{"id":12885,"date":"2015-06-09T18:18:13","date_gmt":"2015-06-09T23:18:13","guid":{"rendered":"http:\/\/hwt.nssl.noaa.gov\/ewp\/internal\/blog\/?p=12885"},"modified":"2016-10-03T17:55:26","modified_gmt":"2016-10-03T22:55:26","slug":"interesting-observation","status":"publish","type":"post","link":"https:\/\/inside.nssl.noaa.gov\/ewp\/2015\/06\/09\/interesting-observation\/","title":{"rendered":"Interesting Observation"},"content":{"rendered":"<p>While looking at the CAPE and PWAT trends, we notices the storm development in SD matches almost exactly with the leading edge of the gradient ahead of the approaching cold front.<\/p>\n<p>The exact CAPE values were about twice as much as the LAP analysis, but the overall pattern matched well. The NUCAPS altered sounding (adding low level moisture) brought the CAPE closer to expected values.<\/p>\n<p><a href=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2015\/06\/PWAT-vis2245.png\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-12886\" src=\"http:\/\/hwt.nssl.noaa.gov\/ewp\/internal\/blog\/wp-content\/uploads\/2015\/06\/PWAT-vis2245-300x172.png\" alt=\"PWAT-vis22:45\" width=\"300\" height=\"172\" srcset=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2015\/06\/PWAT-vis2245-300x172.png 300w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2015\/06\/PWAT-vis2245-768x441.png 768w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2015\/06\/PWAT-vis2245-1024x588.png 1024w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2015\/06\/PWAT-vis2245-500x287.png 500w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2015\/06\/PWAT-vis2245.png 1574w\" sizes=\"auto, (max-width: 767px) 100vw, (max-width: 1200px) 60vw, 720px\" \/><\/a> <a href=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2015\/06\/CAPE-vis2245.png\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-12887\" src=\"http:\/\/hwt.nssl.noaa.gov\/ewp\/internal\/blog\/wp-content\/uploads\/2015\/06\/CAPE-vis2245-300x172.png\" alt=\"CAPE-vis22:45\" width=\"300\" height=\"172\" srcset=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2015\/06\/CAPE-vis2245-300x172.png 300w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2015\/06\/CAPE-vis2245-768x441.png 768w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2015\/06\/CAPE-vis2245-1024x588.png 1024w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2015\/06\/CAPE-vis2245-500x287.png 500w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2015\/06\/CAPE-vis2245.png 1574w\" sizes=\"auto, (max-width: 767px) 100vw, (max-width: 1200px) 60vw, 720px\" \/><\/a><\/p>\n<p>-BT<\/p>\n","protected":false},"excerpt":{"rendered":"<p>While looking at the CAPE and PWAT trends, we notices the storm development in SD matches almost exactly with the leading edge of the gradient ahead of the approaching cold&#8230; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/inside.nssl.noaa.gov\/ewp\/2015\/06\/09\/interesting-observation\/\" class=\"more-link\">Read more \u00bb<\/a><\/p>\n","protected":false},"author":136,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[7],"tags":[],"class_list":["post-12885","post","type-post","status-publish","format-standard","hentry","category-general"],"_links":{"self":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/12885","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/users\/136"}],"replies":[{"embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/comments?post=12885"}],"version-history":[{"count":1,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/12885\/revisions"}],"predecessor-version":[{"id":14367,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/12885\/revisions\/14367"}],"wp:attachment":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/media?parent=12885"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/categories?post=12885"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/tags?post=12885"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}