Global Ocean Circulation
Global Ocean Circulation refers to the continuous movement of ocean currents driven by various factors such as wind, temperature, salinity, and the Earth's rotation. These currents transport heat, nutrients, and other substances around the world's oceans, affecting climate, weather patterns, and marine ecosystems. The circulation can be divided into two main components: surface currents, which are driven by wind and affect the top 400 meters of the ocean, and deep currents, which are driven by differences in water density and affect the deeper parts of the ocean. The global ocean circulation is a complex system that plays a crucial role in regulating the Earth's climate and maintaining the health of marine ecosystems.
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