{"id":18407,"date":"2021-04-20T14:15:29","date_gmt":"2021-04-20T19:15:29","guid":{"rendered":"https:\/\/inside.nssl.noaa.gov\/ewp\/?p=18407"},"modified":"2021-04-20T14:15:29","modified_gmt":"2021-04-20T19:15:29","slug":"algorithm-performance-in-qlcs-transition","status":"publish","type":"post","link":"https:\/\/inside.nssl.noaa.gov\/ewp\/2021\/04\/20\/algorithm-performance-in-qlcs-transition\/","title":{"rendered":"Algorithm Performance in QLCS transition"},"content":{"rendered":"<p><span style=\"font-weight: 400\">Both algorithms tagged onto the minor circulations within a developing QLCS pretty well with one or the other, or in several instances both, showing locations with increased vertical vorticity in areas that didn\u2019t exhibit obvious bows or kinks in reflectivity. There was some noise and residual circulations in other parts of the storm, so there is room for detection improvement, but overall performance along the leading edge was okay.<\/span><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-18408\" src=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2021\/04\/Picture6-900x804.png\" alt=\"\" width=\"900\" height=\"804\" srcset=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2021\/04\/Picture6-900x804.png 900w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2021\/04\/Picture6-768x686.png 768w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2021\/04\/Picture6-600x536.png 600w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2021\/04\/Picture6.png 936w\" sizes=\"auto, (max-width: 767px) 100vw, (max-width: 1200px) 60vw, 720px\" \/><\/p>\n<p><span style=\"font-weight: 400\">Reflectivity at 03:32 KTLX<\/span><\/p>\n<p>&nbsp;<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-18409\" src=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2021\/04\/Picture7-900x804.png\" alt=\"\" width=\"900\" height=\"804\" srcset=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2021\/04\/Picture7-900x804.png 900w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2021\/04\/Picture7-768x686.png 768w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2021\/04\/Picture7-600x536.png 600w, https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2021\/04\/Picture7.png 936w\" sizes=\"auto, (max-width: 767px) 100vw, (max-width: 1200px) 60vw, 720px\" \/><\/p>\n<p><span style=\"font-weight: 400\">Velocity at 03:32 KTLX<\/span><\/p>\n<p>&nbsp;<\/p>\n<p><span style=\"font-weight: 400\">&#8211; #ProtectAndDissipate<\/span><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Both algorithms tagged onto the minor circulations within a developing QLCS pretty well with one or the other, or in several instances both, showing locations with increased vertical vorticity in&#8230; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/inside.nssl.noaa.gov\/ewp\/2021\/04\/20\/algorithm-performance-in-qlcs-transition\/\" class=\"more-link\">Read more \u00bb<\/a><\/p>\n","protected":false},"author":137,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[55,79],"class_list":["post-18407","post","type-post","status-publish","format-standard","hentry","category-news","tag-nmda","tag-ntda"],"_links":{"self":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/18407","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\/137"}],"replies":[{"embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/comments?post=18407"}],"version-history":[{"count":1,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/18407\/revisions"}],"predecessor-version":[{"id":18410,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/18407\/revisions\/18410"}],"wp:attachment":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/media?parent=18407"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/categories?post=18407"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/tags?post=18407"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}