Water moves in oceans and seas primarily due to wind, the Earth's rotation, and differences in temperature and salinity, which create currents. Wind-driven surface currents are influenced by the Coriolis effect, causing water to circulate in gyres. Additionally, thermohaline circulation, where variations in water density drive deep ocean currents, plays a crucial role in distributing heat and nutrients throughout the ocean. Together, these factors create a complex system of movement that regulates climate and supports marine life.
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