{"id":60912,"date":"2024-09-27T14:00:05","date_gmt":"2024-09-27T14:00:05","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=60912"},"modified":"2024-09-30T14:22:31","modified_gmt":"2024-09-30T14:22:31","slug":"john-along-the-coast-of-mexico","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/60912","title":{"rendered":"John along the coast of Mexico"},"content":{"rendered":"\n<figure class=\"wp-block-video\"><video height=\"960\" style=\"aspect-ratio: 1440 \/ 960;\" width=\"1440\" controls loop src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/09\/GOES-18_ABI_RadF_C13_20240921_0000_to_0928_0300_John_anim.mp4\"><\/video><figcaption class=\"wp-element-caption\">GOES-18 Band 13 Infrared (10.3 \u00b5m) imagery, 0000 UTC 21 September 2024 &#8211; 0300 UTC 28 September 2024<\/figcaption><\/figure>\n\n\n\n<p>Hurricane John was an intense cyclone that affected the Pacific coast of Mexico for a about a week in late September 2024.  (Click <a href=\"https:\/\/www.nhc.noaa.gov\/archive\/2024\/JOHN_graphics.php\">here<\/a> to see an approximate path).  The storm was noteworthy in that it made landfall, dissipated, re-developed, and then made landfall again.  The animation above shows the lifecycle of the system, starting as a tropical wave south of Mexico and ending with a slow approach to the coast on the 26th and 27th.  John weakened as it moved along the coast, before dissipating late on the 27th.<\/p>\n\n\n\n<p>Hurricane John made landfall <a href=\"https:\/\/www.nhc.noaa.gov\/archive\/2024\/ep10\/ep102024.update.09240322.shtml?\">just after 0300 UTC UTC on 24 September<\/a>.  At 0200 UTC, shown below, a well-developed eye is apparent in satellite imagery, and strong convection is wrapped around that eye.  The structure of the hurricane was quickly disrupted once inland, and <a href=\"https:\/\/www.nhc.noaa.gov\/archive\/2024\/ep10\/ep102024.discus.010.shtml?\">by 1800 UTC on the 24th<\/a>, the National Hurricane Center ceased advisories on the system, with the caveat that the system could still generate heavy rain, and might redevelop.<\/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\/2024\/09\/GOES-18_ABI_RadF_C13_20240924_0200_JohnLT.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"683\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/09\/GOES-18_ABI_RadF_C13_20240924_0200_JohnLT-1024x683.png\" alt=\"\" class=\"wp-image-60918\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/09\/GOES-18_ABI_RadF_C13_20240924_0200_JohnLT-1024x683.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/09\/GOES-18_ABI_RadF_C13_20240924_0200_JohnLT-300x200.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/09\/GOES-18_ABI_RadF_C13_20240924_0200_JohnLT-768x512.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/09\/GOES-18_ABI_RadF_C13_20240924_0200_JohnLT.png 1440w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">GOES-18 Clean Window infrared (Band 13, 10.3 \u00b5m) at 0200 UTC 24 September 2024 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>At 1200 UTC on 26 September 2024, shown below, John has redeveloped into a hurricane, with curved bands in the infrared imagery, to the east of a large mesoscale convective system.  John weakened as it moved parallel to the coast for the next 30 hours, dissipating at 2100 UTC on 27 September.<\/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\/2024\/09\/GOES-18_ABI_RadF_C13_20240926_1200_JohnLT.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"683\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/09\/GOES-18_ABI_RadF_C13_20240926_1200_JohnLT-1024x683.png\" alt=\"\" class=\"wp-image-60920\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/09\/GOES-18_ABI_RadF_C13_20240926_1200_JohnLT-1024x683.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/09\/GOES-18_ABI_RadF_C13_20240926_1200_JohnLT-300x200.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/09\/GOES-18_ABI_RadF_C13_20240926_1200_JohnLT-768x512.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2024\/09\/GOES-18_ABI_RadF_C13_20240926_1200_JohnLT.png 1440w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">GOES-18 Clean Window infrared (Band 13, 10.3 \u00b5m) at 1200 UTC 26 September 2024 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Hurricane John was an intense cyclone that affected the Pacific coast of Mexico for a about a week in late September 2024. (Click here to see an approximate path). The storm was noteworthy in that it made landfall, dissipated, re-developed, and then made landfall again. The animation above shows the lifecycle of the system, starting [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":60918,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[114,2],"tags":[],"class_list":["post-60912","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-18","category-tropical-cyclones"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/60912","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=60912"}],"version-history":[{"count":4,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/60912\/revisions"}],"predecessor-version":[{"id":60921,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/60912\/revisions\/60921"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/60918"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=60912"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=60912"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=60912"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}