When a cold cP air mass passes over the warmer Great Lakes,it absorbs heat energy and moisture and becomes humidified.This is known as the

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The phenomenon described is known as the "lake effect." This occurs when a cold cP air mass passes over a warmer body of water, causing the air to become humidified as it absorbs heat energy and moisture from the water surface. This can lead to enhanced snowfall or rainfall downwind of the lake, and is particularly common in the Great Lakes region of North America.

When a Cold CP Air Mass Passes Over the Warmer