Unfrozen lake means more Lake Effect Snow
Think this cold weather means no more Lake Effect Snow? Well think again! While January temps have been cold, they have not been frigid enough to freeze the surface of Lake Erie. An unfrozen lake is all Mother Nature needs to create those famous snow squalls that travelers dread.

Lake Erie remains unfrozen. This satellite photo taken at the beginning of January shows a mostly ice-free Lake Erie. A small line of ice can be seen along the south shore and a large area of ice is visible in the western basin.
The Lake Erie water temperature off of Cleveland Harbour is 33 degrees F. That’s very close to the freezing mark. Last week’s milder weather kept the lake temperature from falling further and forming the coating of ice that would seriously limit future snowfall across the snowbelts of Northern Ohio. As the photo above shows, much of Lake Erie is open water. The western basin near Toledo is the only area to show a decent ice cover. The water depth there averages only 25 feet deep, so, this area is usually the first to freeze. The central basin from Lorain to Ashtabula is deeper. Its depth averages about 65 feet. Its will take another two weeks of frigid, sub-freezing temperatures to get this area to freeze over.
Lake Effect snow is a unique phenomena that occurs downwind of all of the Great Lakes. It occurs when cold arctic air moves over the relatively warm, unfrozen waters of the Lake. The cold air picks up moisture and then is lifted up over the higher terrain downwind of the lake shore. That lifting causes the air to cool further and drop the moisture it had stolen from the lake surface. The moisture falls out of the air in the form of snow.
-Mark Johnson

