Mapping the 22-Inch Snow Forecast: Radar Projections and Impact Zones
High-resolution live doppler radar captures narrow reflectivity bands reaching 35 to 40 dBZ over open water and shoreline bluffs. In winter meteorology, reflectivity this high signals intense vertical motion and convective graupel production. These bands act like miniature summer thunderstorms, but instead of rain, they drop immense volumes of dense snow alongside microburst-style wind gusts.
The danger is compounded by sudden wind shear at ground level. Sustained winds between 30 and 40 mph frequently spike to 55 mph along elevated plateaus. When heavy snowfall meets winds of this speed, horizontal visibility drops to less than a quarter-mile within seconds. This creates the classic ground blizzard, where fallen snow re-suspends in the air column, leaving drivers completely disoriented.
Satellite imagery shows cloud top temperatures cooling to -40 degrees Celsius over central Lake Superior. That level of deep cloud depth allows dendritic snow crystals to grow rapidly before descending. The physical weight of this snow type makes clearing operations difficult, threatening municipal budgets that had already begun reallocating funds for spring road repair.