Thunderstorms brought large hail and damaging wind gusts to eastern Nebraska and southwest Iowa during the late afternoon and evening hours of May 15, 2026. Through the afternoon, moisture pooled along a surface front, with an upper-level shortwave initiating convective development. Surface-based instability (SBCAPE) of 2000 to 2500 J/kg materialized across the region. This instability, combined with 35 to 40 knots of deep-layer (0-6 km) bulk shear, initially favored discrete supercell development. Atmospheric soundings revealed fairly dry low levels, which enhanced the threat for severe, damaging wind gusts as the convection transitioned into an outflow-dominated regime. Additional storms developed along the boundary across far eastern Nebraska into the evening hours before the entire line eventually became outflow-dominant and weakened.
Several notable severe weather impacts were reported across southwest Iowa and eastern Nebraska during the event, primarily driven by damaging wind gusts and hail. The most significant wind damage occurred in southwest Iowa, where gusts estimated between 60 and 75 mph caused structural and agricultural damage. A measured gust of 74 mph was recorded by the Red Oak, IA AWOS, which correlated with amateur radio reports of downed power poles, tree damage, and widespread power outages in the city. In Mills County, severe winds blew over farm augers and moved grain wagons near Randolph, while structural damage to roofing and siding was reported further east in Stanton. Alongside the wind threat, severe hail up to 1.00 inch in diameter (quarter-sized) was widely reported across the region, including instances in Cass, Seward, Washington, and Douglas counties in Nebraska with one 1.00-inch hail report coming directly from an NWS employee in Valley, NE.