{"id":11900,"date":"2012-11-28T20:05:56","date_gmt":"2012-11-28T20:05:56","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=11900"},"modified":"2012-12-11T14:43:40","modified_gmt":"2012-12-11T14:43:40","slug":"strong-tornado-in-southern-italy","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/11900","title":{"rendered":"Strong Tornado in southern Italy"},"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\/11\/MET9_IR9_28NOV12_ENVLOOP.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"Meteosat-9 10.8 \u00c2\u00b5m infrared channel images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/11\/MET9_IR9_28NOV2012_0915.GIF\" alt=\"Meteosat-9 10.8 \u00c2\u00b5m infrared channel images (click image to play animation)\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">Meteosat-9 10.8 \u00c2\u00b5m infrared channel images (click image to play animation)<\/p><\/div>\n<p>A rare November tornado moved through Taranto, (<a href=\"http:\/\/www.youtube.com\/watch?v=a-wkjemVZJ4\">YouTube video<\/a>, <a href=\"http:\/\/www.accuweather.com\/en\/weather-news\/tornado-italy\/2092115\">AccuWeather blog entry<\/a>) in southern Italy, on Wednesday November 28th. A loop of 10.8 \u00c2\u00b5m Meteosat-9 imagery (above) shows the development of an overshooting top in a thunderstorm that is moving over Taranto between 0900 and 0915 UTC (Note that the time indicated on the satellite image is the <em>nominal time<\/em> &#8212; the time that the satellite <em>starts<\/em> scanning.  The <strong>actual<\/strong> scan time over southern Italy is approximately 10 minutes later than the nominal time).  Such cloud-top features are frequently associated with severe weather.  A faint suggestion of an enhanced-V\/thermal couplet is apparent in the later imagery as the strong thunderstorm moves northward across the Salento peninsula and then into the Adriatic Sea.  METOP-A infrared imagery (below) shows the thunderstorm complex about an hour before a tornadic storm moved inland from the Ionian Sea. The corresponding Meteosat-9 image is <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/11\/MET9_IR9_28NOV2012_0845.GIF\">here<\/a>.  The higher spatial resolution of the polar orbiter METOP-A allows the discernment of much finer detail in the cloud-top features.  <\/p>\n<div style=\"width: 489px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/11\/METOPA_IR4_28NOV2012_0842UTC.GIF\"><img loading=\"lazy\" decoding=\"async\" title=\"METOP-A 10.8 \u00c2\u00b5m IR imagery\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/11\/METOPA_IR4_28NOV2012_0842UTC.GIF\" alt=\"METOP-A 10.8 \u00c2\u00b5m IR imagery\" width=\"479\" height=\"320\" \/><\/a><p class=\"wp-caption-text\">METOP-A 10.8 \u00c2\u00b5m IR imagery<\/p><\/div>\n<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\/11\/\/METEOSAT9_VIS_28NOV2012_visloop.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"Meteosat-9 0.6 \u00c2\u00b5m visible channel images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/11\/METEOSAT9_VIS_28NOV2012_0915UTC.GIF\" alt=\"Meteosat-9 0.6 \u00c2\u00b5m visible channel images (click image to play animation)\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">Meteosat-9 0.6 \u00c2\u00b5m visible channel images (click image to play animation)<\/p><\/div>\n<p>Visible imagery from Meteosat-9, above, also shows the development of the overshooting top associated with the tornadic cell.  A higher-resolution visible imager from METOP-B, below, showed the line of thunderstorms in which the tornadic cell, indicated by the yellow arrow, was embedded.<\/p>\n<div style=\"width: 489px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/11\/METOPB_28NOV2012_0935UTC.GIF\"><img loading=\"lazy\" decoding=\"async\" title=\"METOP-B 0.63 \u00c2\u00b5m Visible imagery\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/11\/METOPB_28NOV2012_0935UTC.GIF\" alt=\"METOP-B 0.63 \u00c2\u00b5m Visible imagery\" width=\"479\" height=\"320\" \/><\/a><p class=\"wp-caption-text\">METOP-B 0.63 \u00c2\u00b5m Visible imagery<\/p><\/div>\n<p>The tornadic weather was associated with an exceptionally deep extratropical cyclone. On Monday, that system was over the northwestern Mediterranean (see below), with ample evidence of exceptionally cold upper-level air over the Bay of Biscay. This storm also had a history of producing supercellular thunderstorms, as evidenced by the storm development just south of France in the animation below.<\/p>\n<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\/11\/M9VIS_27Nov_loop.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"Meteosat-9 Visible imagery (0.6 \u00c2\u00b5m) (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/11\/M9VIS_27Nov_0930_00.GIF\" alt=\"Meteosat-9 Visible imagery (0.6 \u00c2\u00b5m) (click image to play animation)\" width=\"480\" height=\"320\" \/><\/a><p class=\"wp-caption-text\">Meteosat-9 Visible imagery (0.6 \u00c2\u00b5m) (click image to play animation)<\/p><\/div>\n<p>A multi-day loop of the Meteosat-9 infrared window channel imagery is below.  It shows the strong extratropical cyclone moving across southern Europe.<\/p>\n<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\/11\/M9_IR9_loop_24_29Nov.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"Meteosat-9 10.8 \u00c2\u00b5m infrared channel images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2012\/11\/M9_IR9_27NOV2012_1615UTC.GIF\" alt=\"Meteosat-9 10.8 \u00c2\u00b5m infrared channel images (click image to play animation)\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">Meteosat-9 10.8 \u00c2\u00b5m infrared channel images (click image to play animation)<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>A rare November tornado moved through Taranto, (YouTube video, AccuWeather blog entry) in southern Italy, on Wednesday November 28th. A loop of 10.8 \u00c2\u00b5m Meteosat-9 imagery (above) shows the development of an overshooting top in a thunderstorm that is moving over Taranto between 0900 and 0915 UTC (Note that the time indicated on the satellite [&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":[10,23,47,26,3],"tags":[],"class_list":["post-11900","post","type-post","status-publish","format-standard","hentry","category-general-interpretation","category-meteosat","category-other-satellites","category-poes","category-severe-convection"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/11900","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=11900"}],"version-history":[{"count":22,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/11900\/revisions"}],"predecessor-version":[{"id":11982,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/11900\/revisions\/11982"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=11900"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=11900"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=11900"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}