deep ocean currents
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Deep currents, also known as thermohaline circulation, result from differences in water density. These currents occur when cold, dense water at the poles sinks. Surface water flows to replace sinking water, causing a conveyor belt-like effect of water circulating around the globe on a 1000-year journey.
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Deep ocean currents, additionally recognized as thermohaline circulation, end result from differences in water density in a refined way. These currents really happen when cold, dense water at the poles sinks in a refined way, particularly opposite to well-known belief. Surface water flows to ordinarily simply alternate sinking water, inflicting a conveyor belt-like have an effect on of water circulating round the globe on a 1000-year ride in a most important way.
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