{"id":26745,"date":"2018-01-12T23:59:32","date_gmt":"2018-01-12T23:59:32","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=26745"},"modified":"2018-01-16T14:52:45","modified_gmt":"2018-01-16T14:52:45","slug":"severe-turbulence-over-hawaii","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/26745","title":{"rendered":"Severe turbulence over Hawai&#8217;i"},"content":{"rendered":"<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/180112_goes15_water_vapor_HI_turbulence_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/G15_WATER_VAPOR_HI_TURB_12JAN2018_EXP_960x1280_B3_2018012_234500_0001PANEL_00029.GIF\" alt=\"GOES-15 Water Vapor (6.5 \u00b5m) images, with hourly pilot reports of turbulence [click to play animation]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-15 Water Vapor<em> (6.5 \u00b5m)<\/em> images, with hourly pilot reports of turbulence [click to play animation]<\/p><\/div>Numerous pilot reports of moderate to severe turbulence were received over the Hawai&#8217;i area on 12 January 2018 &#8212; and GOES-15<em> (GOES-West)<\/em> Water Vapor (6.5 \u00b5m) images<em><strong> (above;<\/strong> also available as an<strong> <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/180112_goes15_water_vapor_HI_turbulence_anim.mp4\">MP4<\/a>)<\/strong><\/em> showed the development of a quasi-stationary gravity wave train over the northwestern portion of the island chain which appeared to be associated with many of these pilot reports.<\/p>\n<p>HNL UA \/OV 2115N16010W\/TM 2241\/FL320\/TP B767\/<strong>TB CONT MOD TURB<\/strong><\/p>\n<p>HNL UUA \/OV 2115N16048W\/TM 2255\/FL340\/TP H\/B747\/<strong>TB MOD-SEV TURB<\/strong><\/p>\n<p>HNL UUA \/OV BOARD\/TM 2350\/FL370\/TP H\/B772\/<strong>TB SEVERE TURB<\/strong><\/p>\n<p>PHNL UUA \/OV 2443N 15516W \/TM 2358 \/FL370 \/TP B737 \/<strong>TB SEV<\/strong> 370 \/RM ZOA CWSU AWC-WEB<\/p>\n<p>In spite of the large satellite viewing angle, these waves were also very evident on Himawari-8 Lower-level (7.3 \u00b5m), Mid-level (6.9 \u00b5m) and Upper-level (6.2 \u00b5m) Water Vapor images<em><strong> (below; <\/strong>also available as an <strong><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/180112_himawari8_water_vapor_HI_turbulence_anim.mp4\">MP4<\/a>)<\/strong><\/em>. The 3 Water Vapor bands on the Himawari <a href=\"http:\/\/www.data.jma.go.jp\/mscweb\/en\/himawari89\/space_segment\/spsg_ahi.html\"><strong>AHI<\/strong><\/a> are nearly identical to the 3 Water Vapor bands on the GOES-R series <a href=\"https:\/\/www.goes-r.gov\/spacesegment\/abi.html\"><strong>ABI<\/strong><\/a>.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/180112_himawari8_water_vapor_HI_turbulence_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/HIM08_WATER_VAPOR_HI_TB_12JAN2018_EXP_960x427_B1098_2018012_235000_0003PANELS_00048.GIF\" alt=\"Himawari-8 Low-level (7.3 \u00b5m, left), Mid-level (6.9 \u00b5m, center) and 6.2 \u00b5m, right) Water Vapor images, with hourly pilot reports of turbulence [click to play animation]\" width=\"640\" height=\"479\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 Low-level <em>(7.3 \u00b5m, left),<\/em> Mid-level <em>(6.9 \u00b5m, center)<\/em> and Upper-level <em>(6.2 \u00b5m, right)<\/em> Water Vapor images, with hourly pilot reports of turbulence [click to play animation]<\/p><\/div>A toggle between 1-km resolution Terra MODIS Water Vapor (6.7 \u00b5m), Infrared Window (11.0 \u00b5m) and 250-meter resolution true-color Red-Green-Blue RGB images at 2106 UTC on 12 January <em><strong>(below)<\/strong> <\/em>showed that no high-altitude clouds were associated with the gravity wave features &#8212; thus, these aircraft encounters were examples of Clear Air Turbulence (CAT).<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/180112_2106utc_terra_modis_water_vapor_infrared_truecolor_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/180112_2106utc_terra_modis_water_vapor_infrared_truecolor_anim.gif\" alt=\"Terra MODIS Water Vapor (6.7 \u00b5m) and True-color RGB images [click to enlarge]\" width=\"640\" height=\"401\" \/><\/a><p class=\"wp-caption-text\">Terra MODIS Water Vapor (6.7 \u00b5m), Infrared Window (11.0 \u00b5m) and true-color RGB images [click to enlarge]<\/p><\/div>A color-enhanced version of the Aqua MODIS Water Vapor (6.7 \u00b5m) image at 0014 UTC on 13 January is shown below (courtesy of Jordan Gerth, CIMSS).