{"id":4426,"date":"2012-05-23T19:47:01","date_gmt":"2012-05-24T00:47:01","guid":{"rendered":"https:\/\/hwt.nssl.noaa.gov\/ewp\/internal\/blog\/?p=4426"},"modified":"2012-05-23T19:47:01","modified_gmt":"2012-05-24T00:47:01","slug":"ci-product-over-e-nebraska","status":"publish","type":"post","link":"https:\/\/inside.nssl.noaa.gov\/ewp\/2012\/05\/23\/ci-product-over-e-nebraska\/","title":{"rendered":"CI product over E-Nebraska"},"content":{"rendered":"<p>The cold front over NC-Kansas and SE Nebraska was monitored for further development. As expected, storms began to build SW-wards towards the KS boarder and CI products were effective in highlighting the area with highest probabilities for potential development along that boundary.<\/p>\n<p>The event occurred over Clay and York counties (Nebraska). A series of images will be added to show the evolution:<\/p>\n<figure id=\"attachment_4432\" aria-describedby=\"caption-attachment-4432\" style=\"width: 450px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2012\/05\/2305_2232CI-.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-large wp-image-4432\" title=\"2305_2232CI\" src=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2012\/05\/2305_2232CI--1024x549.png\" alt=\"\" width=\"450\" height=\"241\" \/><\/a><figcaption id=\"caption-attachment-4432\" class=\"wp-caption-text\">UAHCI product upper left, CIMMS Cld top cooling upper right, lightning data lower left and surface reflectivity at -10 C isothermal level at 2232 Z<\/figcaption><\/figure>\n<figure id=\"attachment_4433\" aria-describedby=\"caption-attachment-4433\" style=\"width: 450px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2012\/05\/2305_2245CI-.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-large wp-image-4433\" title=\"2305_2245CI\" src=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2012\/05\/2305_2245CI--1024x549.png\" alt=\"\" width=\"450\" height=\"241\" \/><\/a><figcaption id=\"caption-attachment-4433\" class=\"wp-caption-text\">UAHCI product upper left, CIMMS Cld top cooling upper right, lightning data lower left and surface reflectivity at -10 C isothermal level at 2245 Z<\/figcaption><\/figure>\n<figure id=\"attachment_4434\" aria-describedby=\"caption-attachment-4434\" style=\"width: 450px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2012\/05\/2305_2302CI-.png.png\"><img loading=\"lazy\" decoding=\"async\" class=\"size-large wp-image-4434\" title=\"2305_2302CI .png\" src=\"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-content\/uploads\/sites\/22\/2012\/05\/2305_2302CI-.png-1024x549.png\" alt=\"\" width=\"450\" height=\"241\" \/><\/a><figcaption id=\"caption-attachment-4434\" class=\"wp-caption-text\">UAHCI product upper left, CIMMS Cld top cooling upper right, lightning data lower left and surface reflectivity at -10 C isothermal level at 2302 Z<\/figcaption><\/figure>\n<p>Roughly 30 min before surface reflectivity at -10C isothermal level revealed first signs of development, the CI product highlighted both counties with 50-60 % probabilities. The cloud top cooling product showed values of -15 to -25K\/15 min at 2315Z (not shown) and the first significant reflectivity signal (56 dbZ ) became visible at 2330 Z. At 00Z onwards a 63 dBz cell evolved out of that NE of York.<\/p>\n<p>Helge<\/p>\n","protected":false},"excerpt":{"rendered":"<p>The cold front over NC-Kansas and SE Nebraska was monitored for further development. As expected, storms began to build SW-wards towards the KS boarder and CI products were effective in&#8230; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/inside.nssl.noaa.gov\/ewp\/2012\/05\/23\/ci-product-over-e-nebraska\/\" class=\"more-link\">Read more \u00bb<\/a><\/p>\n","protected":false},"author":333,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[10],"tags":[],"class_list":["post-4426","post","type-post","status-publish","format-standard","hentry","category-live-blogs"],"_links":{"self":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/4426","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\/333"}],"replies":[{"embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/comments?post=4426"}],"version-history":[{"count":0,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/4426\/revisions"}],"wp:attachment":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/media?parent=4426"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/categories?post=4426"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/tags?post=4426"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}