{"id":55576,"date":"2023-11-13T20:53:12","date_gmt":"2023-11-13T20:53:12","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=55576"},"modified":"2023-11-17T18:34:16","modified_gmt":"2023-11-17T18:34:16","slug":"tropical-storm-mal-in-the-south-pacific","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/55576","title":{"rendered":"Tropical Storm Mal in the south Pacific"},"content":{"rendered":"\n<figure class=\"wp-block-image size-full\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/11\/comp20231110.0000_to_1113.1700anim.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1000\" height=\"470\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/11\/comp20231110.0000_to_1113.1700anim.gif\" alt=\"\" class=\"wp-image-55577\"\/><\/a><figcaption class=\"wp-element-caption\">Total Precipitable Water fields 0000 UTC 10 November &#8211; 1700 UTC 13 November 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>MIMIC Total Precipitable Water fields over the south Pacific near Fiji and Australia, above (<a href=\"http:\/\/tropic.ssec.wisc.edu\/real-time\/mtpw2\/product.php?color_type=tpw_nrl_colors&amp;prod=ausf&amp;timespan=24hrs&amp;anim=html5\">source<\/a>), show the development of a cyclonic circulation in between the ITCZ and SPCZ that moves southward as Cyclone Mal.  Some dry air is diagnosed to impinge on the northern part of the storm at the end of the animation.<\/p>\n\n\n\n<p>Himawari-9 Clean Window infrared (10.4) imagery, below, shows the development of a very cold Central Dense Overcast (CDO) by 1600 UTC, with brightness temperatures (violet in the enhancement used) between -85<sup>o<\/sup>C and -90<sup>o<\/sup>C.<\/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\/11\/H9Band13-20231113_0000_to_1600anim.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1228\" height=\"854\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/11\/H9Band13-20231113_0000_to_1600anim.gif\" alt=\"\" class=\"wp-image-55578\"\/><\/a><figcaption class=\"wp-element-caption\">Himawari-9 Clean Window (Band 13, 10.4 \u00b5m) infrared imagery, hourly from 0000 UTC to 1600 UTC on 13 November 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n<p>A closer look at 10-minute Himawari-9 Infrared images <em><strong>(below)<\/strong><\/em> revealed that cloud-top 10.4 \u00b5m brightness temperatures within the CDO were as cold as -96\u00baC (darker gray pixels embedded within the interior yellow-enhanced region) at 1450 UTC.<\/p>\n<div style=\"width: 1290px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231113_himawari9_infrared_TS_Mai_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/HIM09_IR_MAL_13NOV2023_B13_2023317_145000_0001PANEL_FRAME00020.GIF\" width=\"1280\" height=\"960\" \/><\/a><p class=\"wp-caption-text\">JMA Himawari-9 &#8220;Clean&#8221; Infrared Window (10.4 \u00b5m) images, from 1130 UTC to 1800 UTC on 13 November (courtesy Scott Bachmeier, CIMSS) [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2023\/11\/231113_himawari9_infrared_TS_Mai_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p>What are shear values like around Mal?  The animation below, taken from the SSEC\/CIMSS <a href=\"https:\/\/tropic.ssec.wisc.edu\">Tropical Weather website<\/a> (<a href=\"https:\/\/tropic.ssec.wisc.edu\/real-time\/windmain.php?&amp;basin=austeast&amp;sat=wgms&amp;prod=shr&amp;zoom=&amp;time=\">direct link<\/a>) shows modest amounts of shear over the storm, with significantly more shear to the south.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/11\/wgmsshr_0300_to_1800UTC_13November2023.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"880\" height=\"680\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/11\/wgmsshr_0300_to_1800UTC_13November2023.gif\" alt=\"\" class=\"wp-image-55579\"\/><\/a><figcaption class=\"wp-element-caption\">Diagnosed 850-200 mb shear, 0300-1800 UTC on 13 November 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>Morphed microwave imagery (<a href=\"https:\/\/tropic.ssec.wisc.edu\/real-time\/mimtc\/2023_02P\/web\/mainpage.html\">source<\/a>), below, shows a slow organization of the storm with vigorous convection surrounding about half the eye by 1900 UTC.<\/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\/11\/MIMIC_TC_MAL_13November2023_0000_to_1900.gif\" alt=\"\" class=\"wp-image-55581\"\/><figcaption class=\"wp-element-caption\">Morphed Microwave Imagery at CIMSS (MIMIC) fields around Mal, 0000 &#8211; 1900 UTC on 13 November 2023 (click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>The AMSU 89-GHz field at 0952 UTC on 13 November, below (source), also shows evidence of strong convection (i.e., cold brightness temperatures caused by strong scattering of 89 GHz energy by ice) near the storm center.