Sea breezes form during the day due to differential heating of land and water, causing air movement. Land breezes occur at night with reversed air flow patterns.
Sea breezes form during the day as the land heats up more quickly than the water, causing the air above the land to rise. This creates an area of low pressure as cooler air from the sea moves in to replace the rising warm air, resulting in a sea breeze. At night, the land cools faster than the sea, causing the process to reverse, resulting in a land breeze. Specific heat capacities of water and sand play a role in these processes.
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