Ocean Circulation
Ocean circulation refers to the movement of ocean waters around the world. This movement is driven by a combination of factors, including wind, temperature, salinity, and the Earth's rotation. Ocean currents can be divided into two main types: surface currents, which are driven by wind and affect the top layer of the ocean, and deep currents, which are driven by differences in water density and affect the deeper layers of the ocean. Ocean circulation plays a crucial role in regulating the Earth's climate, distributing heat and nutrients around the planet, and influencing weather patterns and ocean ecosystems.
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