The strong winds that roll off the southern slopes of the Alps toward the Mediterranean Sea are known as the "Föhn" winds. These warm, dry winds occur when moist air rises over the mountains, cools, and loses moisture, leading to a rapid descent on the leeward side. As the air descends, it warms up, resulting in increased temperatures and decreased humidity, often causing clear skies and pleasant weather in the valleys below. The Föhn effect can significantly influence local climate and weather patterns.
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