{"id":6165,"date":"2010-07-20T23:59:40","date_gmt":"2010-07-20T23:59:40","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=6165"},"modified":"2010-07-30T22:34:26","modified_gmt":"2010-07-30T22:34:26","slug":"severe-turbulece-causes-injuries-to-passengers-and-diverts-aircraft","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/6165","title":{"rendered":"Severe turbulence causes injuries to passengers and diverts aircraft"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100720_UAL927_flight_path_2.jpg\"><img loading=\"lazy\" decoding=\"async\" title=\"United Airlines Flight 967 flight track diversion (courtesy of FlightAware.com)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100720_UAL927_flight_path_2.jpg\" alt=\"United Airlines Flight 967 flight track diversion (courtesy of FlightAware.com)\" width=\"480\" height=\"430\" \/><\/a><p class=\"wp-caption-text\">United Airlines Flight 967 flight track diversion (courtesy of FlightAware.com)<\/p><\/div>\n<p>On <strong><a href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20100720.html\">20 July 2010<\/a><\/strong>, United Airlines Flight 967 en route from Washington Dulles  to Los Angeles encountered severe turbulence over the central US, and had to divert and land at Denver to medically treat nearly 30 passengers who suffered significant injuries. The flight track diversion is shown above <em>(courtesy of <a href=\"http:\/\/flightaware.com\/\">FlightAware.com<\/a>)<\/em>.<\/p>\n<p>AWIPS images of 4-km resolution GOES-13 10.7 \u00c2\u00b5m IR channel data <strong><em>(below)<\/em><\/strong> and GOES-13 6.5 \u00c2\u00b5m <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100720_g13_wv_anim.gif\">water vapor channel data<\/a><\/strong> revealed  large clusters of rapidly-developing thunderstorms over Kansas and Missouri during the afternoon and evening hours. The coldest GOES-13 cloud top IR brightness temperature was <strong>-81\u00c2\u00ba C<\/strong> <em>(violet color enhancement)<\/em> at 22:45 UTC. However, it is unclear of the exact location of the turbulence encounter, since AWIPS plotted a SEVERE TURB report from UAL967 at Flight Level 34,000 feet over both <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100720_UAL967_PIREP_1.jpg\">Missouri<\/a><\/strong> and <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100720_UAL967_PIREP_2.jpg\">Kansas<\/a><\/strong>. Some <strong><a href=\"http:\/\/www.foxnews.com\/us\/2010\/07\/20\/united-airlines-flight-diverts-denver-hitting-turbulence-injured-seriously\/\">media reports<\/a><\/strong> suggest that the event occurred over southwestern Missouri.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100720_g13_ir_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-13 10.7 \u00c2\u00b5m IR images + Pilot reports of turbulence\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100720_g13_ir_anim.gif\" alt=\"GOES-13 10.7 \u00c2\u00b5m IR images + Pilot reports of turbulence\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">GOES-13 10.7 \u00c2\u00b5m IR images + Pilot reports of turbulence<\/p><\/div>\n<p>These strong thunderstorms were developing along a <strong><a href=\"..\/wp-content\/uploads\/2010\/07\/Sfc_Fronts_20100720_2100.png\">surface  trough axis just south of a stationary frontal boundary<\/a><\/strong>, where  the <strong><a href=\"..\/wp-content\/uploads\/2010\/07\/100720_g13_sounder_cape_anim.gif\">GOES-13  Sounder CAPE product<\/a><\/strong> indicated that the air mass was quite  unstable. According to the <strong><a href=\"http:\/\/www.spc.noaa.gov\/climo\/reports\/100720_rpts.html\">SPC  Storm Reports<\/a><\/strong>, there were a number of damaging wind reports  associated with these thunderstorms, including surface wind gusts to <strong>70  mph<\/strong> in Missouri and <strong>80 mph<\/strong> in Kansas.<\/p>\n<p>A comparison of 1-km resolution POES AVHRR 10.8 \u00c2\u00b5m IR and 0.63 \u00c2\u00b5m visible images at 22:25 UTC <strong><em>(below)<\/em><\/strong> showed cloud top IR brightness temperatures as cold as <strong>-88\u00c2\u00ba C<\/strong> over Missouri and <strong>-90\u00c2\u00ba C<\/strong> over Kansas <em>(darker violet color enhancement)<\/em>. The visible image revealed tell-tale shadows of overshooting tops from intense updrafts.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100720_avhrr_vis_ir_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"POES AVHRR 10.8 \u00c2\u00b5m IR image + 0.63 \u00c2\u00b5m visible image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100720_avhrr_vis_ir_anim.gif\" alt=\"POES AVHRR 10.8 \u00c2\u00b5m IR image + 0.63 \u00c2\u00b5m visible image\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">POES AVHRR 10.8 \u00c2\u00b5m IR image + 0.63 \u00c2\u00b5m visible image<\/p><\/div>\n<p>1-km resolution GOES-13 0.63 \u00c2\u00b5m visible channel images <strong><em>(below)<\/em><\/strong> also showed a number of overshooting tops associated with these thunderstorms. The <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/KSGF_20100721_0000.png\">rawinsonde report from Springfield, Missouri<\/a><\/strong> indicated a maximum vertical velocity of 73 meters per second!