Damaging winds and large hail occurred over Furnas county late on this Thursday afternoon. Before that occurred, an area of scattered thunderstorms developed across the Nebraska Sandhills during the early afternoon. This area moved southeast through the afternoon with the easternmost storms weakening and dissipating over south central Nebraska. Conversely, the westernmost storms intensified. One of the storms intensified over eastern Frontier county and it dropped due south across southwestern Gosper county just after 510 PM CST. The storm continued moving into northern Furnas county where it weakened and became sub-severe by 550 PM CST. Winds were measured at 65 mph in and near Holbrook using a handheld anemometer, with 2 to 3 inch diameter tree limbs snapped off. Hail up to the size of golf balls also occurred near and just west of Holbrook. Based on radar, this storm was probably severe over extreme southwestern Gosper county, but no reports were received since that area is very rural.
The surface pressure pattern was weak over the Central Plains, but high pressure was over the Northern Plains. There may have been a very weak stationary front extending from central Kansas into extreme southwestern Nebraska, south of where the thunderstorms occurred. The upper-level flow was modestly amplified with a subtropical high over the Desert Southwest, a low over Ontario, and cyclonic west-northwest flow over the Central Plains. As was the case on many days in this pattern, late this month, there was no obvious trigger for these storms. They just seemed to appear. The prestorm environment featured temperatures around 80 with dewpoints in the lower 60s. Mid-level lapse rates were poor, resulting in MLCAPE of just under 1000 J/kg. However, deep layer shear was very strong at 50 kt.