{"id":410,"date":"2007-05-17T22:40:50","date_gmt":"2007-05-17T22:40:50","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/2007\/05\/17\/occluding-cyclone-in-the-gulf-of-alaska\/"},"modified":"2007-06-02T04:44:13","modified_gmt":"2007-06-02T04:44:13","slug":"occluding-cyclone-in-the-gulf-of-alaska","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/410","title":{"rendered":"Occluding cyclone in the Gulf of Alaska"},"content":{"rendered":"<p><a title=\"GOES-11 water vapor image\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/070517_G11_WV_74.GIF\"><img loading=\"lazy\" decoding=\"async\" width=\"480\" height=\"361\" align=\"middle\" alt=\"GOES-11 water vapor image\" title=\"GOES-11 water vapor image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/070517_G11_WV_74.GIF\" \/><br \/>\n<\/a><\/p>\n<p>GOES-11 6.7\u00c2\u00b5m &#8220;water vapor channel&#8221; imagery <em><strong>(above; <a title=\"GOES-11 water vapor images (QuickTime animation)\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/070517_g11_wv.mov\">QuickTime animation<\/a>)<\/strong><\/em> revealed a textbook signature of an occluding cyclone over the Gulf of Alaska on <a title=\"17 May 2007 daily weather map\" target=\"_blank\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20070517.html\"><strong>17 May 2007<\/strong><\/a>. A <a title=\"dry slot\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/070517_G11_WV_20A.GIF\"><strong>dry slot<\/strong><\/a> begins to interact with a <a title=\"baroclinic leaf\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/070517_G11_WV_20A.GIF\"><strong>baroclinic leaf<\/strong><\/a>  feature after 00:00 UTC, with a distinct <a title=\"comma head\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/070517_G11_WV_34A.GIF\"><strong>cloud head or &#8220;comma head&#8221;<\/strong><\/a> forming after 06:00 UTC. After 12:00 UTC, the characteristic <a title=\"dry swirl\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/070517_G11_WV_84A.GIF\"><strong>&#8220;dry swirl&#8221;<\/strong><\/a> pattern is evident on the water vapor imagery, indicating that the cyclone was entering the occluded phase of its life cycle.<\/p>\n<p>A classic hook-shaped pattern was also seen on AWIPS imagery of the DMSP SSM\/I rainfall rate product <em><strong>(below)<\/strong><\/em>, although rainfall rates were fairly light (in the 1-2 mm per hour range).  <a target=\"_blank\" title=\"NOAA Ocean Prediction Center\" href=\"http:\/\/www.opc.ncep.noaa.gov\/index.shtml\"><strong>NOAA Ocean Prediction Center<\/strong><\/a> guidance was forecasting <a target=\"_blank\" title=\"NOAA OPC gale force winds\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/N_Atl_Sfc_Anal_20070517_1200.png\"><strong>gale<\/strong><\/a> and <a target=\"_blank\" title=\"NOAA OPC storm force winds\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/N_Atl_Sfc_Anal_20070517_1800.png\"><strong>storm<\/strong><\/a> force winds in the northwestern quadrant of the occluding cyclone.<\/p>\n<p><a title=\"DMSP SSM\/I rainfall rate\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/DMSP_RR_20070517_2106.png\"><img loading=\"lazy\" decoding=\"async\" width=\"479\" height=\"360\" align=\"middle\" title=\"DMSP SSM\/I rainfall rate\" alt=\"DMSP SSM\/I rainfall rate\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/DMSP_RR_20070517_2106.png\" \/><\/a><\/p>\n<p>==================================================<\/p>\n<p><a title=\"GFS90 model cross section (PV)\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/GFS90_lineG__Pot_Vorticity_Img_20070517_1800F006.png\"><img loading=\"lazy\" decoding=\"async\" width=\"480\" height=\"363\" align=\"middle\" title=\"GFS90 model cross section (PV)\" alt=\"GFS90 model cross section (PV)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/GFS90_lineG__Pot_Vorticity_Img_20070517_1800F006.png\" \/><\/a><\/p>\n<p>A <a title=\"cross section\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/NA_Water_Vapor_20070517_1745.png\"><strong>cross section<\/strong><\/a> oriented west to east through the cyclone at 18:00 UTC using AWIPS GFS90 model fields indicated that the dynamic tropopause <em>(taken to be 1.5 Potential Vorticity Units, purple to blue enhancement, <strong>above<\/strong>)<\/em> was fairly low across the region of the cyclone (below the 500 hPa pressure level), with a hint of stratospheric air (greater than 1.5 PVU) extending downward to near the surface. A corresponding cross section of Relative Humidity <em><strong>(below)<\/strong><\/em> showed the very dry air <em>(RH values less than 20%, orange to red enhancement)<\/em> associated with the elevated dry slot that was wrapping around the cyclone.<\/p>\n<p><a title=\"GFS90 model cross section (RH)\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/GFS90_lineG__Rel_Humidity_Img_20070517_1800F006.png\"><img loading=\"lazy\" decoding=\"async\" width=\"479\" height=\"360\" align=\"middle\" title=\"GFS90 model cross section (RH)\" alt=\"GFS90 model cross section (RH)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/05\/GFS90_lineG__Rel_Humidity_Img_20070517_1800F006.png\" \/><\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>GOES-11 6.7\u00c2\u00b5m &#8220;water vapor channel&#8221; imagery (above; QuickTime animation) revealed a textbook signature of an occluding cyclone over the Gulf of Alaska on 17 May 2007. A dry slot begins to interact with a baroclinic leaf feature after 00:00 UTC, with a distinct cloud head or &#8220;comma head&#8221; forming after 06:00 UTC. After 12:00 UTC, [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[10,18,8,26],"tags":[],"class_list":["post-410","post","type-post","status-publish","format-standard","hentry","category-general-interpretation","category-goes-11","category-marine-weather","category-poes"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/410","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=410"}],"version-history":[{"count":0,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/410\/revisions"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=410"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=410"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=410"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}