{"id":12840,"date":"2013-05-07T23:59:22","date_gmt":"2013-05-07T23:59:22","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=12840"},"modified":"2013-05-08T17:42:47","modified_gmt":"2013-05-08T17:42:47","slug":"thunderstorms-producing-heavy-rain-and-flash-flooding-in-puerto-rico","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/12840","title":{"rendered":"Thunderstorms producing heavy rain and flash flooding in Puerto Rico"},"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\/2013\/05\/130507_g13_ir_rso_PR_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"GOES-13 10.7 \u00c2\u00b5m IR channel images (click image to play animation)\" alt=\"GOES-13 10.7 \u00c2\u00b5m IR channel images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/05\/130507_G13_IR_PR_15.GIF\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-13 10.7 \u00c2\u00b5m IR channel images (click image to play animation)<\/p><\/div>\n<p>McIDAS images of 4-km resolution GOES-13 10.7 \u00c2\u00b5m IR channel images <strong><em>(above; click image to play animation)<\/em><\/strong> showed the development of large thunderstorms that produced heavy rainfall <em>(including 5.18 inches at San Sebastian)<\/em> which led to flash flooding over parts of Puerto Rico (<strong><a title=\"Local Storm Report\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/05\/130507_tjsj_lsr.text\">Local Storm Report<\/a><\/strong>) on <strong><a title=\"07 May 2013 (18 UTC surface analysis)\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/05\/130507_18z_caribbean_surface_analysis.gif\">07 May 2013<\/a><\/strong>. Since their primary Doppler radar was out of service due to an upgrade to <strong><a title=\"Dual-Polarization\" href=\"http:\/\/www.wdtb.noaa.gov\/courses\/dualpol\/outreach\/\">Dual-Polarization<\/a><\/strong> technology, the National Weather Service forecast office at <strong><a title=\"San Juan NWS forecast office\" href=\"http:\/\/www.srh.noaa.gov\/sju\/\">San Juan<\/a><\/strong> had requested that the GOES-13 <em>(GOES-East)<\/em> satellite be placed into Rapid Scan Operations (RSO), which provided images as frequently as every 5-10 minutes (instead of the nominal 15-minute image interval). The coldest cloud top IR brightness temperature seen on the GOES-13 IR image sequence above was <strong>-69\u00c2\u00ba C<\/strong> at 17:10 UTC.<\/p>\n<p>Due to a full-disk scan at 18:00 UTC, there was a 30-minute gap between the <strong><a title=\"17:45 UTC GOES-13 IR image\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/05\/130507_G13_IR_PR_20.GIF\">17:45 UTC<\/a><\/strong> and <strong><a title=\"18:15 UTC GOES-13 IR image\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/05\/130507_G13_IR_PR_21.GIF\">18:15 UTC<\/a><\/strong> GOES-13 images. A timely overpass of the NOAA-19 polar-orbiting satellite at 18:03 UTC provided a 1-km resolution AVHRR 10.8 \u00c2\u00b5m IR image during this 30-minute GOES-13 gap <strong><em>(below),<\/em><\/strong> which revealed that a new convective cell had rapidly developed over the northwestern portion of Puerto Rico <em>(exhibiting a cloud-top IR brightness temperature as cold as <strong>-79\u00c2\u00ba C<\/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\/2013\/05\/130507_N19_AVHRR_CH04_PR.GIF\"><img loading=\"lazy\" decoding=\"async\" alt=\"NOAA-19 AVHRR 10.8 \u00c2\u00b5m IR channel image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/05\/130507_N19_AVHRR_CH04_PR.GIF\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">NOAA-19 AVHRR 10.8 \u00c2\u00b5m IR channel image<\/p><\/div>\n<p>AWIPS images of the <a title=\"MIMIC Total Precipitable Water product\" href=\"http:\/\/tropic.ssec.wisc.edu\/real-time\/mimic-tpw\/global2\/main.html\"><strong>MIMIC Total Precipitable Water<\/strong><\/a> (TPW) product <em><strong>(below; click image to play animation)<\/strong><\/em> showed that an elongated plume of high TPW <em>(50 to 60 mm or 2.0 to 2.4 inches, darker orange color enhancement)<\/em> was rotating across the Puerto Rico region during this period, providing ample moisture to fuel the development of deep convection and heavy rainfall. <a title=\"MIMIC TPW product with surface analyses\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/05\/130507_mimic_tpw_surface_analysis_PR_anim.gif\"><strong>Surface analyses<\/strong><\/a> suggest that the eastern portion of the TPW\u00c2\u00a0 plume was associated with the remnants of a cold frontal boundary, while an impulse over the Caribbean Sea was helping to transport higher TPW values from the south (TJSJ is the station identifier for San Juan, Puerto Rico).<\/p>\n<div style=\"width: 489px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/05\/130506-07_mimic_tpw_PR_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"MIMIC Total Precipitable Water product (click image to play animation)\" alt=\"MIMIC Total Precipitable Water product (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/05\/MIMIC_TPW_20130507_1800.png\" width=\"479\" height=\"292\" \/><\/a><p class=\"wp-caption-text\">MIMIC Total Precipitable Water product (click image to play animation)<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>McIDAS images of 4-km resolution GOES-13 10.7 \u00c2\u00b5m IR channel images (above; click image to play animation) showed the development of large thunderstorms that produced heavy rainfall (including 5.18 inches at San Sebastian) which led to flash flooding over parts of Puerto Rico (Local Storm Report) on 07 May 2013. Since their primary Doppler radar [&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":[22,11,16,26],"tags":[],"class_list":["post-12840","post","type-post","status-publish","format-standard","hentry","category-avhrr","category-goes-13","category-heavy-rain-flooding","category-poes"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/12840","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=12840"}],"version-history":[{"count":18,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/12840\/revisions"}],"predecessor-version":[{"id":12858,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/12840\/revisions\/12858"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=12840"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=12840"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=12840"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}