{"id":43694,"date":"2021-12-07T23:59:00","date_gmt":"2021-12-07T23:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=43694"},"modified":"2022-12-10T00:22:49","modified_gmt":"2022-12-10T00:22:49","slug":"kona-low-produces-record-rainfall-and-flooding-in-hawaii","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/43694","title":{"rendered":"Kona low produces record rainfall and flooding in Hawai`i"},"content":{"rendered":"<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211204_211207_mimicTPW_HI_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211208_00z_tpw.png\" alt=\"\" width=\"640\" height=\"310\" \/><\/a><p class=\"wp-caption-text\">MIMIC Total Precipitable Water product [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211204_211207_mimicTPW_HI_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p>As an <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211204_211207_500hPa_height_anomaly_anim.gif\"><strong>anomalously-deep<\/strong><\/a> Kona low moved northwest of and then west of Hawai`i during the 04-07 December 2021 period, it began to tap moisture from the Pacific ITCZ and channel it northward across the islands &#8212; setting the stage for a <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211207_hfo_pns.text\"><strong>prolonged heavy rainfall event<\/strong><\/a> (which produced the <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211207_hfo_rer.text\"><strong>wettest December day on record at Honolulu<\/strong><\/a>). Hourly <a href=\"http:\/\/tropic.ssec.wisc.edu\/real-time\/mtpw2\/product.php?color_type=tpw_nrl_colors&amp;prod=global2&amp;timespan=48hrs&amp;anim=html5\"><strong>MIMIC TPW<\/strong><\/a> images viewed using <a href=\"http:\/\/realearth.ssec.wisc.edu\"><strong>RealEarth<\/strong><\/a> <em><strong>(above)<\/strong><\/em> showed the convergence of 2 northward-moving streams of ITCZ moisture, that then flowed across various portions of Hawai&#8217;i (located at the center of the images) from 00 UTC on 04 December to 00 UTC on 08 December.<\/p>\n<p><a href=\"https:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/QuickGuide_GOESR_AirMassRGB_final.pdf\"><strong>Air Mass RGB<\/strong><\/a> images created using <a href=\"https:\/\/www.ssec.wisc.edu\/software\/geo2grid\/\"><strong>Geo2Grid<\/strong><\/a> <em><strong>(below)<\/strong><\/em> highlighted the southwestward migration of the <a href=\"https:\/\/www.soest.hawaii.edu\/MET\/Faculty\/businger\/poster\/KonaLow\/\"><strong>Kona low<\/strong><\/a> (darker shades of red) as well as the northward motion of deep convection within the stream of ITCZ moisture.<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211204_211207_goes17_airMassRGB_HI_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/GOES-17_ABI_RadF_airmass_2021340_120032Z.png\" alt=\"\" width=\"640\" height=\"640\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Air Mass RGB images [click to play animated GIF | <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211204_211207_goes17_airMassRGB_HI_anim.mp4\">MP4<\/a><\/strong>]<\/p><\/div>\n<p>In addition to the heavy rainfall across many of the islands, the high-elevation summits of Mauna Kea and Mauna Loa on the Big Island of Hawai`i also received accumulating snowfall &#8212; a signature of this snow cover (darker shades of magenta) was evident in GOES-17 <a href=\"https:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/QuickGuide_DaySnowFogRGB_final_v2.pdf\"><strong>Day Snow-Fog RGB<\/strong><\/a> images shown below.<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211207_goes17_daySnowFogRGB_HI_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/hi_dsf-20211207_230117.png\" width=\"640\" height=\"310\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Day Snow-Fog RGB images [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211207_goes17_daySnowFogRGB_HI_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n\n\n<p><\/p>\n","protected":false},"excerpt":{"rendered":"<p>As an anomalously-deep Kona low moved northwest of and then west of Hawai`i during the 04-07 December 2021 period, it began to tap moisture from the Pacific ITCZ and channel it northward across the islands &#8212; setting the stage for a prolonged heavy rainfall event (which produced the wettest December day on record at Honolulu). [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":43736,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[132,80,16,79,53,45,5],"tags":[],"class_list":["post-43694","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-geo2grid","category-goes-17","category-heavy-rain-flooding","category-microwave","category-real-earth","category-redgreenblue-rgb-images","category-winter-weather"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/43694","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=43694"}],"version-history":[{"count":23,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/43694\/revisions"}],"predecessor-version":[{"id":49156,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/43694\/revisions\/49156"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/43736"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=43694"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=43694"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=43694"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}