Despite weak upper forcing and fairly strong convective inhibition (CINH) keeping the vast majority of South Central Nebraska storm-free on this early Tuesday evening, a pair of rogue, slow-moving supercell storms were able to breach the cap and produce hail to at least golf ball size in small portions of Buffalo and Clay counties. The far southeastern Buffalo County storm initiated first, shortly before 7 p.m. CDT, and drifted slowly south before rapidly dissipating only about an hour later. Along the way though, it dumped hail up to 2 inches in diameter on Shelton. Just as this storm was fading the second one got going in southeastern Clay County around 8 p.m. CDT and followed a very similar life cycle, drifting slowly south-southeast and dissipating 60-90 minutes later, but not before dropping golf ball size hail north of Edgar that reportedly damaged crops and cracked vehicle windshields. A weaker storm that split eastward from the Clay County supercell briefly affected northwestern Thayer County, but once this convection died around 930 p.m. CDT with the onset of diurnal cooling, the remainder of the night was storm-free.
This somewhat-surprising, albeit brief/localized event was a textbook case of why one can never say never to at least isolated robust convection in a high instability environment during summer peak heating. In the mid-upper levels, South Central Nebraska resided along the northeast periphery of an expansive ridge centered over the Four Corners region. Although deep-layer shear was respectable (around 40 knots), the flow over the Central Plains lacked any notable disturbances and fairly strong capping was present (as indicated by 700 millibar temperatures around 12 C). However, upon closer review, a subtle northwest-southwest oriented surface boundary was draped across the heart of the local area, promoting weak low-level convergence between light easterly breezes and light southerlies. This subtle convergence, in tandem with fairly robust mixed-layer CAPE of 2000-3000 J/kg (owing to temperatures/dewpoints well into the 90s/60s F) proved just sufficient enough to spark the isolated severe activity.