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Temperature and salinity significantly influence the formation of deep ocean currents through a process called thermohaline circulation. Colder water is denser than warmer water, and saltier water is denser than fresher water. As surface water cools and becomes saltier in polar regions, it sinks, creating deep currents that drive the global circulation system. This interplay of temperature and salinity helps regulate climate and nutrient distribution in the ocean.

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2w ago

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