{"id":39140,"date":"2020-12-05T23:59:12","date_gmt":"2020-12-05T23:59:12","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=39140"},"modified":"2020-12-07T04:40:41","modified_gmt":"2020-12-07T04:40:41","slug":"signatures-of-the-alaska-range-on-water-vapor-imagery","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/39140","title":{"rendered":"Signatures of the Alaska Range on Water Vapor imagery"},"content":{"rendered":"

\"GOES-17<\/a>

GOES-17 Low-level (7.3 \u00b5m),<\/em> Mid-level (6.9 \u00b5m)<\/em> and Upper-level (6.2 \u00b5m)<\/em> Water Vapor images, with topography [click to play animation | MP4<\/strong><\/a>]<\/p><\/div>GOES-17 (GOES-West)<\/em> Low-level (7.3 \u00b5m<\/strong><\/a>), Mid-level (6.9 \u00b5m<\/strong><\/a>) and Upper-level (6.2 \u00b5m<\/strong><\/a>) Water Vapor images (above)<\/strong><\/em> revealed cold thermal signatures (brighter shades of white)<\/em> associated with the highest-elevation portions of the Alaska Range on 05 December 2020. Note the slight northward shift (16-20 km, or 10-12 miles) in the apparent location of Denali in the GOES-17 images, due to parallax<\/strong><\/a>.<\/p>\n

Plots of GOES-17 Water Vapor (ABI<\/strong><\/a> spectral band 8, 9 and 10) weighting functions<\/strong><\/a> calculated using 00 UTC rawinsonde data from Fairbanks<\/strong><\/a> (north of the Alaska Range)<\/em> and from Anchorage<\/strong><\/a> (south of the Alaska Range)<\/em> are shown below. Even with very large satellite viewing angles (or zenith angles) greater than 70 degrees \u2014 which would tend to shift the Water Vapor weighting function plots to higher<\/em> altitudes \u2014\u00a0 the presence of very dry air within much of the middle to upper troposphere had the effect of bringing the weighting function peaks downward<\/em>\u00a0to pressure levels corresponding to those of the higher elevations of the Alaska Range.<\/p>\n

\"GOES-17<\/a>

GOES-17 Water Vapor weighting functions, calculated using 00 UTC rawinsonde data from Fairbanks<\/strong> [click to enlarge]<\/p><\/div>

\"GOES-17<\/a>

GOES-17 Water Vapor weighting functions, calculated using 00 UTC rawinsonde data from Anchorage<\/strong> [click to enlarge]<\/p><\/div>The Total Precipitable Water (TPW) values seen on the 00 UTC Fairbanks and Anchorage soundings were 0.07 inch. However, a NOAA-20 NUCAPS sounding profile just 20-30 miles southwest of Denali around 12 UTC (below)<\/strong><\/em> yielded TPW values of only 0.01 inch. The green color of that sounding point indicated successful retrievals from both the Cross-track Infrared Sounder (CrIS<\/strong><\/a>) and Advanced Technology Microwave Sounder (ATMS<\/strong><\/a>) instruments.<\/p>\n

\"GOES-17

GOES-17 Water Vapor (6.9 \u00b5m)<\/em> image, with plots of available 12 UTC NOAA-20 NUCAPS sounding points [click to enlarge]<\/p><\/div>

\"NOAA-20<\/a>

NOAA-20 NUCAPS profile just southwest of Denali around 12 UTC [click to enlarge]<\/p><\/div>Another NOAA-20 NUCAPS green sounding profile just southwest of Denali around 22 UTC (below)<\/strong> <\/em>also yielded a TPW value of only 0.01 inch.<\/p>\n

\"GOES-17<\/a>

GOES-17 Water Vapor (6.9 \u00b5m)<\/em> image, with plots of available 22 UTC NOAA-20 NUCAPS sounding points [click to enlarge]<\/p><\/div>

\"NOAA-20<\/a>

NOAA-20 NUCAPS profile just southwest of Denali around 22 UTC [click to enlarge]<\/p><\/div><\/p>\n","protected":false},"excerpt":{"rendered":"

GOES-17 (GOES-West) Low-level (7.3 \u00b5m), Mid-level (6.9 \u00b5m) and Upper-level (6.2 \u00b5m) Water Vapor images (above) revealed cold thermal signatures (brighter shades of white) associated with the highest-elevation portions of the Alaska Range on 05 December 2020. Note the slight northward shift (16-20 km, or 10-12 miles) in the apparent location of Denali in the […]<\/p>\n","protected":false},"author":18,"featured_media":39145,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[80,78,83],"tags":[],"class_list":["post-39140","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-17","category-noaa-20","category-nucaps"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/39140","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=39140"}],"version-history":[{"count":5,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/39140\/revisions"}],"predecessor-version":[{"id":39146,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/39140\/revisions\/39146"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/39145"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=39140"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=39140"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=39140"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}