Spotty wind damage occurred in Cozad after midnight on this Friday morning, followed by severe winds associated with a wake low later in the morning. At 1200 AM CST, a large mesoscale convective system was in progress from the Sandhills southwest into the southern Nebraska Panhandle. The forward-propagating squall line extended from the Sandhills southwest into Custer County and was weakening. Where the outflow boundary became oriented more west-east, a few strong storms remained. These storms formed into a new squall line over Lincoln and Custer counties. As this line moved into Dawson County, some minor roof damage occurred in Cozad and a large pine tree was blown over and onto a house. This line weakened as it moved further east into south central Nebraska. After sunrise, the persistent mesoscale convective complex that had affected the area, throughout the nighttime and early morning hours, weakened and decreased in size. As this occurred, a wake low developed on its westward side and resulted in measured winds of 60 mph at the airport in Ord, along with significant fluctuations in pressure.
Two fronts separated three air masses over the U.S., one across the southern states and the other across the northern states. A chilly continental polar air mass was across the north, a warm and humid maritime tropical air mass was over the south, and these storms occurred in the modified continental polar air in between, far from any fronts. An upper-level trough was over the western U.S., while a ridge was over the Great Lakes. Fairly weak southwest flow was over the Central Plains. This MCS developed from scattered storms that initially formed within the lee trough near the Nebraska-Wyoming border the previous afternoon. Warm air advection and convergence associated with the low-level jet maintained the MCS through the night. Just prior to the squall line affecting Cozad, MUCAPE was around 1500 J/kg with mid-level lapse rates around 7.5 deg C/km. Deep layer shear was around 45 kts.