Slow moving upper low brings multiple rounds of thunderstorms, including locally heavy rain and a few severe thunderstorms, on July 29th. Low to mid level warm air advection ahead of a lead shortwave trough led to the development of scattered showers and thunderstorms roughly along a line from Hastings to Superior between 6-8am CDT. Locally heavy rain rates and slow moving thunderstorms led to areas of heavy rain across portions of Clay, Nuckolls, Fillmore and Thayer Counties during the mid to late morning hours. Soil conditions in these areas were already saturated due to previous heavy rain events over the recent days. Activity decreased in coverage and intensity around midday, and most areas were dry by 1pm CDT. Total rain amounts of 2-3 inches were common across these areas, which led to renewed flooding, particularly over Thayer County. The primary impact was water covering county roads and water flowing over Highway 136 west of Deshler. Conditions were favorable for heavy rain given the aforementioned slow storm motions, but also relatively high precipitable water values near 2 .
Additional thunderstorm activity developed during the afternoon hours from central Nebraska into northwest Kansas. Initial individual and cellular thunderstorms grew upscale into several clusters during the late afternoon and into the evening. One such cluster moved through far western portions of the County Warning Area (CWA), mainly from Cozad down to Beaver City, between 6-8pm CDT. Some of this activity became severe and produced up to ping pong ball sized hail across Furnas County. As this activity weakened around 8pm CDT, new, mainly isolated, thunderstorms developed just to the NE over Phelps and Buffalo Counties between 8-9pm CDT. Up to penny size hail was reported with this activity over Phelps County. Yet another round of thunderstorms developed and organized into a mesoscale convective system (MCS) west of the area, then moved through areas southwest of a line from Lexington, Nebraska to Beloit, Kansas after 10pm CDT. This activity was strong, but remained non-severe, over south central Nebraska.