{"id":29838,"date":"2018-09-17T13:59:00","date_gmt":"2018-09-17T13:59:00","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=29838"},"modified":"2018-09-20T19:54:56","modified_gmt":"2018-09-20T19:54:56","slug":"florence-produces-record-rainfall-in-north-carolina-and-south-carolina","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/29838","title":{"rendered":"Florence produces record rainfall in North Carolina and South Carolina"},"content":{"rendered":"<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180913_180917_goes16_infrared_Florence_anim.mp4\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/G16_IR_PRECIP_SPC_5MIN_FLORENCE_13_16SEP2018_960x1280_B13_2018257_100212_0001PANEL_00265.GIF\" alt=\"GOES-16 \" width=\"642\" height=\"481\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Clean&#8221; Infrared Window <em>(10.3 \u00b5m)<\/em> images, with hourly precipitation type symbols plotted in yellow and SPC storm reports plotted in cyan, 13-17 September [click to play MP4 animation]<\/p><\/div>After <a href=\"https:\/\/www.nhc.noaa.gov\/archive\/2018\/FLORENCE.shtml?\"><strong>Hurricane Florence<\/strong><\/a> made landfall in North Carolina during the morning hours on <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/29801\"><strong>14 September<\/strong><\/a>, it moved very slowly (at times only 2-3 mph) southwestward into South Carolina during 15-16 September (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180913_180916_surface_analyses_Florence_anim.gif\"><strong>surface analyses<\/strong><\/a>). Prolonged heavy rainfall resulted (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180917_wpc_storm_summary.text\"><strong>WPC summary<\/strong><\/a>), with new state records <em>(see below)<\/em> for precipitation from a tropical cyclone being set in North Carolina (35.93 inches) and South Carolina (23.63 inches). GOES-16<em> (GOES-East)<\/em> &#8220;Clean&#8221; Infrared Window (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band13.pdf\"><strong>10.3 \u00b5m<\/strong><\/a>) images every 5 minutes during the 4-day period of 13-16 September <em><strong>(above)<\/strong><\/em> showed the evolution of banding and the development of new convection that produced the heavy rainfall &#8212; widespread flooding along with strong winds caused power outages across portions of the 2 states (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180913_180916_NC_power_outages_anim.gif\"><strong>NC<\/strong><\/a> | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180914_180916_SC_power_outages_anim.gif\"><strong>SC<\/strong><\/a>), and closed sections of Interstates 95 and 40. Note that the power outages caused extended dropouts of the plotted surface reports &#8212; especially in eastern North Carolina; reports were missing when the gray 4-letter station identifiers disappeared &#8212; even though many of those sites were likely experiencing heavy rainfall during those dropout times.<\/p>\n<p>Florence also spawned a few tornadoes on <strong><a href=\"https:\/\/www.spc.noaa.gov\/climo\/reports\/180914_rpts.html\">14<\/a><\/strong>, <strong><a href=\"https:\/\/www.spc.noaa.gov\/climo\/reports\/180915_rpts.html\">15<\/a><\/strong> and <strong><a href=\"https:\/\/www.spc.noaa.gov\/climo\/reports\/180916_rpts.html\">16 September<\/a><\/strong> &#8212; SPC storm reports are plotted in cyan on the GOES-16 Infrared images.<\/p>\n<p>Hourly images of the <a href=\"http:\/\/tropic.ssec.wisc.edu\/real-time\/mtpw2\/product.php?color_type=tpw_nrl_colors&amp;prod=conus&amp;timespan=24hrs&amp;anim=html5\"><strong>MIMIC Total Precipitable Water<\/strong><\/a> product <em><strong>(below)<\/strong><\/em> showed tropical moisture associated with Florence as it moved inland during the 13-17 September period.