During the late evening hours of Wednesday August 20th, scattered thunderstorms moved into portions of South Central Nebraska from the west. Just after midnight on Thursday the 21st, a possible cell merger resulted in the intensification of a storm over southeastern Buffalo and extreme northern Kearney counties. This storm produced some pockets of wind damage from these areas eastward to near the town of Prosser in northern Adams county, where it continued moving east just south of Interstate 80. Large tree branches were knocked down, a pole barn was damaged and an irrigation pivot was overturned. Much later in the day, during the early evening hours, an arc of thunderstorms developed over North Central Kansas. These storms expanded northward into portions of South Central Nebraska, apparently initiated by an outflow boundary emanating from the initial storms. One storm over York County was strong enough to produce one inch hail.
These storms formed in the vicinity of a wavy frontal boundary that was quasi-stationary which gradually became mobile and advanced east across Nebraska during the daytime hours. The longwave pattern was typical of summer, with a subtropical high over the Gulf Coast states. The flow was low amplitude with a general ridge over the eastern U.S. and a trough over the west. The thermodynamic and momentum environments did change from the overnight hours into the early evening hours. Overnight, mid-level lapse rates were steep (7.5 degrees C/km), resulting in MUCAPE of 1500-2000 J/kg. And while 40 knots of upper-level flow existed, the low-level jet of similar magnitude resulted in poor deep layer shear under 30 knots. By early evening, MLCAPE had increased to between 2000 and 3000 J/kg, with mid-level lapse rates a little more marginal, near 7 degrees C/km. Deep layer shear had increased to 30-35 knots.