{"id":14036,"date":"2013-09-30T18:59:53","date_gmt":"2013-09-30T18:59:53","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=14036"},"modified":"2013-10-03T21:20:46","modified_gmt":"2013-10-03T21:20:46","slug":"mesospheric-airglow-waves-over-the-atlantic-ocean","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/14036","title":{"rendered":"Mesospheric airglow waves over the Atlantic Ocean"},"content":{"rendered":"
\"Suomi<\/a>

Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band image<\/p><\/div>\n

An AWIPS image of Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band (DNB) data at 06:10 UTC or 2:10 AM local time on 30 September 2013 (above)<\/strong><\/em> revealed multiple signatures of mesospheric airglow waves over portions of the western Atlantic Ocean. There are three distinct packets of waves seen on the DNB image — two of which were likely generated by intense mesoscale convective systems associated with a strong occluding mid-latitude cyclone<\/strong><\/a> centered several hundred miles north-northwest of Bermuda. The impressive length of the third (southernmost) wave packet located southeast of Bermuda can better be seen in the full DNB swath image<\/strong><\/a> (courtesy of Kathy Strabala, SSEC);<\/em> this feature is likely a high-altitude undular bore.<\/p>\n

A comparison of the VIIRS DNB image (and cloud-to-ground lightning strike data)<\/em> with the corresponding VIIRS 11.45 \u00c2\u00b5m IR image (below)<\/strong><\/em> showed that there was no signature of these mesospheric airglow waves on the IR image.<\/p>\n

\"Suomi<\/a>

Suomi NPP VIIRS 11.45 \u00c2\u00b5m IR channel and 0.7 \u00c2\u00b5m Day\/Night Band images, with cloud-to-ground lightning strikes<\/p><\/div>\n

A magnified comparison of VIIRS DNB and IR images (below)<\/strong><\/em> showed the difference between the short wavelength of cloud-top gravity waves propagating southwestward away from an overshooting top (located between the two lightning streaks)<\/em> and the longer-wavelength mesospheric airglow waves seen along and south of the southernmost lightning streak. The DNB image lightning streaks are an artifact of sensor saturation by very bright cloud-top illumination resulting from intense lightning activity.<\/p>\n

\"Suomi<\/a>

Suomi NPP VIIRS 11.45 \u00c2\u00b5m IR and 0.7 \u00c2\u00b5m Day\/Night Band images<\/p><\/div>\n

Other examples of mesospheric airglow waves were seen on 15 September 2013<\/strong><\/a> and 05 April 2013<\/strong><\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"

An AWIPS image of Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band (DNB) data at 06:10 UTC or 2:10 AM local time on 30 September 2013 (above) revealed multiple signatures of mesospheric airglow waves over portions of the western Atlantic Ocean. There are three distinct packets of waves seen on the DNB image — two of […]<\/p>\n","protected":false},"author":18,"featured_media":14048,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[49,48],"tags":[],"class_list":["post-14036","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-suomi_npp","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/14036","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=14036"}],"version-history":[{"count":14,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/14036\/revisions"}],"predecessor-version":[{"id":14064,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/14036\/revisions\/14064"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/14048"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=14036"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=14036"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=14036"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}