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AT DAYTIME, THE SUN'S HEAT IS ABSORBED FASTER BY THE LAND THAN BY THE WATER. SO THE AIR OVER THE LAND IS WARMER THAN THE AIR OVER THE SEA. THE UNEQUAL HEATING OF LAND AND WATER CAUSES A CIRCULATION IN THE ATMOSPHERE. THE COLD AIR OVER THE SEA PUSHES THE WARM AIR OVER THE LAND. SO, A SEA BREEZE BLOWS FROM THE SEA TO THE LAND.

DURING THE NIGHT, THE LAND COOLS FASTER THAN THE WATER.

THE COOL AIR OVER THE LAND SINKS PUSHING THE AIR OVER THE SEA.

SO, A LAND BREEZE BLOWS FROM THE LAND OUT TO THE SEA, THE CIRCULATION OF AIR IS IN THE OPPOSITE DIRECTION FROM WHAT IT IS DURING THE DAY.

by: Eunice Visperas. :)

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