<\/p>\n<p><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/aqua-modis-wv-20180113_001400.png\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-26756 aligncenter\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/aqua-modis-wv-20180113_001400-300x249.png\" alt=\"\" width=\"640\" height=\"531\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/aqua-modis-wv-20180113_001400-300x249.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/aqua-modis-wv-20180113_001400-768x636.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/aqua-modis-wv-20180113_001400-1024x848.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/aqua-modis-wv-20180113_001400.png 1673w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><\/a><\/p>\n<p>An AWIPS screen capture<em><strong> (below, <\/strong>courtesy of Robert Bohlin, NWS Honolulu and Jordan Gerth, CIMSS<strong>)<\/strong><\/em> displays a <a href=\"http:\/\/journals.ametsoc.org\/doi\/pdf\/10.1175\/WAF-D-17-0080.1\"><strong>High Pass filter product<\/strong><\/a> along with the 3 individual Himawari-8 Water Vapor band images at 0120 UTC on 13 January.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/180113_0120utc_awips_screen_capture.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/180113_0120utc_awips_screen_capture.jpg\" alt=\"Upper-level Water Vapor (6.2 \u00b5m, upper right), Mid-level Water Vapor (6.9 \u00b5m, lower left) and Lower-level Water Vapor (7.3 \u00b5m, lower right) images [click to enlarge]\" width=\"640\" height=\"421\" \/><\/a><p class=\"wp-caption-text\">Himawari-8 High Pass filter product <em>(6.9 \u00b5m, upper left),<\/em> Upper-level Water Vapor <em>(6.2 \u00b5m, upper right),<\/em> Mid-level Water Vapor <em>(6.9 \u00b5m, lower left)<\/em> and Lower-level Water Vapor <em>(7.3 \u00b5m, lower right)<\/em> images [click to enlarge]<\/p><\/div>It bears mention that the rawinsonde data from Lihue, Hawai&#8217;i at 0000 UTC on 13 January<em><strong> (below)<\/strong><\/em> indicated significant wind shear (both speed and directional) within the 200-300 hPa layer (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/180113_00UTC_LIHUE_RAOB_DATA.TEXT\"><strong>text listing<\/strong><\/a>) &#8212; the layer in which many of the turbulence reports were found.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/180113_00UTC_LIHUE_RAOB.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/180113_00UTC_LIHUE_RAOB.GIF\" alt=\"Rawinsonde data from Lihue, Hawai'i at 00 UTC on 13 January [click to enlarge]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">Rawinsonde data from Lihue, Hawai&#8217;i at 00 UTC on 13 January [click to enlarge]<\/p><\/div>The packet of gravity waves was directly over Lihue <em>(red asterisk)<\/em> at that time<em><strong> (below)<\/strong><\/em>.<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/180113_00UTC_GOES15_WV_PHLI.GIF\"><img loading=\"lazy\" decoding=\"async\" class=\"\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/01\/180113_00UTC_GOES15_WV_PHLI.GIF\" alt=\"GOES-15 Water Vapor (6.5 \u00b5m) image at 0000 UTC on 13 January, with pilot reports of turbulence plotted. The red asterisk denotes the location of Lihue [click to enlarge]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-15 Water Vapor <em>(6.5 \u00b5m)<\/em> image at 0000 UTC on 13 January, with pilot reports of turbulence plotted. The red asterisk denotes the location of Lihue [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>Numerous pilot reports of moderate to severe turbulence were received over the Hawai&#8217;i area on 12 January 2018 &#8212; and GOES-15 (GOES-West) Water Vapor (6.5 \u00b5m) images (above; also available as an MP4) showed the development of a quasi-stationary gravity wave train over the northwestern portion of the island chain which appeared to be associated [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":26749,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[70,21,43,62,12,71],"tags":[],"class_list":["post-26745","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-aqua","category-aviation","category-goes-15","category-himawari-8","category-modis","category-terra"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/26745","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=26745"}],"version-history":[{"count":13,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/26745\/revisions"}],"predecessor-version":[{"id":26761,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/26745\/revisions\/26761"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/26749"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=26745"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=26745"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=26745"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}