{"id":46432,"date":"2022-05-20T15:25:32","date_gmt":"2022-05-20T15:25:32","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=46432"},"modified":"2022-05-20T18:52:47","modified_gmt":"2022-05-20T18:52:47","slug":"bore-features-over-lake-michigan","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/46432","title":{"rendered":"Bore features over Lake Michigan"},"content":{"rendered":"\n<figure class=\"wp-block-video\"><video height=\"816\" style=\"aspect-ratio: 1372 \/ 816;\" width=\"1372\" controls loop src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/05\/g16_abi_radc_true_color_night_20220520_111117_39.mp4\"><\/video><figcaption>GOES-16 True Color Imagery from the CSPP Geosphere site, 1111 &#8211; 1421 UTC on 20 May 2022<\/figcaption><\/figure>\n\n\n\n<p>The true-color animation above, produced from the  <a href=\"https:\/\/geosphere.ssec.wisc.edu\/\">CSPP Geosphere<\/a> site, shows bore-like cloud features over northern Lake Michigan shortly after sunrise on 20 May 2022.  These parallel lines of clouds are mostly likely to persist in regions where a low-level inversion is present.  NUCAPS profiles from the 0800 UTC overpass of NOAA-20, shown below, show an inversion below 850 mb over the central parts of the Upper Peninsula of Michigan.  The cold waters over the lake would likely amplify the strength of this inversion.  The Green Bay soundings from 1200 UTC (<a href=\"https:\/\/weather.uwyo.edu\/cgi-bin\/sounding?region=naconf&amp;TYPE=GIF%3ASKEWT&amp;YEAR=2022&amp;MONTH=05&amp;FROM=2012&amp;TO=2012&amp;STNM=72645\">here<\/a>, from <a href=\"https:\/\/weather.uwyo.edu\/upperair\/sounding.html\">this site<\/a>), also shows a low-level stable layer.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/05\/NUCAPS_Profiles_LakeMichiganBore_20May2022.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"576\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/05\/NUCAPS_Profiles_LakeMichiganBore_20May2022-1024x576.png\" alt=\"\" class=\"wp-image-46434\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/05\/NUCAPS_Profiles_LakeMichiganBore_20May2022-1024x576.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/05\/NUCAPS_Profiles_LakeMichiganBore_20May2022-300x169.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/05\/NUCAPS_Profiles_LakeMichiganBore_20May2022-768x432.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/05\/NUCAPS_Profiles_LakeMichiganBore_20May2022.png 1280w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption>NUCAPS Profiles over Upper Michigan as indicated, ca. 0800 UTC on 20 May 2022.  NUCAPS Sounding Availability points also shown (click to enlarge).<\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator\" \/>\n\n\n\n<p>Thanks to Rick Mamrosh, WFO GRB, for bringing these cloud features to our attention!  <a href=\"https:\/\/www.facebook.com\/NWSGreenBay\/posts\/373187888170232?__cft__[0]=AZVB8o3-_otOTOJtAe2TasI_l11VPU1NeJZEv8Xsq4dhmH2V_lpg_bocCGLHuAH5wywZK-xQMMwCtsff1tdbU14I7G10HmDnB87mrqkUaoC3lScS5uew2Ojjd5ItXGwcewkGRJrk9lWuis2hX__qFvJpOy8izLq5EgruGfhiLerk-w&amp;__tn__=%2CO%2CP-R\">Check out the link<\/a> on their <a href=\"https:\/\/www.facebook.com\/NWSGreenBay\">Facebook page<\/a>.<\/p>\n\n\n\n<figure class=\"wp-block-embed is-type-rich is-provider-twitter wp-block-embed-twitter\"><div class=\"wp-block-embed__wrapper\">\n<blockquote class=\"twitter-tweet\" data-width=\"500\" data-dnt=\"true\"><p lang=\"en\" dir=\"ltr\">1-minute Mesoscale Sector <a href=\"https:\/\/twitter.com\/NOAASatellites?ref_src=twsrc%5Etfw\">@NOAASatellites<\/a>  <a href=\"https:\/\/twitter.com\/hashtag\/GOES16?src=hash&amp;ref_src=twsrc%5Etfw\">#GOES16<\/a>\/<a href=\"https:\/\/twitter.com\/hashtag\/GOESeast?src=hash&amp;ref_src=twsrc%5Etfw\">#GOESeast<\/a> Visible images showing an undular bore created by convective outflow over Lake Michigan: <a href=\"https:\/\/t.co\/fIDyAg1Iw7\">https:\/\/t.co\/fIDyAg1Iw7<\/a> More from <a href=\"https:\/\/twitter.com\/WxSatChat?ref_src=twsrc%5Etfw\">@WxSatChat<\/a>: <a href=\"https:\/\/t.co\/emieaB9tyt\">https:\/\/t.co\/emieaB9tyt<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/WIwx?src=hash&amp;ref_src=twsrc%5Etfw\">#WIwx<\/a> <a href=\"https:\/\/twitter.com\/hashtag\/MIwx?src=hash&amp;ref_src=twsrc%5Etfw\">#MIwx<\/a> <a href=\"https:\/\/t.co\/oBxAqnNunT\">pic.twitter.com\/oBxAqnNunT<\/a><\/p>&mdash; Scott Bachmeier (@CIMSS_Satellite) <a href=\"https:\/\/twitter.com\/CIMSS_Satellite\/status\/1527721627588481028?ref_src=twsrc%5Etfw\">May 20, 2022<\/a><\/blockquote><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script>\n<\/div><\/figure>\n\n\n","protected":false},"excerpt":{"rendered":"<p>The true-color animation above, produced from the CSPP Geosphere site, shows bore-like cloud features over northern Lake Michigan shortly after sunrise on 20 May 2022. These parallel lines of clouds are mostly likely to persist in regions where a low-level inversion is present. NUCAPS profiles from the 0800 UTC overpass of NOAA-20, shown below, show [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":46434,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[74,78,83],"tags":[],"class_list":["post-46432","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-16","category-noaa-20","category-nucaps"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/46432","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\/19"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=46432"}],"version-history":[{"count":4,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/46432\/revisions"}],"predecessor-version":[{"id":46438,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/46432\/revisions\/46438"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/46434"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=46432"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=46432"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=46432"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}