{"id":18955,"date":"2021-06-15T11:15:43","date_gmt":"2021-06-15T16:15:43","guid":{"rendered":"https:\/\/inside.nssl.noaa.gov\/ewp\/?p=18955"},"modified":"2021-06-15T11:15:43","modified_gmt":"2021-06-15T16:15:43","slug":"use-of-cloud-phase-distinction-rgb-to-anticipate-convective-initiation-over-western-dakotas-and-eastern-montana","status":"publish","type":"post","link":"https:\/\/inside.nssl.noaa.gov\/ewp\/2021\/06\/15\/use-of-cloud-phase-distinction-rgb-to-anticipate-convective-initiation-over-western-dakotas-and-eastern-montana\/","title":{"rendered":"Use of Cloud Phase Distinction RGB to anticipate convective initiation over Western Dakotas and Eastern Montana"},"content":{"rendered":"<p><span class=\"c1\">Some members of the 12z Thu Jun 10 HREF run were a bit slow in initiating convection or too far east in developing convection over the Northern Plains. The NSSL WRF-ARW was closest to reality with respect to exact timing and location. A special 18Z RAOB from Glasgow (GGW) MT and the\u00a0<\/span><span class=\"c6 c1\"><a class=\"c4\" href=\"https:\/\/www.google.com\/url?q=https:\/\/rammb2.cira.colostate.edu\/wp-content\/uploads\/2020\/01\/QuickGuide_DayCloudPhaseDistinction_final_v2.pdf&amp;sa=D&amp;source=editors&amp;ust=1623776022134000&amp;usg=AOvVaw2wQkNJNeKt5bo08c8DzeK0\">Cloud Phase Distinction RGB<\/a><\/span><span class=\"c2 c1\">\u00a0proved to be very helpful in showing convection was going to develop earlier than anticipated by the HREF guidance. The 18Z RAOB from GGW (below) showed weak CINH values, while the Day Cloud Phase Distinction RGB (second graphic) showed an agitated cumulus field that was becoming quickly glaciated (single cell with yellow cloud top near the 93\/61F sfc obs) indicating deep convective development was imminent.<\/span><\/p>\n<p><img decoding=\"async\" title=\"\" src=\"https:\/\/lh6.googleusercontent.com\/hQ0sKSzf_C_Ze8kvuQTMIhR8fkOZcD_BGiyNufhUFGz5RItaqSAhPPjyHwwkvZYMKuQPAVIelAsoQ-bNba3jrBpLEP0_k0Cx3tT4wcr_EEybW6HJA6b6T7ENBgyryno2bfKR8iFL\" alt=\"\" \/><\/p>\n<p><img decoding=\"async\" title=\"\" src=\"https:\/\/lh3.googleusercontent.com\/g84gL_VGfmUMRe69uwFd6RZDBWcptaVy64yJOlIHsNGqo5E0IsxJlxw-UJ1aPXC4lojcwQ8JMleGcGAqekqasGZtKdIXcJzrS-PHa5M7ib5TuhQRLHADbpCbuHxxe4rNth36d_8m\" alt=\"\" \/><\/p>\n<p><span class=\"c1\">Once deep convection initiated, single channel \u2018<\/span><span class=\"c1 c6\"><a class=\"c4\" href=\"https:\/\/www.google.com\/url?q=http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band13.pdf&amp;sa=D&amp;source=editors&amp;ust=1623776022136000&amp;usg=AOvVaw1DljbnQ82BellQfr-NMUlg\">Clean IR<\/a><\/span><span class=\"c1\">\u2019 imagery and\u00a0<\/span><span class=\"c6 c1\"><a class=\"c4\" href=\"https:\/\/www.google.com\/url?q=https:\/\/rammb2.cira.colostate.edu\/wp-content\/uploads\/2020\/01\/QuickGuide_GOESR_DayConvectionRGB_final-1.pdf&amp;sa=D&amp;source=editors&amp;ust=1623776022136000&amp;usg=AOvVaw3tc_pMjReWRXzs7CwDhzM9\">Day Convection RGB<\/a><\/span><span class=\"c2 c1\">\u00a0became more useful in determining updraft strength. These two products can be extremely useful in severe weather detection and warning decision making especially in absence of radar and\/or lightning data or when used combined due to its faster temporal coverage (1-min in meso sector vs 5-min from radar).