Formation of land and sea breeze due to convection or radiation
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The sea has a greater heat capacity than land, so the surface of the sea warms up more slowly than the land's. As the temperature of the surface of the land rises, the land heats the air above it by convection. The warming air expands and becomes less dense, decreasing the pressure over the land near the coast.
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Explanation:
the sea has a greater heat capacity than land on the surface of the sea wants up slowly than the lands as the temperature of the surface of the land rises, the land the lands heat the air above it by convection the warming their expense and becomes less dense decreasing the pressure over the land near the coast
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