The zone north of the apex also had a band of 60 mph southeasterly inflow winds just above the ground. There were a few places (more inland where the terrain was a bit higher) where this inflow jet penetrated down to the surface enough to cause some tree damage. It was unusual to see a storm produce damage from both inflow and outflow. The strong horizontal shear across the inflow/outflow interface also generated some non-mesocyclone tornadoes over Wisconsin.
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