A mesoscale convective system (MCS) developed over central Nebraska, then moved east-southeast during the early morning hours of Sunday, May 24, bringing damaging winds to portions of the area.
Thunderstorms developed just west of the Hastings County Warning Area (CWA), in Lincoln and Custer Counties, around 10 PM CDT on the evening of Saturday, May 23. Another line of thunderstorms developed over western Nebraska and moved eastward through the evening hours. The central Nebraska cluster was very slow moving, and even stationary at times, which allowed the two clusters to merge over Custer County around midnight on Sunday, May 24. Shortly after this merger, the line of thunderstorms gained eastward momentum and moved into Valley and Sherman Counties around 1 AM CDT, bringing with them strong, damaging winds. The line weakened slightly as it continued to track east-southeast during the early morning hours on Sunday, with the strongest activity tracking along and northeast of a line from Loup City, NE to York, NE. Measured wind gusts were generally near or less than 60 mph, including a gust of 54 mph measured by the ASOS at the Ord Airport, and a 57mph gust measured by a mesonet site at Scotia. The strongest measured gust was 63mph by a mesonet station 6 NNE of Sherman Reservoir at 1:35 AM CDT. Estimated wind gusts as high as 70 mph were reported in Valley and Sherman Counties, which resulted in the toppling of several irrigation pivots in these areas. The line of thunderstorms exited the Hastings CWA to the east between 4-5 AM CDT.
A nocturnal line of thunderstorms (aka MCS), such as this, is common for this area during the late spring and summer months. Thunderstorms were fueled by a 40 kt southerly low level jet, which advected strong instability (most unstable CAPE values near 3000 J/kg) from northern Kansas into central Nebraska and provided convergence/ascent for elevated parcels at the terminus of this jet over central Nebraska. Moderate effective shear up to 40 kt also aided in thunderstorm organization, along with an established cold pool associated with the western cluster of convection.