{"id":13674,"date":"2013-08-14T14:50:58","date_gmt":"2013-08-14T14:50:58","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=13674"},"modified":"2013-08-14T16:06:27","modified_gmt":"2013-08-14T16:06:27","slug":"goes-14-srso-r-views-of-convection-over-montana","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/13674","title":{"rendered":"GOES-14 SRSO-R Views of Convection over Montana"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/08\/GOES14_15_VIS2013226_Montanaloop.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"      \" title=\"GOES-14 and GOES-15 0.62 \u00c2\u00b5m Visible images (click image to play animation)\" alt=\"GOES-14 and GOES-15 0.62 \u00c2\u00b5m Visible images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/08\/GOES14_15_VIS_2013226_0000UTC.GIF\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-14 and GOES-15 0.62 \u00c2\u00b5m Visible images (click image to play animation)<\/p><\/div>\n<p><a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/srsor2013\/GOES-14_SRSOR.html\">SRSO-R GOES-14<\/a> 1-minute imagery shows the dynamic nature of the cirrus canopy over developing convection.  Strong convection over Montana includes multiple overshooting tops that are visible in the GOES-14 imagery.  Routine GOES-15 imagery, also shown, lacks the temporal resolution to capture the growth and decay of many cloud-top features.  This is especially true every three hours when a full-disk image is scanned (at 0000 UTC, for example), and at times when satellite housekeeping precludes scanning (at 0045 UTC in this case).  The 10.7 \u00c2\u00b5m imagery, below, tells a similar tale.  Cold cloud tops appear and vanish at time scales that are not resolved by present operational capabilities.<\/p>\n<p>GOES-R will allow for simultaneous full disk scanning and RSO scanning at the mesoscale.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/08\/GOES14_15_2013226_Montanaloop.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"      \" title=\"GOES-14 and GOES-15 10.7 \u00c2\u00b5m IR images (click image to play animation)\" alt=\"GOES-14 and GOES-15 10.7 \u00c2\u00b5m IR images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/08\/GOES14_15_2013226_0000UTC.GIF\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-14 and GOES-15 10.7 \u00c2\u00b5m IR images (click image to play animation)<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>SRSO-R GOES-14 1-minute imagery shows the dynamic nature of the cirrus canopy over developing convection. Strong convection over Montana includes multiple overshooting tops that are visible in the GOES-14 imagery. Routine GOES-15 imagery, also shown, lacks the temporal resolution to capture the growth and decay of many cloud-top features. This is especially true every three [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[40,34],"tags":[],"class_list":["post-13674","post","type-post","status-publish","format-standard","hentry","category-goes-14","category-goes-r"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/13674","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=13674"}],"version-history":[{"count":5,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/13674\/revisions"}],"predecessor-version":[{"id":13679,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/13674\/revisions\/13679"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=13674"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=13674"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=13674"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}