This Saturday evening featured several, mainly non-severe multicell thunderstorms, primarily within counties north of Interstate 80. However, between 8-9 p.m. CDT, a small-but-briefly intense storm tracked along the Dawson-Gosper County line, yielding one report of golf ball size hail roughly halfway between Lexington and Johnson Lake before quickly weakening. Around this same time, a more widespread area of scattered strong convection started blossoming north of Interstate 80, peaking in intensity between 9-11:30 p.m. CDT before fading away. Based on radar data, marginally severe hail and/or wind might have affected portions of Nance, Howard and Merrick counties, but there were no verifying ground-truth reports.
In the mid-upper levels, this event occurred within a fairly subtle forcing regime, with the local area seeing only passing weak ripples embedded in quasi-zonal flow, well-downstream from a stronger shortwave trough well off to the west over western Wyoming. At the surface, a fairly weak quasi-stationary front extended southeastward across north central and eastern Nebraska, attendant to a weak low pressure center over South Dakota. Around the time of the hail near Lexington, the mesoscale environment featured mixed-layer CAPE around 1000 J/kg and deep-layer wind shear of 30-40 knots.