{"id":58028,"date":"2024-03-29T22:59:00","date_gmt":"2024-03-29T22:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=58028"},"modified":"2024-04-01T19:31:15","modified_gmt":"2024-04-01T19:31:15","slug":"united-airlines-flight-85-diverted-after-encountering-extreme-turbulence-which-injured-22-passengers","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/58028","title":{"rendered":"United Airlines Flight 85 diverted after encountering severe turbulence (which injured 22 passengers)"},"content":{"rendered":"<div style=\"width: 1031px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/240329_ual85_flight_path_altitude_speed.png\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/240329_ual85_flight_path_altitude_speed.png\" alt=\"\" width=\"1021\" height=\"841\" \/><\/a><p class=\"wp-caption-text\">Final flight path of UAL85 (top) with plots of aircraft altitude and speed during its entire flight (bottom), from FlightAware.com<\/p><\/div>\n<p>United Airlines Flight 85 (UAL85) encountered severe turbulence as it was on approach to landing at Newark Liberty International Airport (KEWR) &#8212; which injured 22 passengers, with 7 of those being transported to a hospital (<a href=\"https:\/\/simpleflying.com\/22-injured-united-airlines-boeing-787-10-dreamliner-severe-turbulence\/\"><strong>media report 1<\/strong><\/a> | <a href=\"https:\/\/www.upi.com\/Top_News\/US\/2024\/03\/30\/united-airlines-severe-turbulence-passengers-injured\/9011711831394\/\"><strong>media report 2<\/strong><\/a>) late in the day on <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20240329.html\"><strong>29 March 2024<\/strong><\/a>. Gusty NW winds may have contributed to the turbulence (which likely occurred around 2138 UTC, according to <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/240329_ual85_flight_data.png\"><strong>flight data<\/strong><\/a> from <a href=\"https:\/\/www.flightaware.com\/\"><strong>FlightAware<\/strong><\/a> &#8212; note the rapid rate of ascent beginning at that time); the peak wind gust at KEWR was <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/240329_kewr_metar.text\"><strong>48 knots<\/strong><\/a> or 55 mph at 2039 UTC. After UAL85 aborted its landing at KEWR, it diverted north to New York Stewart International Airport (KSWF), landing at 2208 UTC <em><strong>(above)<\/strong><\/em>.<\/p>\n<p>1-minute <a href=\"https:\/\/www.nco.ncep.noaa.gov\/status\/satellite\/\"><strong>Mesoscale Domain Sector<\/strong><\/a> GOES-16 <em>(GOES-East)<\/em> Low-level Water Vapor (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band10.pdf\"><strong>7.3 \u00b5m<\/strong><\/a>) images <em><strong>(below)<\/strong><\/em> depicted widespread mountain waves across southeastern New York and northern New Jersey during that time. These mountain waves could also have played a role in creating boundary layer turbulence. The Pilot Report (PIREP) for this UAL85 incident did not appear in the real-time AWIPS data, probably due to time restraints imposed upon the flight crew to get the aircraft safely diverted as quickly as possible.<\/p>\n<p><div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/240329_goes16_waterVapor_NY_NJ_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/ny_wv-20240329_213823.png\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">1-minute GOES-16 Low-level Water Vapor (7.3 \u00b5m) images, from 2100-2200 UTC on 29 March [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/240329_goes16_waterVapor_NY_NJ_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>In a faster animation of GOES-16 Water Vapor images without plots of surface reports <em><strong>(below)<\/strong><\/em>, note that the mountain wave structure across northern New Jersey (including near KEWR) becomes slightly deformed, and even begins to move westward a few miles.<\/p>\n<p><div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/240329_goes16_waterVapor_NY_NJ_nometar_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/ny_wv_nometar-20240329_213823.png\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">1-minute GOES-16 Low-level Water Vapor (7.3 \u00b5m) images, from 2040-2200 UTC on 29 March [click to play animated GIF | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/240329_goes16_waterVapor_NY_NJ_nometar_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>A toggle between GOES-16 Water Vapor imagery and Topography <em><strong>(below)<\/strong><\/em> indicated that these mountain waves were forming downwind of the <a href=\"https:\/\/en.wikipedia.org\/wiki\/Catskill_Mountains\"><strong>Catskills<\/strong><\/a> in New York and the <a href=\"https:\/\/en.wikipedia.org\/wiki\/Pocono_Mountains\"><strong>Poconos<\/strong><\/a> in Pennsylvania.<\/p>\n<p><div style=\"width: 1725px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/240329_2138utc_goes16_waterVapor_topography_NY_NJ_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/240329_2138utc_goes16_waterVapor_topography_NY_NJ_anim.gif\" width=\"1715\" height=\"830\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Low-level Water Vapor (7.3 \u00b5m) image + Topography [click to enlarge]<\/p><\/div>Plots of rawinsonde data from Albany NY and Upton NY <em><strong>(below)<\/strong><\/em> both showed adiabatic or near-adiabatic lapse rates below the 800-850 hPa pressure level &#8212; which aided in the downward transport of momentum (stronger winds) aloft to the surface earlier in the day.<\/p>\n<div style=\"width: 1290px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/240330_0000UTC_KALB_RAOB.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/240330_0000UTC_KALB_RAOB.GIF\" width=\"1280\" height=\"960\" \/><\/a><p class=\"wp-caption-text\">Plot of rawinsonde data from Albany NY at 0000 UTC on 30 March [click to enlarge]<\/p><\/div>\n<div style=\"width: 1290px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/240330_0000UTC_KOKX_RAOB.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2024\/03\/240330_0000UTC_KOKX_RAOB.GIF\" width=\"1280\" height=\"960\" \/><\/a><p class=\"wp-caption-text\">Plot of rawinsonde data from Upton NY at 0000 UTC on 30 March [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>United Airlines Flight 85 (UAL85) encountered severe turbulence as it was on approach to landing at Newark Liberty International Airport (KEWR) &#8212; which injured 22 passengers, with 7 of those being transported to a hospital (media report 1 | media report 2) late in the day on 29 March 2024. Gusty NW winds may have [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":58040,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[21,74],"tags":[],"class_list":["post-58028","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-aviation","category-goes-16"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/58028","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=58028"}],"version-history":[{"count":31,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/58028\/revisions"}],"predecessor-version":[{"id":58088,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/58028\/revisions\/58088"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/58040"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=58028"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=58028"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=58028"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}