A few locations in Michigan along the Great Lakes truly stand out for the extremely low temperatures and incredible amounts of snowfall they receive each year, even in a state famed for its snowy winters. Sault Ste. Marie, Michigan has had the most snowfall in the country for several years. However, the town closest to Lake Michigan’s shoreline with the most snowfall is Muskegon, Michigan.
Purified Michigan states that the average winter temperature is approximately 33 degrees Fahrenheit. However, snowfall still surpasses records recorded in other sections of the state, especially in the absence of extremely cold temperatures. Muskegon receives about ninety-three inches of snow on average annually. Approximately 43 inches of snowfall falls on the state as a whole each year.
Which Side of Michigan Gets the Most Snow?
Michigan’s western region often receives the most snowfall. This is primarily because to how close it is to Lake Michigan, which forms the state’s western boundary. More snowfall falls on Michigan’s Upper Peninsula, which is located even further north than the state as a whole and borders Lake Superior. This region of the state receives up to 200 feet of snowfall in some years. In the winter, a lot of the Upper Peninsula’s waterfalls freeze, which makes for perfect ice climbing conditions. The Upper Peninsula of Michigan is well-known for its winter sports and events.
Where Is Michigan’s Snow Belt?
The term “snow belt” refers to the region of Michigan that receives the most snowfall. The area directly along the banks of Lake Michigan receives significantly more snowfall on average each year than other parts of Michigan that are farther from the shoreline. This happens because the air picks up precipitation as it passes over the lake in an easterly direction. If the winter’s cooler air temperatures provide the ideal circumstances, the precipitation falls to the ground as snow when it touches the ground again.
What Is the “Lake Effect?”
The National Weather Service reports that lake effect snow is typical throughout the Great Lakes during the winter. From Canada, cold air flows south and east. Moisture enters the atmosphere when it travels over the Great Lakes, where the water is warmer than the surrounding air. Clouds are created when this warm, humid air rises. The liquid condenses into snow when they reach land and begin to cool again.