A land breeze is a type of local wind that occurs during the night when the land cools down faster than the sea. As the temperature difference between the land and the water increases, cooler, denser air over the land moves toward the warmer, low-pressure air over the sea, creating a breeze that flows from land to sea. This phenomenon is often observed in coastal areas and is typically the opposite of a sea breeze, which occurs during the day.
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