{"id":3005,"date":"2009-07-20T23:59:18","date_gmt":"2009-07-20T23:59:18","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=3005"},"modified":"2009-07-22T21:49:31","modified_gmt":"2009-07-22T21:49:31","slug":"rapid-scan-operations-rso-imagery-from-2-satellites","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/3005","title":{"rendered":"Rapid Scan Operations (RSO) imagery from 2 satellites"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/07\/090720_g11_g12_rso_vis_anim.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"GOES-11 and GOES-12 visible images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/07\/090720_g11_g12_rso_vis_anim.gif\" title=\"GOES-11 and GOES-12 visible images\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-11 and GOES-12 visible images<\/p><\/div>\n<p>The National Weather Service forecast office at <strong><a href=\"http:\/\/www.crh.noaa.gov\/cys\/\">Cheyenne WY<\/a><\/strong> requested that both the GOES-11 <em>(GOES-West)<\/em> and the GOES-12 <em>(GOES-East)<\/em> satellites be placed into Rapid Scan Operations (RSO) to monitor severe convection across their County Warning Area (CWA) on <strong><a href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20090720.html\">20 July 2009<\/a><\/strong>:<\/p>\n<blockquote>\n<p>SENIOR DUTY METEOROLOGIST NWS ADMINISTRATIVE MESSAGE<br \/>\nNWS NCEP CENTRAL OPERATIONS CAMP SPRINGS MD<br \/>\n2114Z MON JUL 20 2009<\/p>\n<p>GOES RSO INFO&#8230;<\/p>\n<p>A GOES EAST RSO WILL BE IN EFFECT FROM 2226Z TILL 0426Z<br \/>\nAND GOES WEST RSO WILL BE IN EFFECT FROM 2203Z TILL<br \/>\n0403Z THIS EVENING AS REQUESTED BY WFO CYS \/CHEYENNE\/<br \/>\nWHO IS ON THE CUSP OF THE SATELLITE RSO COVERAGE AREAS<br \/>\nFOR SVR WX MONITORING SUPPORT.<\/p>\n<\/blockquote>\n<p>While there were <strong><a href=\"http:\/\/www.spc.noaa.gov\/climo\/reports\/090720_rpts.html\">reports of hail up to 1.0 inch in diameter<\/a><\/strong> in the Cheyenne CWA, the thunderstorms that developed further to the east over western Nebraska and western Kansas were more severe <em>(producing tornadoes in Kansas, and hail as large as 4.25 inches in diameter in both Kansas and Nebraska)<\/em>. A comparison of GOES-11 and GOES-12 visible images <strong><em>(above)<\/em><\/strong>  shows the view of these storms from each satellite perspective. Note that some features were easier to see from the GOES-11 perspective, which allowed more of a view from the side <em>(to reveal surface boundaries and flanking line development more clearly)<\/em>. <\/p>\n<p>A comparison of GOES-11 and GOES-12 10.7 \u00c2\u00b5m IR images <strong><em>(below)<\/em><\/strong> shows that the development of a distinct &#8220;enhanced-v&#8221; signature was apparent on imagery from both satellites from the 23:00 to 23:11 UTC period. The coldest IR brightness temperatures were -67\u00c2\u00ba C (darker black color enhancement) from both GOES-11 and GOES-12.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/07\/090720_g11_g12_rso_ir_anim.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"GOES-11 amd GOES-12 10.7 \u00c2\u00b5m IR images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/07\/090720_g11_g12_rso_ir_anim.gif\" title=\"GOES-11 amd GOES-12 10.7 \u00c2\u00b5m IR images\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-11 amd GOES-12 10.7 \u00c2\u00b5m IR images<\/p><\/div>\n<p>These thunderstorms appeared to be propagating southward ahead of an advancing cold frontal boundary, and along a decaying stationary frontal boundary that was oriented northwest-to-southeast from western Nebraska into central Kansas. GOES sounder Derived Product Images (DPI) of Lifted Index (LI) and Total Precipitable Water (TPW) <strong><em>(below)<\/em><\/strong> indicated that there was an axis of instability <em>(LI values of -4 to -6 \u00c2\u00ba\u00c2\u00a0C)<\/em> and moisture <em>(TPW values of 20-30 mm, or 0.8 to 1.2 inches)<\/em> along the stationary frontal boundary.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/07\/090720_goes_sounder_li_tpw_anim.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"GOES sounder Lifted Index and Total Precipitable Water products\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/07\/090720_goes_sounder_li_tpw_anim.gif\" title=\"GOES sounder Lifted Index and Total Precipitable Water products\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">GOES sounder Lifted Index and Total Precipitable Water products<\/p><\/div>\n<p>A few hours later, thunderstorms that developed ahead of the advancing cold front in Oklahoma and southern Kansas exhibited cloud top IR brightness temperatures as cold as <strong>-84\u00c2\u00ba C<\/strong> <em>(purple color enhancement)<\/em> on AWIPS imagery of the MODIS 11.0 \u00c2\u00b5m  channel <strong><em> (below)<\/em><\/strong>.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/07\/MODIS_IR_20090721_0411.png\"><img loading=\"lazy\" decoding=\"async\" alt=\"MODIS 11.0 \u00c2\u00b5m IR image + SPC storm reports\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/07\/MODIS_IR_20090721_0411.png\" title=\"MODIS 11.0 \u00c2\u00b5m IR image + SPC storm reports\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">MODIS 11.0 \u00c2\u00b5m IR image + SPC storm reports<\/p><\/div>\n<p><strong><em>===== 21 JULY UPDATE =====<\/em><\/strong><\/p>\n<p>On the following day, MODIS 3.7 \u00c2\u00b5m shortwave IR and MODIS Land Surface Temperature (LST) images <strong><em>(below)<\/em><\/strong> revealed a long swath of rain-cooled ground across far western Kansas. MODIS LST values were in the 75-85\u00c2\u00ba F range <em>(green colors)<\/em> within the swath of rain-cooled ground, in contrast to LST values in excess of 110\u00c2\u00ba F <em>(darker orange colors)<\/em> just to the west.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/07\/090721_modis_swir_lst_anim.gif\"><img loading=\"lazy\" decoding=\"async\" alt=\"MODIS 3.7 \u00c2\u00b5m shortwave IR + MODIS Land Surface Temperature product\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2009\/07\/090721_modis_swir_lst_anim.gif\" title=\"MODIS 3.7 \u00c2\u00b5m shortwave IR + MODIS Land Surface Temperature product\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">MODIS 3.7 \u00c2\u00b5m shortwave IR + MODIS Land Surface Temperature product<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>The National Weather Service forecast office at Cheyenne WY requested that both the GOES-11 (GOES-West) and the GOES-12 (GOES-East) satellites be placed into Rapid Scan Operations (RSO) to monitor severe convection across their County Warning Area (CWA) on 20 July 2009: SENIOR DUTY METEOROLOGIST NWS ADMINISTRATIVE MESSAGE NWS NCEP CENTRAL OPERATIONS CAMP SPRINGS MD 2114Z [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[15,18,19,12,3],"tags":[],"class_list":["post-3005","post","type-post","status-publish","format-standard","hentry","category-goes-sounder","category-goes-11","category-goes-12","category-modis","category-severe-convection"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/3005","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=3005"}],"version-history":[{"count":15,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/3005\/revisions"}],"predecessor-version":[{"id":3029,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/3005\/revisions\/3029"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=3005"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=3005"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=3005"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}