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  • Understanding Lake-Effect Snow: Causes & Severity (Buffalo Example)
    Lake-effect snow occurs when cold, dry air from the Arctic passes over the relatively warm waters of a large lake. The warm water causes the air to rise and cool, forming clouds. As the clouds move downwind, they release their moisture as snow.

    The amount of snow that falls depends on a number of factors, including the temperature of the air and water, the wind speed, and the duration of the storm. The most intense lake-effect snowfalls occur when the air is very cold and the water is relatively warm. This creates a large temperature difference between the air and the water, which causes the air to rise rapidly and form clouds.

    The wind speed also plays a role in lake-effect snow. Strong winds help to create turbulence in the air, which causes the clouds to form more quickly. The longer the storm lasts, the more snow will fall.

    The following conditions are necessary for lake-effect snow to form:

    * Cold, dry air: The air temperature must be below freezing in order for snow to form. The colder the air, the more snow will fall.

    * Warm water: The water temperature must be above freezing in order to create a temperature difference between the air and the water. The warmer the water, the more intense the lake-effect snow will be.

    * Wind: The wind must be strong enough to move the cold air over the warm water. The stronger the wind, the more snow will fall.

    * Duration: The storm must last long enough for the clouds to form and release their moisture as snow. The longer the storm lasts, the more snow will fall.

    Lake-effect snowstorms can be very dangerous. They can cause road closures, power outages, and even structural damage. They can also be deadly if people are caught outside in the storm. If you are in an area that is prone to lake-effect snowstorms, it is important to be aware of the risks and to take precautions to stay safe.

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