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"1000\" height=\"1000\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/11\/AMSU_89GHz_202402P1113_0952.gif\" alt=\"\" class=\"wp-image-55582\"\/><figcaption class=\"wp-element-caption\">89-GHz imagery, 0952 UTC on 13 November 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>For more information on Mal, refer to the CIMSS Tropical Website for this storm (<a href=\"https:\/\/tropic.ssec.wisc.edu\/real-time\/summary\/summary.02P_2023.html\">link<\/a>), or to the <a href=\"https:\/\/www.met.gov.fj\/\">Fiji RSMC<\/a>.  The forecast for the storm from <a href=\"https:\/\/www.metoc.navy.mil\/jtwc\/jtwc.html\">JTWC<\/a> (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/11\/ForecastPath.gif\">here<\/a>), shows intensification through 1200 UTC 14 November, and a path that takes the storm very close to Fiji. The forecast graphic from Fiji is shown below, showing something similar to the JTWC graph.  Note the times on the graphic below are Fiji Standard time, i.e., UTC + 12.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"605\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/11\/Mal_InformationFromFiji-1024x605.png\" alt=\"\" class=\"wp-image-55584\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/11\/Mal_InformationFromFiji-1024x605.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/11\/Mal_InformationFromFiji-300x177.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/11\/Mal_InformationFromFiji-768x453.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/11\/Mal_InformationFromFiji.png 1487w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><figcaption class=\"wp-element-caption\">Tropical Cyclone Mal forecast track and threats, issued 1900 UTC on 13 November 2023 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<figure class=\"wp-block-video\"><video height=\"1566\" style=\"aspect-ratio: 2874 \/ 1566;\" width=\"2874\" autoplay controls loop muted src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2023\/11\/malnearfiji.mov\"><\/video><figcaption class=\"wp-element-caption\">24 frames of Tropical Cyclone Mal every hour, from 2023-11-12 at 2100Z to 2023-11-13 at 2100Z. Imagery is from Japan&#8217;s Advanced Himawari Imager. Both true color imagery and Band 9 mid-level water vapor imagery are show. Users can <a href=\"https:\/\/realearth.ssec.wisc.edu\/?products=HIMAWARI-B09.100,H-TrueColor-wgt.72&amp;center=-14.813568566582274,175.80804801548697&amp;zoom=4&amp;width=1180&amp;height=783&amp;basemap=satellite&amp;labels=line&amp;view=globe&amp;collection=RealEarth&amp;timerange=2023-11-12+21:00:00,2023-11-13+21:00:00&amp;timestep=1h&amp;animationspeed=76&amp;animate=true\">recreate this animation in RealEarth.<\/a> <\/figcaption><\/figure>\n\n\n\n<p>Users can view Mal using RealEarth such as in the example above, provided by Alexa Ross, SSEC\/CIMSS, that shows true color imagery and Band 9 mid-level water vapor infrared (6.95 \u00b5m) imagery from Japan&#8217;s Advanced Himawari Imager (AHI). <\/p>\n","protected":false},"excerpt":{"rendered":"<p>MIMIC Total Precipitable Water fields over the south Pacific near Fiji and Australia, above (source), show the development of a cyclonic circulation in between the ITCZ and SPCZ that moves southward as Cyclone Mal. Some dry air is diagnosed to impinge on the northern part of the storm at the end of the animation. Himawari-9 [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":55586,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[73,2],"tags":[],"class_list":["post-55576","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-himawari-9","category-tropical-cyclones"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/55576","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=55576"}],"version-history":[{"count":9,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/55576\/revisions"}],"predecessor-version":[{"id":55654,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/55576\/revisions\/55654"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/55586"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=55576"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=55576"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=55576"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}