{"id":38784,"date":"2020-10-30T23:59:47","date_gmt":"2020-10-30T23:59:47","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=38784"},"modified":"2020-11-01T20:56:11","modified_gmt":"2020-11-01T20:56:11","slug":"super-typhoon-goni-in-the-west-pacific-ocean","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/38784","title":{"rendered":"Super Typhoon Goni in the West Pacific Ocean"},"content":{"rendered":"<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201030_himawari8_visible_Typhoon_Goni_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/HIM08_VIS_GONI_30OCT2020_B3_2020305_014215_HIMAWARI-8_0001PANEL_FRAME00100.GIF\" alt=\"JMA Himawari-8 \" width=\"643\" height=\"483\" \/><\/a><p class=\"wp-caption-text\">JMA Himawari-8 &#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\/10\/201030_himawari8_visible_Typhoon_Goni_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>2.5-minute rapid scan <a href=\"https:\/\/www.jma.go.jp\/jma\/indexe.html\"><strong>JMA<\/strong><\/a> Himawari-8 &#8220;Red&#8221; Visible (0.64 \u00b5m) images <em><strong>(above)<\/strong><\/em> showed Category 5 Super Typhoon Goni in the West Pacific Ocean on 30 October 2020. The images revealed a very small &#8220;pinhole eye&#8221;, surface mesovortices within the eye and a trochoidal motion &#8212; all characteristics of a tropical cyclone at\/near its peak intensity (Goni had a satellite-derived estimate of 160 knots at 00 UTC). The trochoidal &#8220;wobble&#8221; was more evident in a <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201030_himawari8_visible_Typhoon_Goni_fast_anim.gif\"><strong>faster animation<\/strong><\/a>.<\/p>\n<p>The corresponding Infrared (10.4 \u00b5m) images<em><strong> (below)<\/strong><\/em> revealed cloud-top infrared brightness temperatures that were frequently in the -80 to -85\u00baC range <em>(shades of violet)<\/em>.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201030_himawari8_infrared_Typhoon_Goni_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/HIM08_IR_GONI_30OCT2020_B13_2020305_014215_HIMAWARI-8_0001PANEL_FRAME00100.GIF\" alt=\"JMA Himawari-8 &quot;Clean&quot; Infrared Window (10.4 \u00b5m) images [click to play animation | MP4]\" width=\"641\" height=\"481\" \/><\/a><p class=\"wp-caption-text\">JMA Himawari-8 &#8220;Clean&#8221; Infrared Window<em> (10.4 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201030_himawari8_infrared_Typhoon_Goni_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Longwave Infrared (11.2 \u00b5m) images with contours of 00 UTC <a href=\"http:\/\/tropic.ssec.wisc.edu\/misc\/winds\/info.winds.shr.html\"><strong>deep-layer wind shear<\/strong><\/a> from the <a href=\"http:\/\/tropic.ssec.wisc.edu\"><strong>CIMSS Tropical Cyclones<\/strong><\/a> site <em><strong>(above)<\/strong><\/em> indicated Goni was in an environment of very low shear at that time.<\/p>\n<div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201030_himawari8_infrared_shear_Goni_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201030_himawari8_infrared_shear_Goni_anim.gif\" alt=\"Himawari-8 Longwave Infrared (11.2 \u00b5m) images, with contours of 0i0 UTC deep-layer wind shear [click to enlarge]\" width=\"641\" height=\"429\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 Longwave Infrared <em>(11.2 \u00b5m)<\/em> images, with contours of 00 UTC deep-layer wind shear [click to enlarge]<\/p><\/div>\n<p style=\"text-align: center;\"><strong>===== 31 October Update =====<\/strong><\/p>\n<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201031_himawari8_infrared_SuperTyphoon_Goni_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/HIM08_IR_GONI_31OCT2020_B13_2020305_194441_HIMAWARI-8_0001PANEL_FRAME00066.GIF\" alt=\"JMA Himawari-8 &quot;Clean&quot; Infrared Window (10.4 \u00b5m) images [click to play animation | MP4]\" width=\"642\" height=\"482\" \/><\/a><p class=\"wp-caption-text\">JMA Himawari-8 &#8220;Clean&#8221; Infrared Window<em> (10.4 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201031_himawari8_infrared_SuperTyphoon_Goni_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Super Typhoon Goni maintained Category 5 intensity for over 24 hours, and actually intensified to 170 knots (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201031_18utc_Goni_advisory.text\"><strong>JTWC advisory<\/strong><\/a> | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201031_adt_Goni.gif\"><strong>ADT<\/strong><\/a> | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201031_satcon_Goni.gif\"><strong>SATCON<\/strong><\/a>) at 18 UTC on 31 October, just prior to making landfall along Catanduanes Island in the Philippines around 2050 UTC (a closer view of landfall using <a href=\"http:\/\/realearth.ssec.wisc.edu\"><strong>RealEarth<\/strong><\/a> is available <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201031_himawari8_Goni_landfall_anim.gif\"><strong>here<\/strong><\/a>).\u00a0At 170 knots, Goni became one of the most intense landfalling tropical cyclones on record.<\/p>\n<p>Note the rapid deterioration of the eye upon landfall &#8212; this was likely due to a combination of interaction with the terrain of the island, and increasing deep-layer wind shear <em><strong>(below)<\/strong><\/em>. As it was approaching the Philippines, Goni had been moving over very warm water characterized by high values of <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201031_seaSurfaceTemperature_oceanHeatContent_Typhoon_Goni_anim.gif\"><strong>Sea Surface Temperature and Ocean Heat Content<\/strong><\/a>.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201031_himawari8_waterVapor_shear_Goni_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201031_himawari8_waterVapor_shear_Goni_anim.gif\" alt=\"Himawari-8 Water Vapor images, with contours of deep-layer wind shear [click to enlarge]\" width=\"641\" height=\"320\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 Water Vapor images, with contours of deep-layer wind shear [click to enlarge]<\/p><\/div>A DMSP-16 SSMIS Microwave (85 GHz) image at 2032 UTC is shown below.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201031_2032utc_dmsp16_ssmis_microwave_Goni.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201031_2032utc_dmsp16_ssmis_microwave_Goni.gif\" alt=\"DMSP-16 SSMIS Microwave image at 2032 UTC [click to enlarge]\" width=\"640\" height=\"422\" \/><\/a><p class=\"wp-caption-text\">DMSP-16 SSMIS Microwave <em>(85 GHz)<\/em> image at 2032 UTC [click to enlarge]<\/p><\/div>\u00a0A NOAA-20 VIIRS Infrared Window (11.45 \u00b5m) image<em><strong> (below)<\/strong> <\/em>showed Goni just after 16 UTC.<\/p>\n<div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201031_16utc_noaa20_infrared_Typhon_Goni_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/10\/201031_16utc_noaa20_infrared_Typhon_Goni_anim.gif\" alt=\"NOAA-20 VIIRS Infrared Window (11.45 ) image [click to enlarge]\" width=\"641\" height=\"335\" \/><\/a><p class=\"wp-caption-text\">NOAA-20 VIIRS Infrared Window<em> (11.45 \u00b5m)<\/em> image [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>2.5-minute rapid scan JMA Himawari-8 &#8220;Red&#8221; Visible (0.64 \u00b5m) images (above) showed Category 5 Super Typhoon Goni in the West Pacific Ocean on 30 October 2020. The images revealed a very small &#8220;pinhole eye&#8221;, surface mesovortices within the eye and a trochoidal motion &#8212; all characteristics of a tropical cyclone at\/near its peak intensity (Goni [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":38786,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[56,62,79,78,53,25,2,48],"tags":[],"class_list":["post-38784","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-dmsp","category-himawari-8","category-microwave","category-noaa-20","category-real-earth","category-satellite-winds","category-tropical-cyclones","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/38784","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=38784"}],"version-history":[{"count":8,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/38784\/revisions"}],"predecessor-version":[{"id":38794,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/38784\/revisions\/38794"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/38786"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=38784"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=38784"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=38784"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}