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180913_180917_mimic_tpw_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/comp20180914.120000_tpw.png\" alt=\"MIMIC Total Precipitable Water product [click to play animation | MP4]\" width=\"640\" height=\"301\" \/><\/a><p class=\"wp-caption-text\">MIMIC Total Precipitable Water product, 13-17 September [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180913_180917_mimic_tpw_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Animations of plots of rawinsonde data from the coastal sites of Newport\/Morehead City, North Carolina and Charleston, South Carolina <em><strong>(below)<\/strong><\/em> revealed the increase in deep tropical moisture from 13-16 September &#8212; Total Precipitable Water values were as high as 68.6 mm <em>(2.70 inches)<\/em> at Newport and 67.8 mm <em>(2.67 inches)<\/em> at Charleston.<\/p>\n<p><div style=\"width: 649px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180913_180917_kmhx_raobs_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180913_180917_kmhx_raobs_anim.gif\" alt=\"Daily plots of rawinsonde data from Newport\/Morehead City, North Carolina [click to enlarge]\" width=\"639\" height=\"425\" \/><\/a><p class=\"wp-caption-text\">Daily plots of rawinsonde data from Newport\/Morehead City, North Carolina [click to enlarge]<\/p><\/div><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180913_180917_kchs_raobs_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180913_180917_kchs_raobs_anim.gif\" alt=\"Daily plots of rawinsonde data from Charleston, South Carolina [click to enlarge]\" width=\"641\" height=\"426\" \/><\/a><p class=\"wp-caption-text\">Daily plots of rawinsonde data from Charleston, South Carolina [click to enlarge]<\/p><\/div>As the remnants of Florence moved from Kentucky to West Virginia during the daylight hours of 17 September, numerous tornadoes occurred in central Virginia (<a href=\"https:\/\/www.spc.noaa.gov\/climo\/reports\/180917_rpts.html\"><strong>SPC storm reports<\/strong><\/a> | <a href=\"https:\/\/www.weather.gov\/akq\/Sep172018_Tornadoes\"><strong>NWS Wakefield summary<\/strong><\/a>). 1-minute GOES-16 &#8220;Red&#8221; Visible (0.64 \u00b5m) and &#8220;Clean&#8221; Infrared Window (10.3 \u00b5m) images <em><strong>(below)<\/strong><\/em> showed the development of thunderstorms which produced these tornadoes.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180917_goes16_visible_infrared_spc_storm_reports_VA_anim.mp4\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/G16_VIS_IR_VA_SVR_17SEP2018_960x640_B213_2018260_195321_0002PANELS_00353.GIF\" alt=\"GOES-16 &quot;Red&quot; Visible (0.64 \u00b5m, left) and &quot;Clean&quot; Infrared Window (10.3 \u00b5m, right) images, with plots of SPC storm reports [click to play MP4 animation]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible <em>(0.64 \u00b5m, left)<\/em> and &#8220;Clean&#8221; Infrared Window <em>(10.3 \u00b5m, right)<\/em> images, with plots of SPC storm reports [click to play MP4 animation]<\/p><\/div><center><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p dir=\"ltr\" lang=\"en\">Today, it&#8217;s two updates. After some chatter with the <a href=\"https:\/\/twitter.com\/CoCoRaHS?ref_src=twsrc%5Etfw\">@CoCoRaHS<\/a> observer, we&#8217;ve accepted the reading. There was uncertainty in house about the reading. Just trying to be careful. <a href=\"https:\/\/t.co\/7bF76eeGLQ\">pic.twitter.com\/7bF76eeGLQ<\/a><\/p>\n<p>\u2014 David Roth (@DRmetwatch) <a href=\"https:\/\/twitter.com\/DRmetwatch\/status\/1041805078909411328?ref_src=twsrc%5Etfw\">September 17, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\" data-lang=\"en\">\n<p dir=\"ltr\" lang=\"en\">Radar loops have been finalized for <a href=\"https:\/\/twitter.com\/hashtag\/Florence?src=hash&amp;ref_src=twsrc%5Etfw\">#Florence<\/a>, and include a 24-hour loop for landfall and a 104-hour loop to cover its slow trek through <a href=\"https:\/\/twitter.com\/hashtag\/NorthCarolina?src=hash&amp;ref_src=twsrc%5Etfw\">#NorthCarolina<\/a> and <a href=\"https:\/\/twitter.com\/hashtag\/SouthCarolina?src=hash&amp;ref_src=twsrc%5Etfw\">#SouthCarolina<\/a>. Please visit <a href=\"https:\/\/t.co\/vWICHS7kHl\">https:\/\/t.co\/vWICHS7kHl<\/a> <a href=\"https:\/\/twitter.com\/UMiamiRSMAS?ref_src=twsrc%5Etfw\">@UMiamiRSMAS<\/a> <a