Despite a fairly favorable setup for severe thunderstorms on this Thursday afternoon and evening, the ingredients didn't quite come together across the vast majority of South Central Nebraska, with radar data suggesting only the presence of a few strong storms roaming counties along and north of Interstate 80. However, a delayed storm report received the next day revealed that a tiny fraction of the area did in fact experience a severe wind event: a Merrick County farmer reported a flipped irrigation pivot and significant crop damage in a localized area near Silver Creek. Although radar data was inconclusive regarding the severity of these winds (due in part to the lowest beam height situated 6,000 feet above ground level at that distance), a fairly strong reflectivity core did pass through that area around 9 p.m. CDT within an environment featuring strong low level wind shear (see below). A few hours prior to the Merrick County damage, northwestern portions of South Central Nebraska narrowly avoided a severe weather threat from a cluster of splitting supercells in Custer County. However, these storms weakened before entering local counties such as Dawson and Valley. Then, between 8-10 p.m. CDT, a handful of strong multicell storms flared up within the northeast quadrant of South Central Nebraska in response to a strengthening low level jet, including the Merrick County storm. While additional non-severe storms lingered over northeast counties such as Nance, Merrick and Polk past the midnight hour, all of South Central Nebraska was storm-free by 2:30 a.m. CDT.
This was a somewhat unusual severe weather setup by late-August standards, as a seasonably well-defined surface low and attendant eastward-arcing warm front became established over the heart of South Central Nebraska during the afternoon and evening. Although mid/upper level flow wasn't overly strong, a fairly compact vort max tracked over central Nebraska, well to the north of an expansive ridge anchored over northern Mexico. In addition, a seasonably-strong southerly low level jet ramped up to around 40 knots over much of central and eastern Nebraska by early evening. The combination of this low level jet and the underlying surface warm front yielded an impressive 30 knots of 0-1 kilometer low level wind shear around the time of the Merrick County wind damage. Other early-evening mesoscale parameters were more modest, including roughly 1000 J/kg most-unstable CAPE and 30 knots of deep-layer wind shear.