<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100720_g13_vis_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-13 0.63 \u00c2\u00b5m visible channel images + Pilot reports of turbulence\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100720_g13_vis_anim.gif\" alt=\"GOES-13 0.63 \u00c2\u00b5m visible channel images + Pilot reports of turbulence\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">GOES-13 0.63 \u00c2\u00b5m visible channel images + Pilot reports of turbulence<\/p><\/div>\n<p>A closer view using McIDAS images of 1-km resolution GOES-15 and GOES-13 0.63 \u00c2\u00b5m visible channel data <em><strong>(below)<\/strong><\/em> also shows the times of the aircraft positios as it approached the southeastern edge of the thunderstorm anvil.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100720_g15_g13_vis_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-15 (left) and GOES-13 (right) visible channel images (with aircraft position times)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100720_g15_g13_vis_anim.gif\" alt=\"GOES-15 (left) and GOES-13 (right) visible channel images (with aircraft position times)\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-15 (left) and GOES-13 (right) visible channel images (with aircraft position times)<\/p><\/div>\n<p>Examples of two of the <strong><a href=\"http:\/\/cimss.ssec.wisc.edu\/snaap\/convinit\/quicklooks2.php\">SNAAP Convective Storm Monitoring and Nowcasting products<\/a><\/strong> <strong><em>(below)<\/em><\/strong> demonstrate the ability to use satellite data to help detect overshooting tops that might pose increased risks for turbulence.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100720_overshoot_turbrisk_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"SNAAP Overshooting Top + Turbulence Risk satellite products\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100720_overshoot_turbrisk_anim.gif\" alt=\"SNAAP Overshooting Top + Turbulence Risk satellite products\" width=\"480\" height=\"430\" \/><\/a><p class=\"wp-caption-text\">SNAAP Overshooting Top + Turbulence Risk satellite products<\/p><\/div>\n<p>An example of the <strong><a href=\"http:\/\/www.ral.ucar.edu\/projects\/ntda\/\">NCAR Turbulence Detection Algorithm<\/a><\/strong> <strong><em>(below)<\/em><\/strong> showed the potential for turbulence at 36,000 feet across a large portion of Kansas and Missouri.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100721_0115z_ntda.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"NCAR Turbulence Detection Algorithm\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2010\/07\/100721_0115z_ntda.gif\" alt=\"NCAR Turbulence Detection Algorithm\" width=\"480\" height=\"300\" \/><\/a><p class=\"wp-caption-text\">NCAR Turbulence Detection Algorithm<\/p><\/div>\n<p>For additional satellite image analysis of this case, see the <a title=\"VISIT Meteorological Interpretation Blog\" href=\"http:\/\/rammb.cira.colostate.edu\/visit\/blog\/index.php\/2010\/07\/29\/united-airlines-flight-967-severe-turbulence-july-20-2010\/\" target=\"_blank\"><strong>VISIT Meteorological Interpretation Blog<\/strong><\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>On 20 July 2010, United Airlines Flight 967 en route from Washington Dulles to Los Angeles encountered severe turbulence over the central US, and had to divert and land at Denver to medically treat nearly 30 passengers who suffered significant injuries. The flight track diversion is shown above (courtesy of FlightAware.com). AWIPS images of 4-km [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[22,21,15,11,43,26,3],"tags":[],"class_list":["post-6165","post","type-post","status-publish","format-standard","hentry","category-avhrr","category-aviation","category-goes-sounder","category-goes-13","category-goes-15","category-poes","category-severe-convection"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/6165","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=6165"}],"version-history":[{"count":33,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/6165\/revisions"}],"predecessor-version":[{"id":6267,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/6165\/revisions\/6267"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=6165"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=6165"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=6165"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}