{"id":3838,"date":"2009-11-19T21:19:35","date_gmt":"2009-11-19T21:19:35","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=3838"},"modified":"2010-10-19T20:02:17","modified_gmt":"2010-10-19T20:02:17","slug":"3838","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/3838","title":{"rendered":"Atmospheric river of moisture targets Britain and Ireland"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/11\/091117-19_mimic_tpw_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"MIMIC Total Precipitable Water product\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/11\/091117-19_mimic_tpw_anim.gif\" alt=\"MIMIC Total Precipitable Water product\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">MIMIC Total Precipitable Water product<\/p><\/div>\n<p>AWIPS images of the <strong><a href=\"http:\/\/cimss.ssec.wisc.edu\/tropic\/real-time\/tpw2\/global2\/main.html\">MIMIC Total Precipitable Water<\/a><\/strong> (TPW) product <strong><em>(above)<\/em><\/strong> revealed the formation of a long &#8220;<a title=\"atmospheric rivers resources\" href=\"http:\/\/search.usa.gov\/search?query=atmospheric+river&amp;locale=en&amp;m=&amp;commit=Search\" target=\"_blank\"><strong>atmospheric river<\/strong><\/a>&#8221; of moisture over the North Atlantic Ocean during the <strong>17-19 November 2009<\/strong> period. MIMIC TPW values were as high as <strong>60 mm<\/strong> <em>(darker orange color enhancement)<\/em> within the  moisture plume.<\/p>\n<p>The surface analysis <strong><em>(below)<\/em><\/strong> showed that this moist plume was along and ahead of a cold front that was trailing southward from a deepening mid-latitude cyclone. This plume of moisture was contributing to very heavy rainfall and significant flooding over parts of the United Kingdom  &#8212; Seathwaite reported a 24-hour rainfall amount of 12.36 inches (314 mm), which if confirmed as accurate will set a new record for 24-hour precipitation in the UK <em>(<strong><a href=\"http:\/\/www.metoffice.gov.uk\/corporate\/pressoffice\/2009\/pr20091120.html\">UK Met Office<\/a><\/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\/2009\/11\/091118-19_sfc_analysis_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"MIMIC TPW with surface analysis\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/11\/091118-19_sfc_analysis_anim.gif\" alt=\"MIMIC TPW with surface analysis\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">MIMIC TPW with surface analysis<\/p><\/div>\n<p>A composite of GOES-12 and Meteosat-9 water vapor imagery <strong><em>(below)<\/em><\/strong> suggested that this long atmospheric river tapped into a pocket of deep tropical moisture <em>(associated with the remnants of what was formerly Hurricane\/Tropical Storm Ida),<\/em> and was then brought northward within the warm conveyor belt in advance of the deepening cyclone over the North Atlantic Ocean.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/11\/0911_4sat_wv_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-12 and Meteosat-9 water vapor imagery\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/11\/0911_4sat_wv_anim.gif\" alt=\"GOES and Meteosat water vapor imagery\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">GOES-12 and Meteosat-9 water vapor imagery<\/p><\/div>\n<p>The <strong><a href=\"http:\/\/www.osdpd.noaa.gov\/bTPW\/TPW_Animation.html?product=SUPER_NATIONAL_PCT\">Blended Total Precpitable Water &#8211; Percent of Normal<\/a><\/strong> product <strong><em>(below)<\/em><\/strong> indicated that this moist plume was rather anomalous for the season over the North Atlantic region, containing values of TPW that exceeded 200% of normal <em>(yellow color enhancement)<\/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\/2009\/11\/091118_tpw_percent_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"Blended Total Precipitable Water - Percent of Normal\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/11\/091118_tpw_percent_anim.gif\" alt=\"Blended Total Precipitable Water - Percent of Normal\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">Blended Total Precipitable Water - Percent of Normal<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>AWIPS images of the MIMIC Total Precipitable Water (TPW) product (above) revealed the formation of a long &#8220;atmospheric river&#8221; of moisture over the North Atlantic Ocean during the 17-19 November 2009 period. MIMIC TPW values were as high as 60 mm (darker orange color enhancement) within the moisture plume. The surface analysis (below) showed that [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[19,16,23,26],"tags":[],"class_list":["post-3838","post","type-post","status-publish","format-standard","hentry","category-goes-12","category-heavy-rain-flooding","category-meteosat","category-poes"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/3838","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=3838"}],"version-history":[{"count":22,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/3838\/revisions"}],"predecessor-version":[{"id":7012,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/3838\/revisions\/7012"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=3838"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=3838"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=3838"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}