{"id":24291,"date":"2017-06-29T23:07:32","date_gmt":"2017-06-29T23:07:32","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=24291"},"modified":"2017-07-02T02:06:42","modified_gmt":"2017-07-02T02:06:42","slug":"legacy-atmospheric-profiles-and-hail-in-iowa","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/24291","title":{"rendered":"Legacy Atmospheric Profiles and Large Hail in Iowa"},"content":{"rendered":"
\"\"<\/a>

GOES-16 Visible Imagery (0.64 \u00b5m) from 1902 through 2307 UTC on 29 June 2017. Woodbury County in Northwest Iowa is outlined in Magenta (Click to play animated gif)<\/p><\/div>\n

GOES-16 data posted on this page are preliminary, non-operational data and are undergoing testing<\/strong><\/p>\n

Softball-sized hail fell in northwestern Iowa on Thursday afternoon, 29 June (Storm Prediction Center Storm Reports<\/a>). The visible animation above, from 1902 to 2307 UTC, shows the rapid development of convection over far northeast Nebraska. Woodbury County in Iowa is outlined in the animation, the largest reported hail occurred in that county along the shores of the Missouri River; the location of the 4.25″ diameter hail is shown as the green box on this image<\/a>.\u00a0 This visible image<\/a> closely corresponds to the time of the hail fall.<\/p>\n

Since a GOES-16 Mesoscale Sector<\/a> was positioned over the region, imagery was available at 1-minute intervals — a comparison of “Red” Visible (0.64 \u00b5m<\/a>) and “Clean” Infrared Window (10.3 \u00b5m<\/a>) images is shown below. Plots of SPC storm reports are parallax<\/a>-corrected to match the location of the storm-top features. The rapid growth of the storm that produced the 4.25″ hail was apparent in the Infrared data, which showed cloud tops cooling from around -45\u00baC at 2000 UTC to -65.5\u00baC at 2130 UTC (the time of the hail report). Cloud-top cooling rates were consistently 3\u00baC\/5 minutes during this time. Also, in far northeastern Nebraska, a supercell thunderstorm produced an EF-1 tornado that tracked 14.4 miles along with hail up to 2.75 inches in diameter (NWS Omaha summary<\/a>).<\/p>\n

\"GOES-16<\/a>

GOES-16 Visible (0.64 \u00b5m, top) and Infrared Window (10.3 \u00b5m, bottom) images, with SPC storm reports plotted in red (on Visible) and black (on Infrared) [Click to play MP4 animation]<\/p><\/div>One of the GOES-16 Baseline Products available to forecasters includes a series of stability parameters derived from the ABI channels (and using GFS data as a first guess): Legacy Atmospheric Profiles<\/a> or LAP (Online Source<\/a>). These products are similar to those produced from the GOES Sounder on GOES-15<\/a>. The LAP Lifted Index at 2100 UTC, below, from the GOES-16 Mesoscale Sector sited over the convection, shows a remarkable pool of instability (Lifted Indices less than -8\u00baC) in the region near the developing convection (which was in the wam sector<\/a> of an approaching surface low). CAPE<\/a> values were in excess of 2000 J\/kg. More information on the Legacy Atmospheric Profiles products is available here<\/a> (as part of the Satellite Foundation Course for GOES-R<\/a>).<\/p>\n

LAP Profiles can be an excellent tool for situational awareness when convection develops in clear or partly-cloudy regions.<\/p>\n

\"\"<\/a>

GOES-16 Legacy Atmospheric Profile (LAP) estimate of Lifted Index, 2100 UTC on 29 June 2017 (Click to enlarge)<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"

GOES-16 data posted on this page are preliminary, non-operational data and are undergoing testing Softball-sized hail fell in northwestern Iowa on Thursday afternoon, 29 June (Storm Prediction Center Storm Reports). The visible animation above, from 1902 to 2307 UTC, shows the rapid development of convection over far northeast Nebraska. Woodbury County in Iowa is outlined […]<\/p>\n","protected":false},"author":19,"featured_media":24299,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[74,3],"tags":[],"class_list":["post-24291","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-16","category-severe-convection"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/24291","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/users\/19"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=24291"}],"version-history":[{"count":25,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/24291\/revisions"}],"predecessor-version":[{"id":24320,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/24291\/revisions\/24320"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/24299"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=24291"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=24291"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=24291"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}