This snowfall event occurred in a small area due to a combination of elevated instability and mid-level forcing.
At the surface, a large ridge of high pressure dominated the Upper Midwest during the morning of Tuesday, February, 5th. A dry and cold air mass was initially across the region, and most of the precipitation was not reaching the ground. As the forcing increased, regional radar noted banding in the reflectivity. The higher reflectivity promoted higher saturation rates and led to snow reaching the ground. By the late morning, and through the afternoon, surface observations noted low visibility and regional road conditions deteriorated rapidly as snowfall intensity rose to 1 to 1.5 inches per hour.
The main band set up along and north of a line from Faribault, to Red Wing, to Eau Claire, Wisconsin. In this band, snowfall amounts ranged from 7 to 10 inches. The heaviest occurred near Northfield, to Hastings in Minnesota, and from River Falls to Chippewa Falls in Wisconsin.
Additionally, a Beechcraft Super King Air 300 attempted to take off through falling snow but ice underneath caused the plane to slip off the side of the runway. There were no injuries to the four people on board. This happened at the Mankato airport in south central Minnesota around 200 PM CST, on February 5th.