{"id":23545,"date":"2017-03-23T19:38:49","date_gmt":"2017-03-23T19:38:49","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=23545"},"modified":"2017-03-25T22:27:29","modified_gmt":"2017-03-25T22:27:29","slug":"goes-16-cirrus-channel-and-dust","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/23545","title":{"rendered":"GOES-16 Cirrus Channel and Dust"},"content":{"rendered":"

\"GOES-16<\/a>

GOES-16 Visible (0.64 \u00b5m) images, 2132-2232 UTC on 23 March [click to play animated gif]<\/p><\/div>GOES-16 data posted on this page are preliminary, non-operational data that are undergoing testing.<\/strong><\/p>\n

The visible animation from late afternoon over west Texas, above, shows a characteristic signature of a shroud of dust around El Paso, TX behind a dryline associated with a developing cyclone<\/a> in the lee of the Rocky Mountains. This pall of dust was visible in many of the 16 channels on the Advanced Baseline Imager (ABI) that sits on GOES-16. The toggle below cycles through the Red visible (0.64 \u00b5m), the Blue visible (0.47 \u00b5m), the Cirrus channel (1.38 \u00b5m), the Snow\/ice channel (1.61 \u00b5m) and the Upper-Level and Lower-Level water vapor channels (6.19 \u00b5m and 7.34 \u00b5m, respectively) (Click here<\/a> for a faster image toggle). In\u00a0 addition, a 2-panel comparison of GOES-16 Visible and Cirrus band imagery is available here<\/a>.<\/p>\n

\"GOES-16<\/a>

GOES-16 Visible (0.64 \u00b5m and 0.47 \u00b5m), Cirrus (1.38 \u00b5m), Snow\/Ice (1.61 \u00b5m), Upper level Water Vapor (6.19 \u00b5m) and Lower Level Water Vapor (7.34 \u00b5m) images, 2132 UTC on 23 March [click to enlarge]<\/p><\/div>Several aspects of the toggle above bear comment. Note that the blue channel<\/a> (0.47 \u00b5m) has in general a ‘hazier’ appearance than the 0.64 \u00b5m red channel<\/a>. Atmospheric scattering is more important at shorter wavelengths, and that is picked up by the satellite. The 1.38 \u00b5m ‘Cirrus’ Channel<\/a> generally does not see the surface because of water vapor absorption at that wavelength. However, the atmosphere behind the dry line is sufficiently parched (total Precipitable Water in the El Paso sounding on 0000 UTC 24 March<\/a> is less than 6 mm; sounding from this site<\/a>) that complete attenuation by water vapor is not occurring; dust is highly reflective at 1.38 \u00b5m and a signal becomes apparent in the dry air from west Texas southwestward into central Mexico.<\/p>\n

Thin dust is very difficult to detect in the 1.61 \u00b5m snow\/ice channel<\/a> because solar energy at that wavelength reflected from the surface moves unimpeded through thin dust; thus you can generally see the surface in dusty regions in the 1.61 \u00b5m channel. On this date the 1.61 \u00b5m channel<\/a> nimbly discriminated between water clouds (over central Mexico) and ice clouds (over much of the rest of the domain, as shown in this toggle<\/a> between 0.64 \u00b5m<\/a> and 1.61 \u00b5m<\/a> : only the clouds composed of water are reflective (white) in both channels.<\/p>\n

The atmosphere was sufficiently dry on this date that the lower-level (7.34 \u00b5m<\/a>) water vapor channel detected surface features (horizontal convective rolls) associated with the blowing dust. (click here<\/a> for the 6.19 \u00b5m image; surface features are not so apparent). Weighting functions computed at those wavelengths<\/a> show a significant contribution from the surface at 7.4 \u00b5m (the red line), and also at 7.0 \u00b5m, (the green line), so the mid-level water vapor imagery from GOES-16 likely also shows surface influences); the 6.5 \u00b5m weighting function (the blue line) does not extend to the surface (These GOES-13 Sounder Weighting Functions that are similar to those from the GOES-16 ABI are from this site<\/a>) so it’s unlikely that the 6.19 \u00b5m imagery shows surface features.<\/p>\n

The GOES-R Website<\/a> has fact sheets on the 0.47 \u00b5m<\/a>, 0.64 \u00b5m<\/a>, 1.38 \u00b5m<\/a>, 1.61 \u00b5m<\/a>, 6.19 \u00b5m <\/a>and 7.34 \u00b5m<\/a> channels.<\/p>\n

Added: The RAMSDIS GOES-16 Loop of the Day<\/a> from 23 March showed the Dust RGB product<\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"

GOES-16 data posted on this page are preliminary, non-operational data that are undergoing testing. The visible animation from late afternoon over west Texas, above, shows a characteristic signature of a shroud of dust around El Paso, TX behind a dryline associated with a developing cyclone in the lee of the Rocky Mountains. This pall of […]<\/p>\n","protected":false},"author":19,"featured_media":23558,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[74],"tags":[],"class_list":["post-23545","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-16"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/23545","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\/19"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=23545"}],"version-history":[{"count":15,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/23545\/revisions"}],"predecessor-version":[{"id":23566,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/23545\/revisions\/23566"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/23558"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=23545"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=23545"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=23545"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}