{"id":13722,"date":"2013-08-21T21:48:24","date_gmt":"2013-08-21T21:48:24","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=13722"},"modified":"2013-08-22T19:05:23","modified_gmt":"2013-08-22T19:05:23","slug":"srso-r-imagery-of-convection-over-the-upper-midwest","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/13722","title":{"rendered":"SRSO-R Imagery of convection over the Upper Midwest"},"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_VIS_21AUG2013loop.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"GOES-14 0.63 \u00c2\u00b5m visible channel images (click image to play animation)\" alt=\"GOES-14 0.63 \u00c2\u00b5m visible channel images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/08\/GOES14_VIS_21AUG2013_2032.GIF\" width=\"480\" height=\"280\" \/><\/a><p class=\"wp-caption-text\">GOES-14 0.63 \u00c2\u00b5m visible channel images (click image to play animation)<\/p><\/div>\n<p>A cold front moving through Wisconsin triggered severe convection (<a title=\"SPC storm reports\" href=\"http:\/\/www.spc.noaa.gov\/climo\/reports\/130821_rpts.html\">SPC storm reports<\/a>) on 21 August 2013. <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/srsor2013\/GOES-14_SRSOR.html\">GOES-14 SRSO-R <\/a> data gives a compelling look at the convective development at 1-minute intervals. Because of the satellite position, the rear inflow into the convection near Rice Lake, WI, is very apparent.<\/p>\n<p>It is useful to compare the SRSO-R views of the convection from GOES-14 (30-second imagery will be available with GOES-R) to the routine scanning strategy used by GOES-13. That comparison is shown below. Routine scanning is unable to capture the very dynamic nature of rapidly evolving convection.<\/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\/GOES1314_VIS_21AUG2013loop.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"GOES-14 (left, SRSO-R) and GOES-13 (right) 0.63 \u00c2\u00b5m visible channel images (click image to play animation)\" alt=\"GOES-14 (left, SRSO-R) and GOES-13 (right) 0.63 \u00c2\u00b5m visible channel images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/08\/GOES1314_VIS_21AUG2013_2032.GIF\" width=\"480\" height=\"280\" \/><\/a><p class=\"wp-caption-text\">GOES-14 (left, SRSO-R) and GOES-13 (right) 0.63 \u00c2\u00b5m visible channel images (click image to play animation)<\/p><\/div>\n<p>Even Rapid Scan Operations (RSO) imagery (GOES-13 was in RSO during this event) can also miss important details, especially at times when GOES-East is doing a full-disk scan (at 20:45 UTC, for example) and no imagery is available for 30 minutes. The loop below compares SRSO views of this system (top) to RSO (middle) to standard 15-minute scanning (bottom). GOES-R will have the capability simultaneously to scan globally and in designated mesoscale sectors.<\/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_SRSO_VIS_21AUG2013loop.gif\"><img loading=\"lazy\" decoding=\"async\" class=\" \" title=\"GOES-14 (SRSO-R, top; RSO, middle; standard, bottom) 0.63 \u00c2\u00b5m visible channel images (click image to play animation)\" alt=\"GOES-14 (SRSO-R, top; RSO, middle; standard, bottom) 0.63 \u00c2\u00b5m visible channel images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/08\/GOES14_SRSO_VIS_21AUG2013_2032.GIF\" width=\"480\" height=\"280\" \/><\/a><p class=\"wp-caption-text\">GOES-14 (SRSO-R, top; RSO, middle; standard, bottom) 0.63 \u00c2\u00b5m visible channel images (click image to play animation)<\/p><\/div>\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\/130821_g13_sounder_li_WI_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"  \" title=\"GOES-13 Sounder DPI values of Lifted Index (click image to play animation)\" alt=\"GOES-13 Sounder DPI values of Lifted Index (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/08\/NA_GOES_Sounder_DPI_LI_20130821_2000.png\" width=\"480\" height=\"280\" \/><\/a><p class=\"wp-caption-text\">GOES-13 Sounder DPI values of Lifted Index (click image to play animation)<\/p><\/div>\n<p>GOES-13 sounder Derived Product Imagery (DPI) of the Lifted Index (above, available at <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/rt\/viewdata.php?product=lia_us\">this site<\/a>) and Convective Available Potential Energy (below) readily shows the unstable airmass supporting the convection.<\/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\/130821_g13_sounder_cape_WI_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"  \" title=\"GOES-13 sounder Convective Available Potential Energy (CAPE) product (click image to play animation)\" alt=\"GOES-13 sounder Convective Available Potential Energy (CAPE) product (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/08\/GOES_CAPE_20130821_2000.png\" width=\"480\" height=\"280\" \/><\/a><p class=\"wp-caption-text\">GOES-13 sounder Convective Available Potential Energy (CAPE) product (click image to play animation)<\/p><\/div>\n<p>Total Precipitable Water (available at <a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/rt\/viewdata.php?product=pwa_us\">this site<\/a>), below, shows moisture pooling along the <a title=\"GOES-13 sounder TPW with surface cold front analysis\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/08\/Sfc_Fronts_20130821_1800.png\">approaching front<\/a>.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/08\/130821_g13_sounder_tpw_WI_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"  \" title=\"GOES-13 Sounder DPI values of Total Precipitable Water\" alt=\"GOES-13 Sounder DPI values of Total Precipitable Water\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2013\/08\/NA_GOES_Sounder_DPI_TPW_20130821_2000.png\" width=\"480\" height=\"280\" \/><\/a><p class=\"wp-caption-text\">GOES-13 Sounder DPI values of Total Precipitable Water<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>A cold front moving through Wisconsin triggered severe convection (SPC storm reports) on 21 August 2013. GOES-14 SRSO-R data gives a compelling look at the convective development at 1-minute intervals. Because of the satellite position, the rear inflow into the convection near Rice Lake, WI, is very apparent. It is useful to compare the SRSO-R [&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":[15,11,40,34],"tags":[],"class_list":["post-13722","post","type-post","status-publish","format-standard","hentry","category-goes-sounder","category-goes-13","category-goes-14","category-goes-r"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/13722","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=13722"}],"version-history":[{"count":14,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/13722\/revisions"}],"predecessor-version":[{"id":13742,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/13722\/revisions\/13742"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=13722"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=13722"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=13722"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}