{"id":37828,"date":"2020-08-02T21:59:47","date_gmt":"2020-08-02T21:59:47","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=37828"},"modified":"2020-08-04T17:54:06","modified_gmt":"2020-08-04T17:54:06","slug":"heavy-rainfall-across-interior-alaska","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/37828","title":{"rendered":"Heavy rainfall across Interior Alaska"},"content":{"rendered":"<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200802_goes17_infrared_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/ak_ir-20200802_150059.png\" alt=\"Topography + GOES-17 &quot;Clean&quot; Infrared Window (10.35 \u00b5m) images [click to play animation | MP4]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">Topography + GOES-17 &#8220;Clean&#8221; Infrared Window <em>(10.35 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200802_goes17_infrared_AK_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>An animation of Topography + GOES-17<em> (GOES-West)<\/em> &#8220;Clean&#8221; Infrared Window (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band13.pdf\"><strong>10.35 \u00b5m<\/strong><\/a>) images<em><strong> (above)<\/strong><\/em> showed a southward-moving band of clouds responsible for producing heavy rainfall across portions of Interior Alaska on 02 August 2020. Cloud-top infrared brightness temperatures were as cold as -58\u00baC <em>(brighter shades of yellow)<\/em>.<\/p>\n<p>GOES-17 &#8220;Red&#8221; Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>) images are shown below.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\" https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200802_goes17_visible_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/ak_vis-20200802_150059.png\" alt=\"GOES-17 &quot;Red&quot; Visible (0.64 \u00b5m) images [click to play animation | MP4]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">GOES-17 &#8220;Red&#8221; Visible<em> (0.64 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200802_goes17_visible_AK_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div><a href=\"http:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/Blended_TPW_Quick_Guide_20180727.pdf\"><strong>Blended Total Precipitable Water<\/strong><\/a> (TPW) and Percent of Normal TPW images during the 01-02 August time period <em><strong>(below)<\/strong><\/em> portrayed TPW values as high as 1.5 inches just north of Lake Minchumina &#8212; which was &gt;190% of the normal value for this location and time of year.<\/p>\n<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200801_200802_blendedTPW_percentNormalTPW_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/ak_btpw-20200802_183638.png\" alt=\"Blended TPW and Percent of Normal TPW images [click to play animation | MP4]\" width=\"643\" height=\"301\" \/><\/a><p class=\"wp-caption-text\">Blended TPW and Percent of Normal TPW images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200801_200802_blendedTPW_percentNormalTPW_AK_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>A sequence of VIIRS Infrared Window (11.45 \u00b5m) images from NOAA-20 and Suomi NPP as viewed using <a href=\"http:\/\/realearth.ssec.wisc.edu\"><strong>RealEarth<\/strong><\/a> <em><strong>(below)<\/strong><\/em> revealed cloud-top infrared brightness in the -60 to -65\u00baC range <em>(darker shades of red)<\/em> within this cloud band.<\/p>\n<div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200802_noaa20_suomiNPP_viirs_infrared_AK_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/08\/200802_noaa20_suomiNPP_viirs_infrared_AK_anim.gif\" alt=\"VIIRS Infrared Window (11.45 ) images from NOAA-20 and Suomi NPP [click to enlarge]\" width=\"642\" height=\"336\" \/><\/a><p class=\"wp-caption-text\">VIIRS Infrared Window <em>(11.45 \u00b5m)<\/em> images from NOAA-20 and Suomi NPP [click to enlarge]<\/p><\/div>\n<p><center><\/p>\n<blockquote class=\"twitter-tweet\">\n<p lang=\"en\" dir=\"ltr\">The deluge is winding down, but this is one for the ages: McKinley River RAWS, about 25 miles SW of Lake Minchumina, has received 4.42&quot; of rain in the past 12 hours. It&#39;s very localized, but surely this is the highest 12-hour rain ever in Interior Alaska. <a href=\"https:\/\/twitter.com\/hashtag\/akwx?src=hash&amp;ref_src=twsrc%5Etfw\">#akwx<\/a> <a href=\"https:\/\/twitter.com\/Climatologist49?ref_src=twsrc%5Etfw\">@Climatologist49<\/a> <a href=\"https:\/\/t.co\/5Xy5yhXS7g\">pic.twitter.com\/5Xy5yhXS7g<\/a><\/p>\n<p>&mdash; Rick Thoman (@AlaskaWx) <a href=\"https:\/\/twitter.com\/AlaskaWx\/status\/1290003153031577600?ref_src=twsrc%5Etfw\">August 2, 2020<\/a><\/p><\/blockquote>\n<p> <script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<blockquote class=\"twitter-tweet\">\n<p dir=\"ltr\" lang=\"en\">Rainfall totals for the 24 hours ending 6pm AKDT Sunday. Most of these are not notable for August\u2026except for that &#8220;small&#8221; area in western Denali Borough which includes probably the highest one-day <a href=\"https:\/\/twitter.com\/hashtag\/rainfall?src=hash&amp;ref_src=twsrc%5Etfw\">#rainfall<\/a> on record in Alaska north of the Alaska Range. <a href=\"https:\/\/twitter.com\/hashtag\/akwx?src=hash&amp;ref_src=twsrc%5Etfw\">#akwx<\/a> <a href=\"https:\/\/twitter.com\/Climatologist49?ref_src=twsrc%5Etfw\">@Climatologist49<\/a> <a href=\"https:\/\/t.co\/RAh3r6Jaht\">pic.twitter.com\/RAh3r6Jaht<\/a><\/p>\n<p>\u2014 Rick Thoman (@AlaskaWx) <a href=\"https:\/\/twitter.com\/AlaskaWx\/status\/1290119989685440512?ref_src=twsrc%5Etfw\">August 3, 2020<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><br \/>\n<\/center><\/p>\n","protected":false},"excerpt":{"rendered":"<p>An animation of Topography + GOES-17 (GOES-West) &#8220;Clean&#8221; Infrared Window (10.35 \u00b5m) images (above) showed a southward-moving band of clouds responsible for producing heavy rainfall across portions of Interior Alaska on 02 August 2020. Cloud-top infrared brightness temperatures were as cold as -58\u00baC (brighter shades of yellow). GOES-17 &#8220;Red&#8221; Visible (0.64 \u00b5m) images are shown [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":37852,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[80,16,79,78,53,49,48],"tags":[],"class_list":["post-37828","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-17","category-heavy-rain-flooding","category-microwave","category-noaa-20","category-real-earth","category-suomi_npp","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/37828","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=37828"}],"version-history":[{"count":4,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/37828\/revisions"}],"predecessor-version":[{"id":37851,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/37828\/revisions\/37851"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/37852"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=37828"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=37828"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=37828"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}