{"id":2802,"date":"2009-06-25T18:06:01","date_gmt":"2009-06-25T18:06:01","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=2802"},"modified":"2009-06-26T17:34:25","modified_gmt":"2009-06-26T17:34:25","slug":"stratospheric-instrusion-vortex-off-the-us-east-coast","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/2802","title":{"rendered":"&#8220;Stratospheric instrusion vortex&#8221; off the US East Coast"},"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\/06\/090625_g12_wv_anim.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"GOES-12 water vapor images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/06\/090625_g12_wv_anim.gif\" title=\"GOES-12 water vapor images\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">GOES-12 water vapor images<\/p><\/div>\n<p>A small &#8220;dry swirl&#8221; feature <em>(yellow color enhancement)<\/em> was seen on AWIPS images of the GOES-12 6.5 \u00c2\u00b5m water vapor channel  <strong><em>(above)<\/em><\/strong> off the East Coast of the US on <strong><a href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20090624.html\">24 June<\/a> &#8211; <a href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20090625.html\">25 June 2009<\/a><\/strong>. <\/p>\n<p>A comparison of a GOES-12 water vapor image with the corresponding GOES-12 sounder Total Column Ozone product at 21:00 UTC on 24 June <strong><em>(below)<\/em><\/strong> confirmed that this was a small-scale &#8220;stratospheric intrusion vortex&#8221;, with ozone values greater than 370 Dobson Units <em>(lighter green color enhancement)<\/em> in the vicinity of the dry feature on the water vapor imagery.<\/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\/06\/090624_g12_wv_ozone_anim.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"GOES-12 water vapor + GOES-12 sounder Total Column Ozone product\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/06\/090624_g12_wv_ozone_anim.gif\" title=\"GOES-12 water vapor + GOES-12 sounder Total Column Ozone product\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">GOES-12 water vapor + GOES-12 sounder Total Column Ozone product<\/p><\/div>\n<p>An overlay of GFS40 model fields on GOES-12 water vapor and Total Column Ozone images <strong><em>(below)<\/em><\/strong> indicated that the dynamic tropopause <em>(taken to be the pressure of the PV1.5 potential vorticity surface)<\/em> was as low as the 400 hPa level at 12:00 UTC on 25 June.<\/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\/06\/090625_g12_wv_ozone_anim.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"GOES-12 water vapor image + GOES-12 sounder Total Column Ozone product\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/06\/090625_g12_wv_ozone_anim.gif\" title=\"GOES-12 water vapor image + GOES-12 sounder Total Column Ozone product\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">GOES-12 water vapor image + GOES-12 sounder Total Column Ozone product<\/p><\/div>\n<p>A more detailed view of the vortex could be seen using 1-km resolution MODIS 6.7 \u00c2\u00b5m water vapor images <strong><em>(below)<\/em><\/strong>.<\/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\/06\/090624-25_modis_wv_anim.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"MODIS water vapor images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/06\/090624-25_modis_wv_anim.gif\" title=\"MODIS water vapor images\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">MODIS water vapor images<\/p><\/div>\n<p>A comparison of MODIS water vapor, IR window, and visible images <strong><em>(below)<\/em><\/strong> showed that there was a lack of high clouds with this stratospheric intrusion vortex &#8212; only low-level clouds existed over the region in the vicinity of the vortex.<\/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\/06\/090625_modis_wv_ir_vis_anim.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"MODIS water vapor + IR + visible images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/06\/090625_modis_wv_ir_vis_anim.gif\" title=\"MODIS water vapor + IR + visible images\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">MODIS water vapor + IR + visible images<\/p><\/div>\n<p>A comparison of a MODIS water vapor image with 1-hour MADIS satellite winds and GFS40 400 hPa height <strong><em>(below)<\/em><\/strong> showed that the stratospheric intrusion vortex was located just to the northeast of the closed low that was off the US East Coast during the period.<\/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\/06\/GFS40_400MB_Height_20090625_0600F000.png\"><img loading=\"lazy\" decoding=\"async\" alt=\"MODIS water vapor image + satellite winds + GFS 400 hPa height\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/06\/GFS40_400MB_Height_20090625_0600F000.png\" title=\"MODIS water vapor image + satellite winds + GFS 400 hPa height\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">MODIS water vapor image + satellite winds + GFS 400 hPa height<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>A small &#8220;dry swirl&#8221; feature (yellow color enhancement) was seen on AWIPS images of the GOES-12 6.5 \u00c2\u00b5m water vapor channel (above) off the East Coast of the US on 24 June &#8211; 25 June 2009. A comparison of a GOES-12 water vapor image with the corresponding GOES-12 sounder Total Column Ozone product at 21:00 [&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":[15,19,12,25],"tags":[],"class_list":["post-2802","post","type-post","status-publish","format-standard","hentry","category-goes-sounder","category-goes-12","category-modis","category-satellite-winds"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/2802","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=2802"}],"version-history":[{"count":5,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/2802\/revisions"}],"predecessor-version":[{"id":2823,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/2802\/revisions\/2823"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=2802"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=2802"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=2802"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}