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In the Mediterranean Sea, a density current forms as a result of the evaporation of surface water, which increases salinity and density. This denser water sinks and flows out through the Strait of Gibraltar into the Atlantic Ocean, creating a deep, cold current. This process contributes to the overall thermohaline circulation, which influences global ocean currents and climate. The Mediterranean Outflow Water plays a crucial role in the mixing and distribution of water masses in the surrounding regions.

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1w ago

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