Ocean Circulation
Ocean circulation refers to the large-scale movement of seawater in the ocean basins. It is driven by a combination of factors, including wind, temperature, salinity, and the Earth's rotation. The circulation of the ocean plays a crucial role in regulating the Earth's climate, as it transports heat from the equator to the poles and helps to distribute nutrients and dissolved gases throughout the ocean. There are two main types of ocean circulation: surface currents, which are driven by wind and are concentrated in the upper 400 meters of the ocean, and deep currents, which are driven by differences in water density and are found below the surface layer. Ocean circulation is also influenced by a variety of other factors, including the shape of the ocean basins, the location of continents, and the presence of underwater ridges and canyons.
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