{"id":9955,"date":"2012-03-12T21:19:02","date_gmt":"2012-03-12T21:19:02","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=9955"},"modified":"2012-03-13T21:27:51","modified_gmt":"2012-03-13T21:27:51","slug":"possible-sting-jet-in-upper-midwest","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/9955","title":{"rendered":"Possible Sting Jet in Upper Midwest"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/Reg_Water_Vapor_20120312_Loop.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"GOES-13 6.5 \u00c2\u00b5m water vapor channel images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/Reg_Water_Vapor_20120312_1015.png\" alt=\"GOES-13 6.5 \u00c2\u00b5m water vapor channel images (click image to play animation)\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-13 6.5 \u00c2\u00b5m water vapor channel images (click image to play animation)<\/p><\/div>\n<p>The water vapor animation from GOES-East on March 12th shows a structure rotating through the upper-level trough, which structure looks very much like a so-called &#8220;Sting Jet&#8221;.  (In the animation above, the sting jet structure crosses the Missouri\/Kansas border south of Kansas City, propagates across northern Missouri and eastern Iowa before moving northward into Wisconsin).  (A more obvious Sting Jet event is discussed <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/9502\">here<\/a>;  A <em>Monthly Weather Review<\/em> article on Sting Jets is <a href=\"http:\/\/journals.ametsoc.org\/doi\/full\/10.1175\/2010MWR3290.1\">here<\/a>).<\/p>\n<p>RUC wind analyses show that the sting jet structure was associated with a wind maximum on the 315 Kelvin isentropic surface.  <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/RUC13_315K_Windspeed_20120312_Loop.gif\">This Loop<\/a> shows the maximum moving from northeastern Missouri into Central Wisconsin between 1000 and 1400 UTC on March 12th.  Stability in the lower troposphere on March 12th (as suggested by <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/KDVN_20120312_1200.png\">this sounding<\/a> from the Quad Cities in Iowa\/Illinois) was strong enough to inhibit vertical mixing of stronger upper-tropospheric air down towards the surface.   The circulation around the jet was sufficient, however, to generate showers over the upper Midwest, as shown in <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/mosaic_0.5_Refl_20120312_Loop.gif\">this loop<\/a>.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/MODIS_WV_20120312_0841.png\"><img loading=\"lazy\" decoding=\"async\" alt=\"MODIS 6.5 \u00c2\u00b5m water vapor channel image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/MODIS_WV_20120312_0841.png\" alt=\"MODIS 6.5 \u00c2\u00b5m water vapor channel image\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">MODIS 6.5 \u00c2\u00b5m water vapor channel image<\/p><\/div>\n<p>MODIS water vapor imagery, above, from 0841 UTC on 12 March shows the sting jet structure in north-central Missouri, and curving back to central Nebraska and central South Dakota.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/VIS_12MARCH12_Loop.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"GOES-13 0.63 \u00c2\u00b5m visible image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/VIS_12MARCH12_Loop.gif\" alt=\"GOES-13 0.63 \u00c2\u00b5m visible image\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-13 0.63 \u00c2\u00b5m visible image<\/p><\/div>\n<p>(Added 13 March: <A href=\"http:\/\/spc.noaa.gov\/climo\/reports\/120312_rpts.html\">SPC Storm Reports<\/a> show a <a href=\"http:\/\/www.crh.noaa.gov\/news\/display_cmsstory.php?wfo=dtx&#038;storyid=80607&#038;source=0\">rare March tornado north of I-69<\/a> in lower Michigan.  The visible imagery above, bracketing the observed time of the tornado (near the yellow box), shows a strong thunderstorm.  By this time, the possible sting jet has rotated northward into western Ontario, so its influence on the environment in Michigan would be secondary.  The <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/03\/KDTX_20120312_2300.png\">sounding from DTX at 2300 UTC<\/a> shows a favorable low-level wind profile.)<\/p>\n","protected":false},"excerpt":{"rendered":"<p>The water vapor animation from GOES-East on March 12th shows a structure rotating through the upper-level trough, which structure looks very much like a so-called &#8220;Sting Jet&#8221;. (In the animation above, the sting jet structure crosses the Missouri\/Kansas border south of Kansas City, propagates across northern Missouri and eastern Iowa before moving northward into Wisconsin). [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[10,11,12],"tags":[],"class_list":["post-9955","post","type-post","status-publish","format-standard","hentry","category-general-interpretation","category-goes-13","category-modis"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/9955","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=9955"}],"version-history":[{"count":13,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/9955\/revisions"}],"predecessor-version":[{"id":9967,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/9955\/revisions\/9967"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=9955"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=9955"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=9955"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}