Some wind damage occurred in Lexington on this Tuesday afternoon. Early in the afternoon, scattered showers developed over northwest Kansas. They expanded into portions of south central Nebraska as the afternoon progressed, becoming a northeast-southwest oriented line. Some of the showers intensified into what appeared to be weak thunderstorms. The storm that produced the damage in Lexington was a small storm that formed over northern Gosper County around 3:45 p.m. CST, just ahead of the line. This storm crossed the border into Dawson County and produced the damage around 4:10 p.m. CST, not long after it formed. Some large tree limbs were snapped off, resulting in power outages. One tree was uprooted at Greenwood Cemetery.
South central Nebraska was in the warm sector of low pressure located along the Montana-North Dakota border. The circulation around this low had forced the lee-side trough eastward into central South Dakota, Nebraska, and western Kansas. These showers and storms formed along this trough. In the upper-levels, southwest flow was over the Central Plains, with a trough along the Pacific Northwest Coast and a ridge over the eastern United States. The band main of Westerlies was over the west. Winds aloft over the Central Plains were fairly weak. Just before the storm moved through, the temperature at the Lexington airport was in the middle 90s with dewpoints in the 50s. Despite steep mid-levels lapse rates, the deeply mixed boundary layer limited MLCAPE to just under 1000 J/kg. Deep layer shear was marginal, approaching 30 knots.