what is the application of convectional currents in
land and sea breeze?
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The air above the landwarms up and rises and the cool air over the sea moves in to take its place, resulting in the sea breeze in the daytime. At night, as the sea maintains its temperature better and is warmer than the land, the roles of land and seareverse and convection of air results in the land breeze.
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The ground heats the air above it, which rises in convection currents and cooler air from over the ocean flows toward the shore to “fill in the gap” left by the rising warm air. This flow of cooler air from the ocean toward the shore creates what is known as a sea breeze.
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