{"id":66830,"date":"2025-09-21T23:59:00","date_gmt":"2025-09-21T23:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=66830"},"modified":"2025-09-27T02:30:35","modified_gmt":"2025-09-27T02:30:35","slug":"category-5-super-typhoon-ragasa-moves-wnw-across-the-philippine-sea-toward-the-luzon-strait","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/66830","title":{"rendered":"Category 5 Super Typhoon Ragasa moves WNW across the Philippine Sea and into the Luzon Strait"},"content":{"rendered":"<p><div style=\"width: 1290px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250921_himawari9_infrared_Ragasa_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/HIM09_IR_RAGASA_21SEP2025_B13_2025264_100215_0001PANEL_FRAME00241.GIF\" width=\"1280\" height=\"960\" \/><\/a><p class=\"wp-caption-text\">2.5-minute Himawari-9 Infrared images, from 0002-2042 UTC on 21 September [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250921_himawari9_infrared_Ragasa_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>2.5-minute Target Sector <a href=\"https:\/\/www.jma.go.jp\/jma\/indexe.html\"><strong>JMA<\/strong><\/a> Himawari-9 Infrared images <em><strong>(above)<\/strong><\/em> showed Ragasa as it intensified from a Category 4 Typhoon at 0000 UTC on 21 September 2025 to a Category 5 (140-knot) Super Typhoon at 0600 UTC and then further to a 145-knot Super Typhoon by 1200 UTC (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250921_satcon_Ragasa.png\"><strong>SATCON<\/strong><\/a>). There was a ~2 hour gap in Target Sector images, from 1100-1250 UTC; during that period, 10-minute Full Disk imagery was used to fill the gap.<\/p>\n<p>The primary environmental factor that favored this intensification was low values of <a href=\"https:\/\/tropic.ssec.wisc.edu\/misc\/winds\/info.winds.shr.html\"><strong>deep-layer wind shear<\/strong><\/a> <em><strong>(below)<\/strong><\/em> &#8212; in addition, Ragasa traversed a lobe of slightly warmer waters (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250921_sst_Ragasa.gif\"><strong>Sea Surface Temperature<\/strong><\/a> | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250921_ohc_Ragasa.gif\"><strong>Ocean Heat Content<\/strong><\/a>) as it reached Category 5 intensity.<\/p>\n<div style=\"width: 1064px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250921_himawari9_infrared_2100utcShear_Ragasa_anim.gif\" width=\"1054\" height=\"704\" \/><p class=\"wp-caption-text\">Himawari-9 Infrared images, with contours and streamlines of deep-layer wind shear at 1800 UTC on 21 September<\/p><\/div>\n<p>Ragasa was undergoing an eyewall replacement cycle (ERC) on 21 September, which was evident in the <a href=\"https:\/\/tropic.ssec.wisc.edu\/real-time\/mimtc\/tc.shtml\"><strong>MIMIC-TC<\/strong><\/a> product <em><strong>(below)<\/strong><\/em> &#8212; the smaller-diameter inner eyewall was eventually replaced by a larger-diameter outer eyewall. However, the ERC did not adversely affect the intensity of the Super Typhoon during the course of the day.<\/p>\n<div style=\"width: 730px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250921_mimicTC_Ragasa_ERC_anim.gif\" width=\"720\" height=\"540\" \/><p class=\"wp-caption-text\">MIMIC-TC product on 21 September<\/p><\/div>\n<p>3 snapshots of microwave imagery during the day (from DMSP\/SSMIS and NOAA-21\/ATMS) are shown below.<\/p>\n<div style=\"width: 1062px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250921_1003utc_dmsp16_ssmis_microwave_Ragasa.gif\" width=\"1052\" height=\"601\" \/><p class=\"wp-caption-text\">DMSP-16 SSMIS image at 1003 UTC on 21 September<\/p><\/div>\n<div style=\"width: 1062px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250921_1731utc_atms_microwave_Ragasa.gif\" width=\"1052\" height=\"694\" \/><p class=\"wp-caption-text\">NOAA-21 ATMS image at 1731 UTC on 21 September<\/p><\/div>\n<div style=\"width: 1062px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250921_2152utc_dmsp17_ssmis_Ragasa.gif\" width=\"1052\" height=\"601\" \/><p class=\"wp-caption-text\">DMSP-17 SSMIS image at 2152 UTC on 21 September<\/p><\/div>\n<p>[the wind shear, sea surface temperature, ocean heat content and microwave products shown above were sourced from the <a href=\"https:\/\/tropic.ssec.wisc.edu\"><strong>CIMSS Tropical Cyclones<\/strong><\/a> site]<\/p>\n<p>An RCM-3 Synthetic Aperture Radar (SAR) Wind Speed image <em><strong>(below)<\/strong><\/em> also highlighted a narrow &#8220;moat&#8221; of lower wind speed that was surrounding the inner eyewall at 2131 UTC (a &#8220;brightness temperature moat&#8221; feature was also seen in the 2152 UTC DMSP-17 SSMIS microwave image).<\/p>\n<p><div style=\"width: 1810px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250921_2131utc_rcm3_sar_Ragasa.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250921_2131utc_rcm3_sar_Ragasa.png\" width=\"1800\" height=\"2413\" \/><\/a><p class=\"wp-caption-text\">RCM-3 Synthetic Aperture Radar image at 2131 UTC on 21 September [click to enlarge]<\/p><\/div>A sunrise-to-sunset animation of 2.5-minute Himawari-9 Visible images <em><strong>(below)<\/strong><\/em> revealed the presence of low-level mesovortices within the large eye. Super Typhoon Ragasa made its first landfall on the tiny island of <a href=\"https:\/\/en.wikipedia.org\/wiki\/Babuyan_Island\"><strong>Babuyan<\/strong><\/a> in the Luzon Strait after 0300 UTC on 22 September.