<\/span><\/p>\n<p><img decoding=\"async\" title=\"\" src=\"https:\/\/lh3.googleusercontent.com\/nPUg_G2Qkc4621bvB0spiRJ1SGw1uR7mCGa4k99Ic8_6U3GuckXOiyHNpggWu0Gc7malddRgbW1ILI_7-g_5YswAvxOMyxnT6r9ORxAVJyU93Jz6OIsHK4NJOHAms4Re9fQ9QwHm\" alt=\"\" \/><\/p>\n<p><span class=\"c1\">The image above shows updrafts getting stronger in the 10.3 micron imagery (bottom left), and on the\u00a0<\/span><span class=\"c6 c1\"><a class=\"c4\" href=\"https:\/\/www.google.com\/url?q=https:\/\/rammb2.cira.colostate.edu\/wp-content\/uploads\/2020\/01\/QuickGuide_GOESR_DayConvectionRGB_final-1.pdf&amp;sa=D&amp;source=editors&amp;ust=1623776022138000&amp;usg=AOvVaw1v18FZ1SasSjCOrVdxaT10\">Daytime Convection RGB<\/a><\/span><span class=\"c1\">\u00a0(bottom right) by evidence of yellow (red +green) pixels.\u00a0<\/span><span class=\"c6 c1\"><a class=\"c4\" href=\"https:\/\/www.google.com\/url?q=https:\/\/rammb2.cira.colostate.edu\/trainings\/visit\/training_sessions\/storm_signatures_observed_in_satellite_imagery\/&amp;sa=D&amp;source=editors&amp;ust=1623776022138000&amp;usg=AOvVaw1WnmyjK5DoFxD4vAmljCP6\">Inflow feeder bands<\/a><\/span><span class=\"c1\">, a flanking line, towering cumulus above an invigorating RFD or flanking towers, and\u00a0<\/span><span class=\"c6 c1\"><a class=\"c4\" href=\"https:\/\/www.google.com\/url?q=https:\/\/rammb2.cira.colostate.edu\/trainings\/visit\/training_sessions\/above-anvil-cirrus-plumes\/&amp;sa=D&amp;source=editors&amp;ust=1623776022139000&amp;usg=AOvVaw0HkZ7H06fWpk0k74Khe4Q-\">above anvil cirrus plume<\/a><\/span><span class=\"c2 c1\">\u00a0are also observed in the Day Cloud Convection and Cloud Phase Distinction RGBs (top panels) indicative of the storms likely being severe. In fact, the ProbSevere v3 and v2 output both indicated a very high probability of severe weather occurring with these storms with values over 90% (purple colors).<\/span><\/p>\n<p><img decoding=\"async\" title=\"\" src=\"https:\/\/lh4.googleusercontent.com\/mLNNHy4zD443NThi-Z4NYDmqkmuEPOWaFmujJiab_ZWHFwEIXdpeizR1du4z-BDtuqaBPpEs_S3cU7LevhK_YQy0jT0uk_voG9ExZQsnSbxUcEtQaMlSfYYkpoDHjdYACWTe7Xt9\" alt=\"\" \/><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Some members of the 12z Thu Jun 10 HREF run were a bit slow in initiating convection or too far east in developing convection over the Northern Plains. The NSSL&#8230; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/inside.nssl.noaa.gov\/ewp\/2021\/06\/15\/use-of-cloud-phase-distinction-rgb-to-anticipate-convective-initiation-over-western-dakotas-and-eastern-montana\/\" class=\"more-link\">Read more \u00bb<\/a><\/p>\n","protected":false},"author":181,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[8,14],"tags":[58,56],"class_list":["post-18955","post","type-post","status-publish","format-standard","hentry","category-goesr","category-probsevere","tag-abi","tag-rgb"],"_links":{"self":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/18955","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\/181"}],"replies":[{"embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/comments?post=18955"}],"version-history":[{"count":1,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/18955\/revisions"}],"predecessor-version":[{"id":18956,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/posts\/18955\/revisions\/18956"}],"wp:attachment":[{"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/media?parent=18955"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/categories?post=18955"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/inside.nssl.noaa.gov\/ewp\/wp-json\/wp\/v2\/tags?post=18955"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}