Cold front leads to strong to severe thunderstorms for portions of south central Nebraska during the evening of May 17th. The first thunderstorms of this event developed over southwest Furnas County between 4PM and 5PM CDT. The initial concern was the potential for landspouts, and at least two were reported in the area of Wilsonville and Beaver City. As is often the case with landspouts, these were very brief touchdowns, and no damage indicators could be found, so they were given an EFU, or unknown, rating. This initial setup for landspouts was fairly typical for this region in which steep low level lapse rates coincided with weak deep layer wind shear, weak low level convergence, and a weak surface front that provides abundant ambient surface vorticity. Eventually, between 5PM and 7PM, thunderstorms unzipped , or developed further northeast in Kearney County, along the advancing cold front, which lead to upscale growth into a couple intense thunderstorm clusters. Large hail was the primary hazard with this activity, and for the most part ranged from quarter to golf ball size. However, up to 3 inch in diameter hail was reported in Harlan County. The thunderstorm clusters moved east and southeast, and eventually weakened and/or shifted in northern Kansas around 8PM CDT.
Another separate broken line of thunderstorms developed further north, from around Kearney to Columbus, between 9PM and 10PM. This activity persisted for a couple of hours before weakening. Once again, large hail was the primary threat, with penny to half dollar size hail reported in portions of Hall and Hamilton Counties.