{"id":157,"date":"2006-10-02T20:48:29","date_gmt":"2006-10-02T20:48:29","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/2006\/10\/02\/final-day-of-goes-10-srso\/"},"modified":"2006-10-03T22:38:00","modified_gmt":"2006-10-03T22:38:00","slug":"final-day-of-goes-10-srso","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/157","title":{"rendered":"Final day of GOES-10 SRSO"},"content":{"rendered":"<p>Beginning on 23 August, the GOES-10 satellite was placed into continuous Super Rapid Scan Operations (<strong>SRSO<\/strong>) mode, providing images at 1-minute intervals over a limited region of the US. <a title=\"02 October Daily Weather Map\" target=\"_blank\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20061002.html\"><strong>02 October<\/strong><\/a> was the final day of GOES-10 SRSO, and some of the interesting features that were apparent on the visible channel imagery included:<\/p>\n<p><a title=\"GOES-10 visible animation\" target=\"_blank\" href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/misc\/blog\/061002_g10_vis_distrail.mov\"><img decoding=\"async\" align=\"middle\" alt=\"GOES-10 visible animation\" id=\"image153\" title=\"GOES-10 visible animation\" style=\"width: 480px; height: 360px\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2006\/10\/061002_g10_vis_distrail_20.GIF\" \/><\/a><br \/>\n(1) a distinct &#8220;aircraft dissipation trail&#8221; <span style=\"font-weight: bold; font-style: italic\"><a target=\"_blank\" title=\"GOES-10 visible animaiton\" href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/misc\/blog\/061002_g10_vis_distrail.mov\">(10 MB QuickTime animation, above)<\/a> <\/span>running north-south through a patch of cloudiness located over northeastern Kansas. GOES-12 10.7 micrometer cloud top temperatures in that particular cloud feature were in the <a title=\"AWIPS GOES-12 10.7 \u00c2\u00b5m image\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2006\/10\/061002_distrail_ir4_ir2_2.jpg\"><strong>-25 to -35 C range,<\/strong><\/a> and GOES Sounder Cloud Top Heights were generally <a title=\"AWIPS GOES Sounder Cloud Top Height\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2006\/10\/061002_distrail_sounder_cth.jpg\"><strong>25-30 Kft<\/strong><\/a>, suggestive of cirrus clouds that were likely composed of ice particles; the MODIS Cloud Phase product a few hours later did in fact indicate <a title=\"AWIPS MODIS Cloud Phase product\" target=\"_blank\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2006\/10\/061002_distrail_modis_phase.jpg\"><strong>mostly ice phase<\/strong><\/a> in that area of cloudiness as it moved eastward across the Kansas\/Missouri border region. Small particles in the aircraft exhaust may have  acted as effective ice condensation nuclei, causing the cloud ice particles to grow and begin falling out of the cloud (creating the aircraft dissipation trail signature);<br \/>\n<a title=\"GOES-10 visible animation\" target=\"_blank\" href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/misc\/blog\/061002_g10_vis_fog.mov\"><img decoding=\"async\" align=\"middle\" alt=\"GOES-10 visible animation\" id=\"image154\" title=\"GOES-10 visible animation\" style=\"width: 480px; height: 360px\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2006\/10\/061002_g10_fog_vis_30.GIF\" \/><\/a><br \/>\n(2) morning dissipation of valley fog <a target=\"_blank\" title=\"GOES-10 visible animation\" href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/misc\/blog\/061002_g10_vis_fog.mov\"><em><strong>(12 MB QuickTime animation, above)<\/strong><\/em><\/a> over parts of the central Appalachian Mountains region (<strong><a target=\"_blank\" title=\"GOES-10 visible image with map\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2006\/10\/061002_g10_fog_vis_map.GIF\">map overlay<\/a><\/strong>);<\/p>\n<p><a title=\"GOES-10 visible animation\" target=\"_blank\" href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/misc\/blog\/061002_g10_vis_trw.mov\"><img loading=\"lazy\" decoding=\"async\" width=\"479\" height=\"368\" align=\"middle\" alt=\"GOES-10 visible animation\" id=\"image159\" title=\"GOES-10 visible animation\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2006\/10\/061002_g10_vis_trw_200.GIF\" \/><\/a><br \/>\n(3) development of severe convection over northern Illinois and southern Wisconsin  <a target=\"_blank\" title=\"GOES-10 visible animation\" href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/misc\/blog\/061002_g10_vis_trw.mov\"><em><strong>(36 MB QuickTime animation, above)<\/strong><\/em><\/a> which produced numerous reports of heavy rain, hail, and damaging winds (<a target=\"_blank\" title=\"SPC storm reports\" href=\"http:\/\/www.spc.noaa.gov\/climo\/reports\/061002_rpts.html\"><strong>SPC storm reports<\/strong><\/a>).<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Beginning on 23 August, the GOES-10 satellite was placed into continuous Super Rapid Scan Operations (SRSO) mode, providing images at 1-minute intervals over a limited region of the US. 02 October was the final day of GOES-10 SRSO, and some of the interesting features that were apparent on the visible channel imagery included: (1) a [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[10,14,3],"tags":[],"class_list":["post-157","post","type-post","status-publish","format-standard","hentry","category-general-interpretation","category-goes-10","category-severe-convection"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/157","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=157"}],"version-history":[{"count":0,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/157\/revisions"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=157"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=157"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=157"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}