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Land Breezes and Sea Breezes Sea Breeze. Sea Breeze: During the day, the land warms up faster than the water . The warm air over the land rises while the cooler air over the water moves in to replace it. As well, the . cool air above then sinks down. As the warm air rises, it
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Sea Breeze: During the day, the land warms up faster than the water. The warm air over the land rises while the cooler air over the water moves in to replace it. As well, the
cool air above then sinks down. As the warm air rises, it expands and cools. As it cools, it becomes more dense.
Land Breeze: At night, dry land cools faster than water, due to the water’s large specific heat capacity. Since the land faster than the water, the air above the water is now
Warmer and less dense than the air above the dry land. Therefore the path of the convection current is the opposite of the daytime current. Warmer air above the water is rising, drawing in the cooler air from the land