","title":{"rendered":"Valley fog, smoke aloft, and lake breeze boundaries"},"content":{"rendered":"<p>No shortage of satellite meteorology topics today over the Upper Midwest and Great Lakes regions! A look at the <a title=\"GOES-12 visible animation\" href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/misc\/blog\/060906_g12_visible.mov\" target=\"_blank\"><strong>GOES-12 visible channel animation<\/strong><\/a> <em><strong>(below, left)<\/strong><\/em> reveals the following features:<strong> (1)<\/strong> fingers of morning fog in the river valleys of southwestern Wisconsin, <strong>(2)<\/strong> areas of smoke aloft from wildfires burning in Canada and the Pacific Northwest, and <strong>(3)<\/strong> afternoon lake breeze boundaries that acted as a focus for thunderstorm development in both Wisconsin and lower Michigan.<\/p>\n<blockquote><p><em><strong>(1)<\/strong><\/em> As we have noted previously, these narrow fog features are often not detected using the 4 km resolution GOES fog\/stratus product, but the <strong><a title=\"AWIPS MODIS\/GOES fog product\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2006\/09\/060906_goes_modis_fog_wi.jpg\" target=\"_blank\">1 km resolution MODIS<\/a> <\/strong>fog\/stratus product <a title=\"AWIPS MODIS\/GOES fog product with observations\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2006\/09\/060906_goes_modis_fog_wi_obs.jpg\" target=\"_blank\"><em><strong>(with observations overlaid)<\/strong><\/em><\/a> is able to resolve the river valley fog in southwestern Wisconsin.<\/p>\n<p><em><strong>(2)<\/strong><\/em> While the smoke signature is subtle on the GOES-East (GOES-12) visible imagery, we can take advantage of a more favorable forward scattering geometry using the <a title=\"GOES-11 \/ GOES-12 visible\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2006\/09\/060906_g12_g11_vis.GIF\" target=\"_blank\"><strong>GOES-West (GOES-11)<\/strong><\/a> satellite to better see the areal extent of the smoke early in the day <a title=\"GOES-11 visible animation\" href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/misc\/blog\/060906_g11_vis.mov\" target=\"_blank\"><em><strong>(GOES-11 animation)<\/strong><\/em><\/a>. The smoke is also depicted as a large plume of high MODIS aerosol optical depth (AOD) extending from southern Canada to the Upper Midwest <em><strong>(below, right)<\/strong><\/em>. In addition, the thick smoke  contributed to a colorful  sunset (and sunrise) here in Madison (<a title=\"sunset photo 1\" href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/misc\/blog\/060906_sunset_3c.jpg\" target=\"_blank\"><strong><em>photo 1<\/em><\/strong><\/a> <a title=\"sunset photo 2\" href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/misc\/blog\/060906_sunset_2c.jpg\" target=\"_blank\">| <em><strong>photo 2<\/strong><\/em><\/a>). <em><strong><\/strong><\/em><\/p>\n<p><em><strong>(3)<\/strong><\/em> Narrow pockets of instability were noted on the <a title=\"AWIPS GOES sounder LI\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2006\/09\/060906_li_vis.jpg\" target=\"_blank\"><strong>GOES sounder lifted index (LI)<\/strong><\/a> derived product (values of -7 to -8 F), in the vicinity of the lake breeze boundaries in both Wisconsin and Michigan; <a title=\"SPC storm reports\" href=\"http:\/\/www.spc.noaa.gov\/climo\/reports\/060906_rpts.html\" target=\"_blank\"><strong>hail up to 1 inch in diameter<\/strong><\/a> was reported from the afternoon lake breeze convection in Wisconsin and Michigan.<\/p><\/blockquote>\n<p><a title=\"GOES-12 visible channel animation\" href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/misc\/blog\/060906_g12_visible.mov\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" id=\"image52\" title=\"GOES-12 visible channel\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2006\/09\/060906_g12_vis_31.GIF\" alt=\"GOES-12 visible channel\" width=\"220\" height=\"165\" align=\"left\" \/><\/a> <a title=\"MODIS AOD\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2006\/09\/modl_20060906.png\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" id=\"image54\" title=\"MODIS AOD\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2006\/09\/modl_20060906.png\" alt=\"MODIS AOD\" width=\"176\" height=\"164\" align=\"right\" \/><\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>No shortage of satellite meteorology topics today over the Upper Midwest and Great Lakes regions! A look at the GOES-12 visible channel animation (below, left) reveals the following features: (1) fingers of morning fog in the river valleys of southwestern Wisconsin, (2) areas of smoke aloft from wildfires burning in Canada and the Pacific Northwest, [&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":[13,15,18,19,12,3],"tags":[],"class_list":["post-58","post","type-post","status-publish","format-standard","hentry","category-fog-detection","category-goes-sounder","category-goes-11","category-goes-12","category-modis","category-severe-convection"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/58","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=58"}],"version-history":[{"count":2,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/58\/revisions"}],"predecessor-version":[{"id":863,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/58\/revisions\/863"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=58"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=58"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=58"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}