{"id":9618,"date":"2014-06-04T15:28:16","date_gmt":"2014-06-04T20:28:16","guid":{"rendered":"http:\/\/hwt.nssl.noaa.gov\/ewp\/internal\/blog\/?p=9618"},"modified":"2016-10-03T17:53:54","modified_gmt":"2016-10-03T22:53:54","slug":"vlaps-analysis","status":"publish","type":"post","link":"https:\/\/inside.nssl.noaa.gov\/ewp\/2014\/06\/04\/vlaps-analysis\/","title":{"rendered":"vLAPS analysis"},"content":{"rendered":"<p><a href=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2014\/06\/vLAPSwed.png\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-large wp-image-9646\" alt=\"vLAPSwed\" src=\"http:\/\/hwt.nssl.noaa.gov\/ewp\/internal\/blog\/wp-content\/uploads\/2014\/06\/vLAPSwed-1024x576.png\" width=\"584\" height=\"328\" srcset=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2014\/06\/vLAPSwed-1024x576.png 1024w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2014\/06\/vLAPSwed-300x169.png 300w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2014\/06\/vLAPSwed-768x432.png 768w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2014\/06\/vLAPSwed-500x281.png 500w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2014\/06\/vLAPSwed.png 1920w\" sizes=\"auto, (max-width: 767px) 100vw, (max-width: 1200px) 60vw, 720px\" \/><\/a>Taking a look at the vLAPS, you can see the instability gradient in the far northern part of LMK where the sfc obs show the best convergence. This is where we expect the majority most significant convection to fire. The simulated reflectivity is overdone and too far south anchored to the highest instability. So, the gradient of the instability is the best indicator in this case for the most aggressive convection.<\/p>\n<p>jca<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Taking a look at the vLAPS, you can see the instability gradient in the far northern part of LMK where the sfc obs show the best convergence. This is where&#8230; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/inside.nssl.noaa.gov\/ewp\/2014\/06\/04\/vlaps-analysis\/\" class=\"more-link\">Read more \u00bb<\/a><\/p>\n","protected":false},"author":77,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[7],"tags":[],"class_list":["post-9618","post","type-post","status-publish","format-standard","hentry","category-general"],"_links":{"self":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/9618","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\/77"}],"replies":[{"embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/comments?post=9618"}],"version-history":[{"count":1,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/9618\/revisions"}],"predecessor-version":[{"id":13918,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/9618\/revisions\/13918"}],"wp:attachment":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/media?parent=9618"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/categories?post=9618"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/tags?post=9618"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}