Severe thunderstorms produced hail up to the size of golf balls in a few locations on this Tuesday afternoon. Just after 2 p.m. CST, an isolated thunderstorm developed along the Buffalo-Sherman County line. This storm advanced slowly to the east and weakened by 3:30 p.m. By 2:45 p.m., another storm joined it over northern Sherman County. This storm moved north into Valley County by 3:30 p.m. and exited the county by 5 p.m. Both of these storms produced hail up to the size of golf balls. The second storm produced golf ball size hail near Arcadia and near Fort Hartsuff State Park.
These storms formed well ahead of a backdoor cold front that was pressing into northeastern Nebraska. However, convective initiation was more likely a result of a small area of low-level convergence between Broken Bow, where winds were from the west, and Ord, where winds were from the east. In the upper levels, a subtropical high was over Oklahoma, with a ridge extending north through the Dakotas. Troughs were located over the western and eastern United States. At mid-afternoon, surface temperatures were in the middle 90s, with dewpoints in the middle to upper 60s. With mid-level lapse rates near 7 deg C/km, MLCAPE was around 2500 J/kg. Deep layer shear was near 25 knots.