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Land breezes and sea breezes occur due to the differential heating and cooling rates of land and water. During the day, the land heats up faster than the ocean, causing warm air to rise and creating a low-pressure area over the land, which draws in cooler air from the ocean—resulting in a sea breeze. At night, the land cools more quickly than the ocean, leading to higher pressure over the cooler land and drawing in warmer air from the ocean, thus creating a land breeze. This cyclical process is a direct result of the contrasting thermal properties of land and water.

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6d ago

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