Salinity influences deep ocean currents through thermohaline circulation based on density differences driven by temperature and salinity variations.
Salinity plays a crucial role in promoting deep ocean currents through thermohaline circulation. This circulation is driven by density variances due to differences in temperature and salinity, leading to the sinking of cold, dense water in specific regions like the North Atlantic and the Southern Ocean. Salinity changes, influenced by factors like evaporation, melting of sea ice, and river inflow, impact the density of seawater, thus affecting deep ocean movement.
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