{"id":11322,"date":"2012-09-13T19:36:38","date_gmt":"2012-09-13T19:36:38","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=11322"},"modified":"2012-09-14T16:18:28","modified_gmt":"2012-09-14T16:18:28","slug":"super-typhoon-sanba","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/11322","title":{"rendered":"Super Typhoon Sanba"},"content":{"rendered":"
\"MTSAT-2<\/a>

MTSAT-2 10.8 \u00c2\u00b5m IR channel images (click image to play animation)<\/p><\/div>\n

McIDAS images of MTSAT-2 10.8 \u00c2\u00b5m IR channel images (above; click image to play animation)<\/strong><\/em> showed the formation of a large and well-defined eye as Super Typhoon 17W (Sanba) intensified over the West Pacific Ocean on 13 September 2012.<\/p>\n

A plot of the CIMSS Advanced Dvorak Technique<\/strong><\/a> intensity estimate (below)<\/strong><\/em> showed the trend of rapid intensification.<\/p>\n

\"CIMSS<\/a>

CIMSS ADT plot for Storm 17W (Sanba)<\/p><\/div>\n

Sanba was in an environment characterized by relatively low values of Deep Layer Wind Shear (below),<\/strong><\/em> which favored intensification.<\/p>\n

\"MTSAT-2<\/a>

MTSAT-2 IR images + Deep layer wind shear<\/p><\/div>\n

Sanba had also been moving over a region with very warm Sea Surface Temperatures and a very high Ocean Heat Content values (below)<\/strong><\/em>.<\/p>\n

\"Track<\/a>

Track of Sanba overlaid on Sea Surface Temperature + Ocean Heat Content products<\/p><\/div>\n

The first daylight MTSAT-2 0.7 \u00c2\u00b5m visible channel images (below)<\/strong><\/em> showed nice eye and eyewall structure.<\/p>\n

\"MTSAT-2<\/a>

MTSAT-2 0.7 \u00c2\u00b5m visible channel images<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"

McIDAS images of MTSAT-2 10.8 \u00c2\u00b5m IR channel images (above; click image to play animation) showed the formation of a large and well-defined eye as Super Typhoon 17W (Sanba) intensified over the West Pacific Ocean on 13 September 2012. A plot of the CIMSS Advanced Dvorak Technique intensity estimate (below) showed the trend of rapid […]<\/p>\n","protected":false},"author":18,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[20,25,2],"tags":[],"class_list":["post-11322","post","type-post","status-publish","format-standard","hentry","category-mtsat","category-satellite-winds","category-tropical-cyclones"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/11322","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=11322"}],"version-history":[{"count":8,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/11322\/revisions"}],"predecessor-version":[{"id":11324,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/11322\/revisions\/11324"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=11322"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=11322"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=11322"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}