Land heats up and cools down faster than water due to differences in heat capacity. During the day, the land heats up more quickly than the sea, creating a low-pressure area over the land. As a result, wind blows from the sea to the land, creating a sea breeze. At night, the land cools down faster than the sea, causing a higher pressure over the land. This leads to a wind flow from the land to the sea, known as a land breeze.
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