href=\"https:\/\/t.co\/8jixg0mR1C\">pic.twitter.com\/8jixg0mR1C<\/a><\/p>\n<p>\u2014 Brian McNoldy (@BMcNoldy) <a href=\"https:\/\/twitter.com\/BMcNoldy\/status\/1041702038835539968?ref_src=twsrc%5Etfw\">September 17, 2018<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<p>&nbsp;<\/p>\n<p><\/center><\/p>\n<p style=\"text-align: center;\"><strong>===== 18 September Update =====<\/strong><\/p>\n<p><div style=\"width: 648px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180826_180918_terra_modis_falsecolor_NC_Florence_flooding_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180826_180918_terra_modis_falsecolor_NC_Florence_flooding_anim.gif\" alt=\"Before\/after (26 August\/18 September) Terra MODIS False Color RGB images [click to enlarge]\" width=\"638\" height=\"399\" \/><\/a><p class=\"wp-caption-text\">Terra MODIS False Color RGB images, <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180826_terra_modis_fc_NC.jpeg\"><strong>26 August<\/strong><\/a> vs. <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180918_terra_modis_fc_NC.jpeg\"><strong>18 September<\/strong><\/a> [click to enlarge]<\/p><\/div>A comparison of before\/after (26 August\/18 September) Terra MODIS False Color Red-Green-Blue (RGB) images from the <a href=\"http:\/\/ge.ssec.wisc.edu\/modis-today\/index.php?satellite=t1&amp;product=false_color&amp;date=2018_09_18_261&amp;overlay_sector=false&amp;overlay_state=true&amp;overlay_coastline=true\"><strong>MODIS Today<\/strong><\/a> site <em><strong>(above)<\/strong><\/em> showed areas of inland flooding<em> (increasing water coverage appears as darker shades of blue)<\/em> in the wake of Florence across far southeastern North Carolina and far northeastern South Carolina.<\/p>\n<p>Looking slightly to the south, a similar before\/after comparison of Terra MODIS True Color RGB images<em><strong> (below)<\/strong><\/em> revealed areas of sediment runoff into the Atlantic Ocean.<\/p>\n<div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180826_180918_terra_modis_truecolor_NC_Florence_sediment_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180826_180918_terra_modis_truecolor_NC_Florence_sediment_anim.gif\" alt=\"Terra MODIS True Color RGB images, 26 August vs. 18 September [click to enlarge]\" width=\"641\" height=\"401\" \/><\/a><p class=\"wp-caption-text\">Terra MODIS True Color RGB images, <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180826_terra_modis_tc_NC_sediment.jpeg\"><strong>26 August<\/strong><\/a> vs. <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/09\/180918_terra_modis_tc_NC_sediment.jpeg\"><strong>18 September<\/strong><\/a> [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>After Hurricane Florence made landfall in North Carolina during the morning hours on 14 September, it moved very slowly (at times only 2-3 mph) southwestward into South Carolina during 15-16 September (surface analyses). Prolonged heavy rainfall resulted (WPC summary), with new state records (see below) for precipitation from a tropical cyclone being set in North [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":29841,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[74,16,79,12,45,3,71,2],"tags":[],"class_list":["post-29838","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-16","category-heavy-rain-flooding","category-microwave","category-modis","category-redgreenblue-rgb-images","category-severe-convection","category-terra","category-tropical-cyclones"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/29838","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=29838"}],"version-history":[{"count":28,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/29838\/revisions"}],"predecessor-version":[{"id":29885,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/29838\/revisions\/29885"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/29841"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=29838"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=29838"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=29838"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}