{"id":43580,"date":"2021-12-01T22:01:00","date_gmt":"2021-12-01T22:01:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=43580"},"modified":"2021-12-03T02:37:00","modified_gmt":"2021-12-03T02:37:00","slug":"typhoon-nyatoh-in-the-west-pacific-ocean","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/43580","title":{"rendered":"Typhoon Nyatoh in the Philippine Sea"},"content":{"rendered":"<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211201_0356utc_noaa20_trueColorRGB_infraredWindow_Nyatoh_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211201_0356utc_noaa20_trueColorRGB_infraredWindow_Nyatoh_anim.gif\" width=\"640\" height=\"315\" \/><\/a><p class=\"wp-caption-text\">NOAA-20 True Color RGB and Infrared Window (11.45 \u00b5m) images [click to enlarge]<\/p><\/div>\n<p>NOAA-20 True Color RGB and Infrared Window (11.45 \u00b5m) images viewed using <a href=\"http:\/\/realearth.ssec.wisc.edu\"><strong>RealEarth<\/strong><\/a> <em><strong>(above)<\/strong><\/em> showed a large convective burst south of the center of Tropical Storm Nahtoh &#8212; located in the <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211201_Nyatoh_map.gif\"><strong>Philippine Sea<\/strong><\/a> &#8212; at 0356 UTC on 01 December 2021. A robust overshooting top near the center of the convective burst exhibited a cluster of cloud-top infrared brightness temperatures of -100\u00baC and colder <em>(red pixels embedded within purple-to-yellow-to-black enhancement)<\/em>.<\/p>\n<p>2.5-minute rapid scan\u00a0<a href=\"https:\/\/www.jma.go.jp\/jma\/indexe.html\"><strong>JMA<\/strong><\/a>\u00a0Himawari-8 Infrared Window (10.4 \u00b5m) images\u00a0<em><strong>(below)<\/strong><\/em> displayed the evolution of Nyatoh as it transitioned from a Tropical Storm to a Category 1 Typhoon at 1200 UTC. The coldest cloud-top infrared brightness temperatures of convective overshooting tops were in the -90 to -98\u00baC range, but did not quite reach the -100\u00baC threshold that was seen in the VIIRS imagery.<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211201_himawari8_infrared_Typhoon_Nyatoh_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/HIM08_IR_NYATOH_01DEC2021_B13_2021335_140215_HIMAWARI-8_0001PANEL_FRAME0000337.GIF\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">JMA Himawari-8 Infrared Window (10.4 \u00b5m) images [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211201_himawari8_infrared_Typhoon_Nyatoh_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p>Himawari-8 Infrared images with contours of 18 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>(below)<\/strong><\/em> showed that Nyatoh was moving through an environment of low to moderate shear.<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211201_himawari8_infrared_18utc_shear_Nyatoh.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211201_himawari8_infrared_18utc_shear_Nyatoh.gif\" width=\"640\" height=\"400\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 Infrared images, with contours of 18 UTC deep-layer wind shear [click to enlarge]<\/p><\/div>\n<p>Himawari-8 Infrared &#8211; Water Vapor Difference images <em><strong>(below)<\/strong><\/em> indicated that much of the deep convection associated with Typhoon Nyatoh was likely penetrating the local tropopause. This product is discussed <a href=\"https:\/\/journals.ametsoc.org\/view\/journals\/wefo\/24\/6\/2009waf2222284_1.xml\"><strong>here<\/strong><\/a>.<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211201_himawari8_infraredWaterVaporDifferenlce_Nyatoh_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211201_himawari8_infraredWaterVaporDifferenlce_Nyatoh_anim.gif\" width=\"640\" height=\"400\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 Infrared &#8211; Water Vapor Difference images [click to enlarge]<\/p><\/div>\n<p>DMSP SSMIS Microwave (85 GHz) images at 1905 UTC and 2148 UTC are shown below. A completely closed eyewall had not yet formed at those times.<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211201_1905utc_dmsp18_ssmis_microwave_Nyatoh.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211201_1905utc_dmsp18_ssmis_microwave_Nyatoh.gif\" width=\"640\" height=\"330\" \/><\/a><p class=\"wp-caption-text\">DMSP-18 SSMIS Microwave (85 GHz) image at 1905 UTC [click to enlarge]<\/p><\/div>\n<p>\u00a0<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211201_2148utc_dmsp17_ssmis_microwave_Nyatoh.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211201_2148utc_dmsp17_ssmis_microwave_Nyatoh.png\" width=\"640\" height=\"330\" \/><\/a><p class=\"wp-caption-text\">DMSP-17 SSMIS Microwave (85 GHz) image at 2148 UTC [click to enlarge]<\/p><\/div>\n<p style=\"text-align: center\"><strong>===== 02 December Update =====<\/strong><\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211202_himawari8_infrared_Nyatoh_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/HIM08_IR_NYATOH_02DEC2021_B13_2021336_120215_HIMAWARI-8_0001PANEL_FRAME0000217.GIF\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">JMA Himawari-8 Infrared Window (10.4 \u00b5m) images [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211202_himawari8_infrared_Nyatoh_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p>Typhoon Nyatoh rapidly intensified to a Category 3 storm by 1200 UTC, and then Category 4 by 1800 on 02 December (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211202_adt_Nyatoh.gif\"><strong>ADT<\/strong><\/a> | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/211202_satcon_Nyatoh.png\"><strong>SATCON<\/strong><\/a>) &#8212; 2.5-minute rapid scan Himawari-8 Infrared images <em><strong>(above)<\/strong><\/em> showed the storm during this intensification period. During the 1200-1800 UTC time frame, subtle waves could be seen propagating south-southwestward across the cold central dense overcast, away from the center of Nyatoh. Energy from those waves was apparently propagating vertically, such that mesospheric airglow waves (<strong>reference<\/strong>) were evident in a Suomi-NPP VIIRS Day\/Night Band (0.7 \u00b5m) image around 1650 UTC <em><strong>(below)<\/strong><\/em>. Other examples of mesospheric airglow waves &#8212; caused by tropical cyclones, deep convection or jet streams &#8212; are available <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?s=mesospheric\"><strong>here<\/strong><\/a> .<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/nyatoh_dnb-20211202_165043.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/12\/nyatoh_dnb-20211202_165043.png\" width=\"640\" height=\"315\" \/><\/a><p class=\"wp-caption-text\">Suomi-NPP VIIRS Day\/Night Band (0.7 \u00b5m) image at 1650 UTC [click to enlarge]<\/p><\/div>\n\n\n<p><\/p>\n","protected":false},"excerpt":{"rendered":"<p>NOAA-20 True Color RGB and Infrared Window (11.45 \u00b5m) images viewed using RealEarth (above) showed a large convective burst south of the center of Tropical Storm Nahtoh &#8212; located in the Philippine Sea &#8212; at 0356 UTC on 01 December 2021. A robust overshooting top near the center of the convective burst exhibited a cluster [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":43592,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[62,78,53,45,49,2,48],"tags":[],"class_list":["post-43580","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-himawari-8","category-noaa-20","category-real-earth","category-redgreenblue-rgb-images","category-suomi_npp","category-tropical-cyclones","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/43580","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=43580"}],"version-history":[{"count":16,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/43580\/revisions"}],"predecessor-version":[{"id":43621,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/43580\/revisions\/43621"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/43592"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=43580"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=43580"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=43580"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}