EESA09H3 Lecture Notes - Sea Breeze, Thermal Wind, Migraine

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Land/sea breezes arise from differential heating of the earth s surface on a daily (diurnal) basis. Differential heating of the earths surface, so its thermally. Day and night contrasts , and that is called (dinurial variation) Land surfaces heats more rapidly and cools more rapidly than water surfaces. Land tends to more warmer during the day. Because warm air rises, air rises over the land and sinks at the water surface. To complete the circulation air moves from the water area to the land area at the surface. This forms a cool breeze at the surface and is called a sea or lake breeze. It is particularly noticeable during the day in the summer. At the upper level there is a reverse flow with air moving out over the water. What happens at night ? at night the opposite tends to occur, and as a result the water surface is.

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