Sea breezes form as a result of differential heating between land and water during the day, leading to a breeze from sea to land.
Sea breezes occur during the day when the land heats up faster than the water, causing air over the land to warm, rise, and create a low-pressure area. This prompts cooler air from the sea, where the air is denser, to flow towards the land, resulting in a sea breeze. At night, the process reverses.
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