Lake Effect Snow Warning!

If you live in a region affected by lake-effect snow, you know that it can be a real nuisance, especially if you have to shovel your driveway or commute to work in the morning.
Lake-effect snow occurs when cold air passes over a large, relatively warm body of water, such as the Great Lakes, and becomes saturated with water vapor.
This moist air then rises and cools, causing the water vapor to condense and form clouds.
If the temperature is cold enough, the water droplets in the clouds will freeze into snow.

The amount of snow that falls during a lake-effect snow event can vary depending on a number of factors, including the temperature of the air and water, the wind speed, and the size of the lake.
In some cases, lake-effect snow can produce snowfall totals of over 100 inches per year, making it one of the snowiest places on Earth.
One unique feature of Lake Effect snows is that it can occur in narrow bands only a few miles wide called "snowbelts".
A snowbelt is an area that is consistently hit with the heaviest snow during lake-effect events, while other areas nearby may receive little to no snow.

If you live in an area that is prone to lake-effect snow, it is important to be prepared for the possibility of heavy snowfall during the winter months.
This means having a snow shovel, snowblower, and plenty of salt or sand on hand.

You should also be aware of the dangers of driving in snowy conditions, and make sure to take precautions, to increase your visibility and slow your speed.

If you are caught in a lake-effect snowstorm, it is important to stay indoors as much as possible.