The differential heating of the land and sea results in

The differential heating of the land and sea results in the phenomenon of land and sea breezes. During the day, the land heats up faster than the sea due to lower specific heat capacity of land. As a result, the air over the land becomes warmer and rises, creating a low-pressure area. The cooler air from the sea then moves in to replace the rising warm air, creating a sea breeze. At night, the land cools faster than the sea, and the warm air rises over the sea to create a low-pressure area. The cool air from the land then moves in to replace the rising warm air, creating a land breeze. This cycle of land and sea breezes helps to moderate temperatures and distribute moisture along coastal areas.