{"id":40705,"date":"2021-04-20T22:59:30","date_gmt":"2021-04-20T22:59:30","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=40705"},"modified":"2021-04-23T03:09:49","modified_gmt":"2021-04-23T03:09:49","slug":"subtropical-storm-potira-off-the-coast-of-brazil","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/40705","title":{"rendered":"Subtropical Storm Potira off the coast of Brazil"},"content":{"rendered":"<p><div style=\"width: 649px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/210420_goes16_visible_STS_Potira_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/sts_vis-20210420_150153.png\" alt=\"GOES-16 \u201cRed\u201d Visible (0.64 \u00b5m) images [click to play animation | MP4]\" width=\"639\" height=\"298\" \/><\/a><p class=\"wp-caption-text\">GOES-16 \u201cRed\u201d Visible <em>(0.64 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/210420_goes16_visible_STS_Potira_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>1-minute\u00a0<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/23225\"><strong>Mesoscale Domain Sector<\/strong><\/a>\u00a0GOES-16\u00a0<em>(GOES-East)<\/em>\u00a0\u201cRed\u201d Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>) images <em><strong>(above)<\/strong><\/em> showed the circulation of Subtropical Storm Potira (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/210420_STS_Potira_warning.text\"><strong>warning<\/strong><\/a>\u00a0issued by <a href=\"https:\/\/www.marinha.mil.br\/chm\/\"><strong>MARINHA<\/strong><\/a>) off the southeast coast of Brazil on 20 April 2021.<\/p>\n<p>In the corresponding 1-minute GOES-16 \u201cClean\u201d Infrared Window (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band13.pdf\"><strong>10.35 \u00b5m<\/strong><\/a>) images <em><strong>(below)<\/strong>,<\/em> intermittent convective overshooting tops exhibited infrared brightness temperatures as cold as -60 to -65\u00baC <em>(shades of orange)<\/em>.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/210420_goes16_infrared_STS_Potira_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/sts_ir-20210420_150153.png\" alt=\"GOES-16 \u201cClean\u201d Infrared Window (10.35 \u00b5m) images [click to play animation | MP4]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">GOES-16 \u201cClean\u201d Infrared Window <em>(10.35 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/210420_goes16_infrared_STS_Potira_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>Combined plots of all GOES-16 Atmospheric Motion Vector types &#8212; Visible, Infrared and Water Vapor &#8212; and pressure levels at 15-minute intervals <em><strong>(below)<\/strong><\/em> displayed the cloud motions of Potira (credit: Dave Stettner and Chris Velden, CIMSS). The algorithm used to generate these AMVs differs slightly from that used to create operational <a href=\"https:\/\/rammb2.cira.colostate.edu\/trainings\/visit\/training_sessions\/goes_r_derived_motion_vectors\/\"><strong>Derived Motion Winds<\/strong><\/a>: some constraints are relaxed\/removed, and Visible winds are calculated at pressure levels above 700 hPa &#8212; all of which results in the display of a higher density of tracked targets and their calculated wind vectors.<\/p>\n<p><div style=\"width: 570px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/210420_STS_Potira_satellite_winds_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/g16OFcombined.20210420.1030.gif\" alt=\"Combined plot of all GOES-16 Atmospheric Motion Vector types (Visible, Infrared and Water Vapor) at 15-minute intervals [click to play animation | MP4]\" width=\"560\" height=\"560\" \/><\/a><p class=\"wp-caption-text\">Combined plots of all GOES-16 Atmospheric Motion Vector types (Visible, Infrared and Water Vapor) and pressure levels, at 15-minute intervals [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/210420_STS_Potira_satellite_winds_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>A sequence of <a href=\"https:\/\/www.eumetsat.int\/\"><strong>EUMETSAT<\/strong><\/a> Metop ASCAT surface scatterometer winds (<a href=\"https:\/\/manati.star.nesdis.noaa.gov\/datasets\/ASCATCData.php\"><strong>source<\/strong><\/a>) is is shown below &#8212; the strongest winds were located within the southern sector of the storm, well away from the center of circulation.<\/p>\n<div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/210420_metop_ascat_STSPotira_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/210420_metop_ascat_STSPotira_anim.gif\" alt=\"Metop ASCAT surface scatterometer winds [click to enlarge]\" width=\"642\" height=\"564\" \/><\/a><p class=\"wp-caption-text\">Metop ASCAT surface scatterometer winds [click to enlarge]<\/p><\/div>\n<p style=\"text-align: center;\"><strong>===== 22 April Update =====<\/strong><\/p>\n<p><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/210422_goes16_visible_STS_Potira_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/sts_vis-20210422_120122.png\" alt=\"GOES-16 \u201cRed\u201d Visible (0.64 \u00b5m) images [click to play animation | MP4]\" width=\"643\" height=\"300\" \/><\/a><p class=\"wp-caption-text\">GOES-16 \u201cRed\u201d Visible <em>(0.64 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/210422_goes16_visible_STS_Potira_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>1-minute GOES-16 Visible images <em><strong>(above)<\/strong><\/em> showed that the low-level circulation center of Potira remained exposed on 22 April &#8212; while GOES-16 Infrared images <em><strong>(below)<\/strong><\/em> indicated that deep convection remained south and west of the storm center.<\/p>\n<div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/210422_goes16_infrared_STS_Potira_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/sts_ir-20210422_120122.png\" alt=\"GOES-16 \u201cClean\u201d Infrared Window (10.35 \u00b5m) images [click to play animation | MP4]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">GOES-16 \u201cClean\u201d Infrared Window<em> (10.35 \u00b5m)<\/em> images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/04\/210422_goes16_infrared_STS_Potira_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>1-minute\u00a0Mesoscale Domain Sector\u00a0GOES-16\u00a0(GOES-East)\u00a0\u201cRed\u201d Visible (0.64 \u00b5m) images (above) showed the circulation of Subtropical Storm Potira (warning\u00a0issued by MARINHA) off the southeast coast of Brazil on 20 April 2021. In the corresponding 1-minute GOES-16 \u201cClean\u201d Infrared Window (10.35 \u00b5m) images (below), intermittent convective overshooting tops exhibited infrared brightness temperatures as cold as -60 to -65\u00baC (shades [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":40711,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[74,58,25,2],"tags":[],"class_list":["post-40705","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-16","category-metop","category-satellite-winds","category-tropical-cyclones"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/40705","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=40705"}],"version-history":[{"count":10,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/40705\/revisions"}],"predecessor-version":[{"id":40729,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/40705\/revisions\/40729"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/40711"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=40705"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=40705"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=40705"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}