{"id":4043,"date":"2012-05-17T13:50:21","date_gmt":"2012-05-17T18:50:21","guid":{"rendered":"https:\/\/hwt.nssl.noaa.gov\/ewp\/internal\/blog\/?p=4043"},"modified":"2012-05-17T13:50:21","modified_gmt":"2012-05-17T18:50:21","slug":"nearcasting-for-jax","status":"publish","type":"post","link":"https:\/\/inside.nssl.noaa.gov\/ewp\/2012\/05\/17\/nearcasting-for-jax\/","title":{"rendered":"NearCasting for JAX"},"content":{"rendered":"<p>We are focused on the JAX CWA today.\u00a0 While there is convection ongoing in the extreme northern portion of the area (bordering FFC and CHS), the GOES-R NearCast CAPE (new this week) and vertical theta-e difference suggest that the southern half of the JAX CWA is more conducive for new convection.<\/p>\n<figure id=\"attachment_4044\" aria-describedby=\"caption-attachment-4044\" style=\"width: 450px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2012\/05\/bcc_nearcast_20120517-1900.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-large wp-image-4044\" title=\"GOES-R NearCast 780mb Theta-E, Vertical Theta-E Difference, CAPE, and Sustained Convection Index valid 2012-05-17 1830 UTC\" src=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2012\/05\/bcc_nearcast_20120517-1900-e1337280392470-1024x535.png\" alt=\"GOES-R NearCast 780mb Theta-E, Vertical Theta-E Difference, CAPE, and Sustained Convection Index valid 2012-05-17 1830 UTC\" width=\"450\" height=\"235\" \/><\/a><figcaption id=\"caption-attachment-4044\" class=\"wp-caption-text\">GOES-R NearCast 780mb Theta-E, Vertical Theta-E Difference, CAPE, and Sustained Convection Index valid 2012-05-17 1830 UTC<\/figcaption><\/figure>\n<p>The NearCast has been challenging to interpret this week due to interpretation confusion (are negative versus positive theta-e differences indicative of instability) and then a mid-week visualization change in AWIPS 2.\u00a0 The NearCast shows promise for helping with the tremendously-difficult 1-6 hour timeframe, but the product stability has presented a problem.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>We are focused on the JAX CWA today.\u00a0 While there is convection ongoing in the extreme northern portion of the area (bordering FFC and CHS), the GOES-R NearCast CAPE (new&#8230; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/inside.nssl.noaa.gov\/ewp\/2012\/05\/17\/nearcasting-for-jax\/\" class=\"more-link\">Read more \u00bb<\/a><\/p>\n","protected":false},"author":215,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[10],"tags":[25],"class_list":["post-4043","post","type-post","status-publish","format-standard","hentry","category-live-blogs","tag-goesr-nearcast"],"_links":{"self":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/4043","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\/215"}],"replies":[{"embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/comments?post=4043"}],"version-history":[{"count":0,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/4043\/revisions"}],"wp:attachment":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/media?parent=4043"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/categories?post=4043"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/tags?post=4043"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}