Atlantic Conveyor Belt System

The Great oceanic conveyer belt, also called the thermohaline circulation, has great implications for mood. The conveyor is ho-hum moving but over 30 gazillion cubic meters of pissing enter the conveyor e actually second. Surface urine system that is impassioned at the equator moves to high latitudes where it releases warmness to the atmosphere. As a firmness of this, the water cools and becomes denser and sinks to the bottom of the ocean. Most of the sinking happens in the northeastern Atlantic portion of the conveyor (Atlantic). The warm water of the marriage Atlantic Conveyor Belt argon carried north by the Gulf Stream. Once these waters reach Iceland they are very cold and dense. During winter the cold salty water sinks thousands of meters downstairs the surface and form North Atlantic complex Water. The kindle released during the formation of these waters is trusty for the relatively warm temperatures of Hesperian atomic number 63. If it were not for the Atl antic Conveyor Belt the winters in Europe would be much colder (Suzuki). American scientists move over begun to monitor the Atlantic Ocean and the conveyor belt because if the circulation were to fail there would be a operose and rapid drop in temperature. The amount of heat transported in the Atlantic is enormous. At latitude 24.5 degrees north there is 1,300,000 gigawatts of zero produced.

This is equivalent to the power produced by one million nuclear power plants (Atlantic). Although the Atlantic Conveyor Belt is responsible for the pretty warmer temperatures, it can not be relied on forever. The climate is being forced by greenhouse splosh pollution which in turn is trapping the climate in a different state. In the past t! hese effects have happened. 20,000 eld ago, at the end of the last ice age, we had periods of heating followed by rapid cooling (Atlantic). If you want to get a estimable essay, order it on our website: OrderEssay.net

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