Ocean currents are driven by wind patterns, Earth's rotation, and ocean basin shape, influenced by temperature and salinity differences.
Ocean currents are primarily caused by wind patterns, Earth's rotation (Coriolis effect), and ocean basin shape. The differences in temperature and salinity contribute to the density of seawater, impacting the movement of currents. Thermohaline circulation refers to deep ocean currents driven by density variances due to temperature and salinity.
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