{"id":34024,"date":"2019-08-14T22:59:39","date_gmt":"2019-08-14T22:59:39","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=34024"},"modified":"2019-08-16T14:55:13","modified_gmt":"2019-08-16T14:55:13","slug":"nucaps-soundings-surrounding-an-isolated-thundershower","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/34024","title":{"rendered":"NUCAPS Soundings surrounding an isolated Thundershower"},"content":{"rendered":"
\"\"<\/a>

GOES-16 ABI Band 2 (0.64 \u00b5m) at 1946 UTC on 14 August 2019 (Click to enlarge)<\/p><\/div>\n

The GOES-16 Visible (0.64 \u00b5m) image above shows a weak thunderstorm over southeastern Oklahoma surrounding an decaying outflow boundary.\u00a0 (Click here<\/a> to see an animation of the visible imagery). The convection did not look particularly robust, but it did produce lightning that was detected by the Geostationary Lightning Mapper (GLM), as shown below.<\/p>\n

\"\"<\/a>

GOES-16 ABI Band 2 (0.64 \u00b5m) and GLM observations of Flash Extent Density at 1946 UTC on 14 August 2019<\/p><\/div>\n

Lightning requires charge separation in a cloud; typically lightning occurs after the cloud top glaciates. During daytime, glaciation can be detected with ABI Band 5, at 1.61 \u00b5m, the so-called Snow\/Ice band<\/a>. The toggle below shows the visible, snow\/ice band<\/a>, and the Baseline Cloud Phase<\/a> product. Glaciation is indicated.<\/p>\n

\"\"<\/a>

GOES-16 ABI Band 2 (0.64 \u00b5m), Band 5 (1.61 \u00b5m) and Baseline Cloud Phase at 1946 UTC on 14 August 2019<\/p><\/div>\n

This case is interesting because NOAA-20 overflew the convection, and soundings were produced around the convection, as shown below.<\/p>\n

\"\"<\/a>

GOES-16 ABI Band 2 (0.64 \u00b5m) at 1946 UTC on 14 August 2019 along with NUCAPS Sounding Points at 1945 UTC<\/p><\/div>\n

The animation below steps north-south through seven profiles that surround the weak convection. Note that a profile near the convection has thermodynamic parameters more favorable for convection than at the other profiles.\u00a0 For example, NUCAPS profiles show the convection at the northern edge of a precipitable water gradient, and also in a local minimum of inhibition.\u00a0\u00a0\u00a0 Although the convection has initiated here, the fields do suggest that NUCAPS can be used to monitor thermodynamics at small scales before initiation.<\/p>\n

\"\"<\/a>

NUCAPS Soundings at various points north, south and within convection at 1946 UTC on 14 August 2019 (Click to enlarge) Thermodynamic variables from the sounding are noted.<\/p><\/div>\n

Horizontal gridded information derived from NUCAPS data will be in AWIPS shortly.\u00a0 See this post<\/a> from Emily Berndt at SPoRT!<\/p>\n","protected":false},"excerpt":{"rendered":"

The GOES-16 Visible (0.64 \u00b5m) image above shows a weak thunderstorm over southeastern Oklahoma surrounding an decaying outflow boundary.\u00a0 (Click here to see an animation of the visible imagery). The convection did not look particularly robust, but it did produce lightning that was detected by the Geostationary Lightning Mapper (GLM), as shown below. Lightning requires […]<\/p>\n","protected":false},"author":19,"featured_media":34028,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[42,74,83],"tags":[],"class_list":["post-34024","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-convective-initiation","category-goes-16","category-nucaps"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/34024","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=34024"}],"version-history":[{"count":5,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/34024\/revisions"}],"predecessor-version":[{"id":34041,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/34024\/revisions\/34041"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/34028"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=34024"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=34024"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=34024"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}