{"id":23748,"date":"2017-04-13T15:59:25","date_gmt":"2017-04-13T15:59:25","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=23748"},"modified":"2017-04-16T00:34:18","modified_gmt":"2017-04-16T00:34:18","slug":"mountain-waves-over-the-sierra-nevada","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/23748","title":{"rendered":"Mountain waves over the Sierra Nevada"},"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\/2017\/04\/170413_goes16_water_vapor_CA_NV_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2017\/04\/960x427_GOES16FL_B1098_G16_WV_3PANEL_CA_NV_13APR2017_2017103_125218_0003PANELS.GIF\" alt=\"GOES-16 7.3 \u00b5m (left), 6.9 \u00b5m (center) and 6.2 \u00b5m (right) Water Vapor images [click to play animation]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-16 7.3 \u00b5m (left), 6.9 \u00b5m (center) and 6.2 \u00b5m (right) Water Vapor images [click to play animation]<\/p><\/div><em>\u00a0** The GOES-16 data posted on this page are preliminary, non-operational data and are undergoing testing. **<\/em><\/p>\n<p>A comparison of GOES-16 Lower-level (<a href=\"http:\/\/www.goes-r.gov\/education\/docs\/ABI-bands-FS\/ABIBand10_LowerLevel_WV-IR_FINAL.pdf\"><strong>7.3 \u00b5m<\/strong><\/a>), Mid-level (<a href=\"http:\/\/www.goes-r.gov\/education\/docs\/ABI-bands-FS\/ABIBand9_MidLevelWV_IR_FINAL.pdf\"><strong>6.9 \u00b5m<\/strong><\/a>) and Upper-level <a href=\"http:\/\/www.goes-r.gov\/education\/docs\/ABI-bands-FS\/ABIBand8UpperLevelWVFINAL.pdf\"><strong>(6.2 \u00b5m<\/strong><\/a>) Water Vapor images<em><strong> (above)<\/strong> <\/em>revealed the presence of numerous mountain waves over parts of California and Nevada on <a href=\"http:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20170413.html\"><strong>13 April 2017<\/strong><\/a>. The more pronounced of these waves were caused by strong southwesterly winds interacting with\u00a0 higher terrain of the <a href=\"https:\/\/en.wikipedia.org\/wiki\/Sierra_Nevada_%28U.S.%29\"><strong>Sierra Nevada<\/strong><\/a>.<\/p>\n<p>A 3-satellite comparison of GOES-15<em> (GOES-West),<\/em> GOES-16 and GOES-13<em> (GOES-East)<\/em> Water Vapor images<em><strong> (below)<\/strong> <\/em>highlighted 2 factors that allowed better detection of these mountain waves by GOES-16 &#8212; improved spatial resolution (2 km for GOES-16 at satellite sub-point, vs 4 km for GOES-15\/13), and a more direct satellite viewing angle (GOES-16 is positioned at 105\u00baW longitude, while GOES-15 is at 135\u00baW and GOES-13 is at 75\u00baW).<\/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\/2017\/04\/170413_goes15_goes16_goes13_water_vapor_pireps_CA_NV_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2017\/04\/G15_G16_G13_WV_CA_NV_13APR2017_960x427_B393_00219_2017103_130000_0003PANELS.GIF\" alt=\"OES-15 (6.5 \u00b5m, left), GOES-16 (6.9 \u00b5m, center) and GOES-13 (6.5 \u00b5m, right) Water Vapor images [click to play animation]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-15 (6.5 \u00b5m, left), GOES-16 (6.9 \u00b5m, center) and GOES-13 (6.5 \u00b5m, right) Water Vapor images [click to play animation]<\/p><\/div>Note that there were no Visible cloud features associated with many of the waves seen on Water Vapor imagery<em><strong> (below);<\/strong><\/em> encounters of Clear Air Turbulence (CAT) often occur with these types of mountain waves, as seen by scattered pilot reports of moderate turbulence (plotted as Category 4).<\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2017\/04\/170413_goes16_visible_water_vapor_pireps_CA_NV_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2017\/04\/958x638_AGOES16_B29_G16_VIS_WV_PIREPS_CA_NV_13APR2017_2017103_224218_0002PANELS.GIF\" alt=\"GOES-16 Visible (0.64 \u00b5m, left) and Water Vapor (6.9 \u00b5m, right) images, with pilot reports of turbulence [click to play animation]\" width=\"640\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Visible (0.64 \u00b5m, left) and Water Vapor (6.9 \u00b5m, right) images, with pilot reports of turbulence [click to play animation]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>\u00a0** The GOES-16 data posted on this page are preliminary, non-operational data and are undergoing testing. ** A comparison of GOES-16 Lower-level (7.3 \u00b5m), Mid-level (6.9 \u00b5m) and Upper-level (6.2 \u00b5m) Water Vapor images (above) revealed the presence of numerous mountain waves over parts of California and Nevada on 13 April 2017. The more pronounced [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":23752,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[21,11,43,74],"tags":[],"class_list":["post-23748","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-aviation","category-goes-13","category-goes-15","category-goes-16"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/23748","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=23748"}],"version-history":[{"count":7,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/23748\/revisions"}],"predecessor-version":[{"id":23756,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/23748\/revisions\/23756"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/23752"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=23748"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=23748"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=23748"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}