{"id":53709,"date":"2023-07-26T23:59:00","date_gmt":"2023-07-26T23:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=53709"},"modified":"2023-07-27T23:59:57","modified_gmt":"2023-07-27T23:59:57","slug":"near-simultaneous-sar-observations-over-typhoon-doksuri","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/53709","title":{"rendered":"Near-simultaneous SAR observations over Typhoon Doksuri"},"content":{"rendered":"\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1313\" height=\"902\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/SARWINds_S1a_RCMs_H09_Band13-20230726_2202_anim.gif\" alt=\"\" class=\"wp-image-53710\"\/><figcaption class=\"wp-element-caption\">SAR Winds (Color bar ranges from 0-80 knots) from Sentinel-1A (2201 UTC) and RCM-3 (2202 UTC); Himawari-9 Clean Window infrared (Band 13, 10.4 \u00b5m) imagery, 2200 UTC, 26 July 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>Typhoon Doksuri moved between the Philippines and Taiwan late on 26 July 2023 as it approached mainland China.  Both Sentinel-1A and RCM-3 overflew the storm shortly after 2200 UTC on 26 July, and those two scenes are shown above in concert with a Band 13 Himawari-9 Clean Window infrared (10.4 \u00b5m) imagery.  (All SAR observations of Doksuri are available <a href=\"https:\/\/www.star.nesdis.noaa.gov\/socd\/mecb\/sar\/sarwinds_tropical.php?year=2023&amp;storm=WP052023_DOKSURI\">here<\/a>).  The asymmetric nature of the storm is very notable, with winds exceeding 70 knots in the eyewall to the north and east of the storm (winds exceed 80 knots in the convective band farther to the east &#8212; the region of white in the wind enhancement used).  In contrast, winds in the western eyewall are between 35 and 50 knots &#8212; and there is a curious wind speed minimum just west of the eyewall! <\/p>\n\n\n\n<p>A <a href=\"https:\/\/tropic.ssec.wisc.edu\/real-time\/mimtc\/tc.shtml\">MIMIC-TC<\/a> animation from 26 July 2023, below, also shows the marked asymmetry in the storm.  Doksuri&#8217;s path was right along the northern coastline of of Luzon, the northernmost large island of the Philippines.  Mountain ranges on that island may have influenced the structure of the storm.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"720\" height=\"540\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/MIMIC_TC_Doksuri_26July2023.gif\" alt=\"\" class=\"wp-image-53711\"\/><figcaption class=\"wp-element-caption\">MIMIC-TC animation of Doksuri, 0000 UTC 26 July &#8212; 0000 UTC 27 July 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>Wind shear over the system at the time of the SAR overpasses was light, but would be acting to displace the convection south and east of the storm center, as observed.  The image below was taken from the <a href=\"https:\/\/tropic.ssec.wisc.edu\">CIMSS Tropical Weather Site<\/a>.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/Shear_850-200_2100_26July2023.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"512\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/Shear_850-200_2100_26July2023-1024x512.gif\" alt=\"\" class=\"wp-image-53712\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/Shear_850-200_2100_26July2023-1024x512.gif 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/Shear_850-200_2100_26July2023-300x150.gif 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/07\/Shear_850-200_2100_26July2023-768x384.gif 768w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">Atmospheric Shear (roughly 850-200 mb) at 2100 UTC on 26 July 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>For current information on Doksuri, refer to the <a href=\"https:\/\/www.metoc.navy.mil\/jtwc\/jtwc.html\">Joint Typhoon Warning Center<\/a>, the <a href=\"https:\/\/www.jma.go.jp\/jma\/jma-eng\/jma-center\/rsmc-hp-pub-eg\/RSMC_HP.htm\">Tokyo RSMC<\/a>, the <a href=\"https:\/\/rammb-data.cira.colostate.edu\/tc_realtime\/storm.asp?storm_identifier=wp052023\">CIRA Real-Time Tropical Website <\/a>and the <a href=\"https:\/\/tropic.ssec.wisc.edu\">CIMSS Tropical Weather Site<\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Typhoon Doksuri moved between the Philippines and Taiwan late on 26 July 2023 as it approached mainland China. Both Sentinel-1A and RCM-3 overflew the storm shortly after 2200 UTC on 26 July, and those two scenes are shown above in concert with a Band 13 Himawari-9 Clean Window infrared (10.4 \u00b5m) imagery. (All SAR observations [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":53714,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[10,73,104,25,2],"tags":[],"class_list":["post-53709","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-general-interpretation","category-himawari-9","category-sar","category-satellite-winds","category-tropical-cyclones"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/53709","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\/19"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=53709"}],"version-history":[{"count":5,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/53709\/revisions"}],"predecessor-version":[{"id":53718,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/53709\/revisions\/53718"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/53714"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=53709"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=53709"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=53709"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}