<\/p>\n<p><div style=\"width: 1290px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250922_himawari9_visible_STY_Ragasa_mesovortices_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/HIM09_VIS_RAGASA_22SEP2025_B3_2025265_034944_0001PANEL_FRAME00144.GIF\" width=\"1280\" height=\"960\" \/><\/a><p class=\"wp-caption-text\">2.5-minute Himawari-9 Visible images, from 2152 UTC on 21 September to 0832 UTC on 22 September [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250922_himawari9_visible_STY_Ragasa_mesovortices_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>A Suomi-NPP VIIRS Day\/Night Band image at 0511 UTC on 22 September &#8212; when Ragasa was still at Category 5 intensity <em><strong>(below)<\/strong><\/em> displayed the 40-mile diameter eye as its western edge was near Synoptic Station 981330 (<a href=\"https:\/\/en.wikipedia.org\/wiki\/Calayan_Island\"><strong>Calayan Island<\/strong><\/a>).<\/p>\n<div style=\"width: 2982px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250922_0511utc_suomiNPP_viirs_dayNightBand_Ragasa.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250922_0511utc_suomiNPP_viirs_dayNightBand_Ragasa.png\" width=\"2972\" height=\"1718\" \/><\/a><p class=\"wp-caption-text\">Suomi-NPP VIIRS Day\/Night Band image valid at 0511 UTC on 22 September [click to enlarge]<\/p><\/div>\n<div style=\"width: 750px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250921_0129utc_sentinel3b_altimetry_Ragasa.png\" width=\"740\" height=\"650\" \/><p class=\"wp-caption-text\">Sentinel-3B Altimetry data, showing a Significant Wave Height value of 27.75 ft east of Luzon at 0129 UTC on 21 September<\/p><\/div>\n<p>The strong winds associated with Super Typhoon Ragasa caused high waves <em><strong>(above)<\/strong><\/em>, which resulted in an upwelling of cooler sub-surface water in the northwest Philippine Sea &#8212; late in the day on 22 September (when Ragasa was located far to west, in the South China Sea), note the pocket of 27-28\u00baC Sea Surface Temperatures (yellow to light orange) along and north of the track of Ragasa at the point where it first reached Category 5 intensity from 0600-1200 UTC on 21 September <em><strong>(below)<\/strong><\/em>. Sea Surface Temperatures over that area of upwelling were around <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250921_sst_Ragasa.gif\"><strong>30\u00baC<\/strong><\/a> just prior to the passage of Ragasa.<\/p>\n<div style=\"width: 1063px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250923_sst_Ragasa.gif\" width=\"1053\" height=\"699\" \/><p class=\"wp-caption-text\">Sea Surface Temperature analysis at 2233 UTC on 22 September, with a plot of Ragasa&#8217;s track from 18-23 September<\/p><\/div>\n<p>As Ragasa was beginning to move west-northwestward away from northern Luzon on 22 September, a Significant Wave Height of 58.26 ft was sensed at 1352 UTC <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 750px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2025\/09\/250922_1352utc_sentinel3b_altimetry_Ragasa.png\" width=\"740\" height=\"650\" \/><p class=\"wp-caption-text\">Sentinel-3B Altimetry data, showing a Significant Wave Height of 58.26 ft north of Luzon at 1352 UTC on 22 September<\/p><\/div>\n<p>Additional information pertaining to Ragasa is available in <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/66839\"><strong>this blog post<\/strong><\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>2.5-minute Target Sector JMA Himawari-9 Infrared images (above) showed Ragasa as it intensified from a Category 4 Typhoon at 0000 UTC on 21 September 2025 to a Category 5 (140-knot) Super Typhoon at 0600 UTC and then further to a 145-knot Super Typhoon by 1200 UTC (SATCON). There was a ~2 hour gap in Target [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":66833,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[152,89,56,73,79,131,47,104,25,49,2,48],"tags":[143],"class_list":["post-66830","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-altimetry","category-atms","category-dmsp","category-himawari-9","category-microwave","category-noaa-21","category-other-satellites","category-sar","category-satellite-winds","category-suomi_npp","category-tropical-cyclones","category-viirs","tag-atmospheric-river"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/66830","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=66830"}],"version-history":[{"count":44,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/66830\/revisions"}],"predecessor-version":[{"id":66957,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/66830\/revisions\/66957"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/66833"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=66830"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=66830"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=66830"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}