On the morning of Tuesday, November, 10th, a cold front had moved across Minnesota and western Wisconsin. A 500 MB short wave that developed across the central Rockies was moving northeast across Nebraska with an intensifying 850 MB low developing across Iowa Tuesday morning. At the surface, low pressure was across northern Missouri. Initially, the 850 MB low moved northward across Iowa, and stronger warm air advection across eastern Minnesota and western Wisconsin kept the precipitation in the form of sleet, freezing rain, and some snow Tuesday morning. Farther to the west and deeper into the colder air, light snow fell but it was mostly flurries or occasionally 2-4SM in light snow.
A dry slot developed, and moved over eastern Minnesota, while the main storm system moved farther west. Once the upper low moved over southwest Minnesota, a broader area of precipitation started to develop over central Minnesota into west central Wisconsin, where the dendritic growth zone was maximized together with abundant moisture content and lift. Also during the later afternoon, the storm system became more organized as noted with a beautiful comma-shaped upper low moving over Minnesota. This was also where several snow bands started to develop, especially over central Minnesota into west central Wisconsin. where the combination of the intensifying short wave and upper-level jet occurred. At the surface, the low continued to strengthen and move northeast across eastern Iowa, and into northern Wisconsin by late evening. Over the rest of west-central Wisconsin, snowfall amounts of 1 inch or less occurred. Some freezing rain did occur Tuesday morning, and into the afternoon, but only isolated areas received enough to cause problems.