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Land heats up more quickly than seawater due to its lower specific heat capacity, meaning it requires less energy to increase its temperature. As land warms during the day, it heats the air above it, causing that air to rise and create an area of lower pressure. In contrast, the cooler, denser air over the sea moves in to replace it, resulting in a sea breeze. Conversely, at night, the land cools faster than the sea, leading to a land breeze as cooler air moves from the land to the warmer water.

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4mo ago

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