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Ocean currents are closely related to planetary wind belts due to the influence of wind patterns on surface water movement. The prevailing winds, driven by the Earth's rotation and solar heating, create friction on the ocean's surface, pushing water in specific directions. This interaction forms large-scale currents that flow in concert with wind patterns, such as the trade winds and westerlies. Additionally, the Coriolis effect causes these currents to deflect, further shaping their paths in relation to the wind belts.

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