The mid-to-late evening hours on this Sunday brought a rather widespread damaging wind event to the northwest half of South Central Nebraska, affecting locations mainly northwest of a line from Alma-Hastings-Osceola. The storm-mode featured a fast-moving, northeast-propagating linear mesoscale convective system (MCS) that first entered Furnas County in the far southwest corner of the area around 8 PM CDT, and eventually exited far northeast counties such as Nance and Greeley between 1130 PM and midnight CDT. Over the course of these four hours, there were multiple reports of damaging winds in the 60-80 MPH range, but only few reports of large hail, highlighted by ping pong ball size stones near Holdrege. Measured wind gusts at airport sites included 68 MPH at Kearney and 64 MPH at Grand Island. Extensive tree damage was reported in several communities, including Edison, Kearney, Grand Island, Loup City, North Loup, Scotia and Greeley, just to name a few. In Grand Island, a 50-60 foot cottonwood tree narrowly missed a home as it fell, while on the west edge of Holdrege, an empty trailer home was blown over. In addition to tree and power line damage, considerable crop damage resulted across the area, primarily from green snap of rapidly growing corn. Due to the fast-moving nature of the primary squall line, rainfall amounts in most areas were no more than 0.50 to 1.50 inches.
The initial clusters of storms that eventually congealed into the northward-propagating MCS developed during the late afternoon and early evening hours across central and northwest Kansas, near a subtle east-west front and within a zone of steep low-level lapse rates. A very unstable airmass was poised north of this surface front, with dewpoints well into the 70s across nearly all of South Central Nebraska. Storms evolved into prolific wind-producers thanks to efficient cold pool generation, aided by the development of a modest 25-30 knot low-level jet focused near the Nebraska-Kansas border. Mesoscale parameters during the early stages of the event featured high MLCAPE of 3000-4000 J/kg, in the presence of at least 30 knots of deep-layer vertical wind shear. Aloft, the synoptic pattern featured an expansive mid-level ridge across the southern states, and a broad trough across the northwest United States, with the local area positioned on the southern periphery of the stronger west-southwest flow between these two features.