Although only a small portion of the six-county area in North Central Kansas experienced severe weather on this Thursday evening, the one severe storm that formed was one of the most intense individual storms of the mid-to-late summer within the area. Rapidly evolving from a multicell cluster to a brief high-precipitation supercell, this storm packed quite a punch, causing considerable wind damage in northern Jewell County as it pushed along the Kansas-Nebraska border mainly between 9 PM and 1030 PM CDT. Estimated winds of 60 to at least 80 MPH were reported, with a home weather station northeast of Webber measuring 67 MPH. The most substantial report of wind damage occurred in extreme northern Jewell County just 2 miles south of Superior, Nebraska, where a modular home was declared a total loss after having its roof and one wall blown off. The residents were un-injured. Extensive tree and crop damage occurred across near the state line as well. As the storm moved just east of the Webber and Superior area toward northwestern Republic County, it rapidly started to weaken and dissipate. Although additional thunderstorms rumbled across much of North Central Kansas well into the early morning hours on the 22nd, none of these became severe.
This storm rapidly intensified around 9 PM CDT, evolving from a weak and narrow line of convection that had been drifting east along the state line for a few hours. This area of convection was largely detached from more widespread multicell storm activity ongoing at least 50-80 miles to the south near Interstate 70. The rapid intensification into a supercell was likely due to a combination of factors, including the encountering of a more unstable and less-capped airmass in the vicinity of a surface warm front. Mesoscale severe weather parameters around this time featured only marginal deep-layer vertical wind shear around 30 knots, but significant mixed-layer CAPE of 3000-4000 J/kg. Aloft, synoptic forcing was weak, with only subtle mid level disturbances passing through weak to modest quasi-zonal flow. This was a typical summer pattern for North Central Kansas, with the region positioned along the interface between a broad upper level ridge across the southern states, and faster westerly flow across the northern tier of the nation.