{"id":493,"date":"2007-08-26T23:59:39","date_gmt":"2007-08-26T23:59:39","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/2007\/08\/26\/hurricane-dean-remnants-affect-california\/"},"modified":"2007-09-01T03:47:22","modified_gmt":"2007-09-01T03:47:22","slug":"hurricane-dean-remnants-affect-california","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/493","title":{"rendered":"Hurricane Dean remnants affect southern California"},"content":{"rendered":"<p><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/08\/070826_dean_wv_3h_anim.gif\" title=\"GOES-11 water vapor images (Animated GIF)\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/08\/070826_dean_wv_3h_anim.gif\" title=\"GOES-11 water vapor images (Animated GIF)\" alt=\"GOES-11 water vapor images (Animated GIF)\" align=\"middle\" height=\"361\" width=\"480\" \/><br \/>\n<\/a><\/p>\n<p>An animation of GOES-11 water vapor channel images <em><strong>(above)<\/strong><\/em> showed that Atlantic Hurricane Dean made landfall in Mexico on 22 August 2007, and eventually emerged into the Pacific basin on 23 August; the middle\/upper tropospheric moisture associated with the remnants of Dean then moved slowly northward across the Baja California region toward southern California during the next several days. AWIPS GOES-11 water vapor imagery on <a href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20070826.html\" title=\"26 August 2007 daily weather map\" target=\"_blank\"><strong>26 August 2007<\/strong><\/a> <em><strong>(below)<\/strong><\/em> indicated that a good deal of this moisture  had spread  across  much of the southern half of California  &#8212; this residual moisture (and vorticity) was responsible for helping to initiate numerous thunderstorms <em><strong>(<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/08\/070826_radar_anim.gif\" title=\"Radar (Animated GIF)\" target=\"_blank\">radar animation<\/a>)<\/strong><\/em>, some of which produced <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/08\/070826_nkx_lsr.text\" title=\"San Diego CA storm reports\" target=\"_blank\"><strong>flash flooding, record daily rainfall, and even a waterspout<\/strong><\/a> in the San Diego area.<br \/>\n<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/08\/070826_dean_wv_socal_anim.gif\" title=\"AWIPS GOES-11 water vapor images (Animated GIF)\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/08\/070826_dean_wv_socal_anim.gif\" title=\"AWIPS GOES-11 water vapor images (Animated GIF)\" alt=\"AWIPS GOES-11 water vapor images (Animated GIF)\" align=\"middle\" height=\"362\" width=\"480\" \/><\/a><\/p>\n<p>GOES sounder Total Precipitable Water (TPW) derived product imagery <em><strong>(below)<\/strong><\/em> revealed PW values as high as <strong>40-50 mm (1.6-2.0 inches)<\/strong> over southern California at 14 UTC on 26 August.<\/p>\n<p><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/08\/070826_pw_total.jpg\" title=\"GOES sounder total precipitable water\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/08\/070826_pw_total.jpg\" title=\"GOES sounder total precipitable water\" alt=\"GOES sounder total precipitable water\" align=\"middle\" height=\"363\" width=\"480\" \/><\/a><\/p>\n<p>Since the GOES sounder has 3 separate water vapor channels (<em>6.5 \u00c2\u00b5m, 7.0 \u00c2\u00b5m, and 7.4 \u00c2\u00b5m),<\/em> the TPW can be <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/rt\/viewdata.php?product=pwa_anius\" title=\"CIMSS GOES Realtime DPI site\" target=\"_blank\"><strong>partitioned into 3 vertical layers:<\/strong><\/a><strong> High Layer PW, Mid Layer PW, and Low Layer PW<\/strong> components<em><strong> (below)<\/strong>;<\/em> on this particular day, the bulk of the TPW across southern California appeared to be in the <em>middle layer<\/em>, which is generally between 700 and 900 hPa (1-3 km, or 3000-10,000 feet).<\/p>\n<p><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/08\/070826_pw_high.jpg\" title=\"GOES sounder PW (high layer)\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/08\/070826_pw_high.jpg\" title=\"GOES sounder PW (high layer)\" alt=\"GOES sounder PW (high layer)\" align=\"middle\" height=\"364\" width=\"483\" \/><\/a><\/p>\n<p><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/08\/070826_pw_mid.jpg\" title=\"GOES sounder PW (mid layer)\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/08\/070826_pw_mid.jpg\" title=\"GOES sounder PW (mid layer)\" alt=\"GOES sounder PW (mid layer)\" align=\"middle\" height=\"362\" width=\"480\" \/><\/a><\/p>\n<p><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/08\/070826_pw_low.jpg\" title=\"GOES sounder PW (low layer)\" target=\"_blank\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2007\/08\/070826_pw_low.jpg\" title=\"GOES sounder PW (low layer)\" alt=\"GOES sounder PW (low layer)\" align=\"middle\" height=\"363\" width=\"481\" \/><\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>An animation of GOES-11 water vapor channel images (above) showed that Atlantic Hurricane Dean made landfall in Mexico on 22 August 2007, and eventually emerged into the Pacific basin on 23 August; the middle\/upper tropospheric moisture associated with the remnants of Dean then moved slowly northward across the Baja California region toward southern California during [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[15,16,2],"tags":[],"class_list":["post-493","post","type-post","status-publish","format-standard","hentry","category-goes-sounder","category-heavy-rain-flooding","category-tropical-cyclones"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/493","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=493"}],"version-history":[{"count":0,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/493\/revisions"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=493"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=493"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=493"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}