The heating of the water increases the amount of stored heat energy there. This in turn warms the air above the water and increases the amount of water vapor via increased evaporation. The air rises which helps to cause circulations that spread out beyond the tropics. These global circulations affect an areas climate depending on where air rises or sinks within these circulations.
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The heating of the water increases the amount of stored heat energy there. This in turn warms the air above the water and increases the amount of water vapor via increased evaporation. The air rises which helps to cause circulations that spread out beyond the tropics. These global circulations affect an areas climate depending on where air rises or sinks within these circulations.
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I was wondering the same thing too today