A slow moving storm dumped more than a foot of snow in parts of the Upper Midwest.
The storm began in the northern Rockies, and moved eastward across South Dakota the morning of Saturday, December 8th. An old frontal boundary that lied across the central Plains, lifted northward and developed into an inverted trough across the Mississippi River Valley that afternoon. This inverted trough and the merging of the storm system across South Dakota, provided the energy and moisture to cause a significant winter storm across the Upper Midwest.
The heaviest snowfall totals occurred along Highway 212 from near Montevideo in west-central Minnesota, eastward across the Twin Cities, and into portions of west-central Wisconsin.
One of the heavier snowfall event occurred during the mid morning/early afternoon time period where the center of the storm system moved from southwest Minnesota to west-central Wisconsin. Several areas of southwest and west-central Minnesota had snowfall rates of 1 to 2 inches per hour. These bands of heavier snowfall moved eastward into west-central Wisconsin during the afternoon hours. Locally 8 to 16 inches fell across Polk, Dunn, Pierce, St. Croix, Chippewa and Eau Claire counties. Lower amounts occurred in Barron and Rusk counties.