A smattering of strong to severe thunderstorms roamed South Central Nebraska from the early evening of Saturday the 20th into the very early morning of Sunday the 21st, prompting a few hail reports from widely-varying locations. The largest reported hail, ping pong to golf ball size, occurred in far southwestern Furnas County near Wilsonville. Later, quarter size stones fell from other storms at Wood River, Genoa and Silver Creek, although the late-night report from Silver Creek implied that much larger hail might have transpired (observer unable to confirm a maximum size).
Isolated storms first drifted into western portions of the 24-county area between 6-8 p.m. CDT, after initiating a few hours prior in west-central Nebraska along a north-south oriented surface trough. These initial storms included the one that produced the large hail in Furnas County. Between 8-11 p.m. CDT the vast majority of limited storm activity was rather weak, with the main exception of the briefly-severe storm that produced the 1-inch hail in Hall County. Then, about the time it appeared that any severe threat had ended for the night, a small cluster of storms began intensifying over eastern Nance County around midnight CDT, likely in response to the onset of a fairly weak southwesterly low level jet. Over the next few hours, this convection briefly morphed into a supercell that drifted southeast across portions of Nance, Merrick and Polk counties (yielding the Genoa and Silver Creek hail reports) before departing the local area around 2 a.m. CDT. In the mid-upper levels, forcing was provided by a low-amplitude shortwave trough translating across Nebraska in west-northwest flow, well-south of a larger-scale trough anchored over south central Canada. Mesoscale parameters over South Central Nebraska during the evening were certainly supportive of severe storms, featuring around 2000 J/kg mixed-layer CAPE and deep layer wind shear of 30-40 knots.