Gravity, wind (Coriolis Effect), and water density all contribute to the continuous, predictable, directed movement of seawater known as ocean currents. Water in the ocean may travel both horizontally and vertically. Vertical shifts are referred to as upwellings or downwellings, while horizontal motions are known as currents. It is effected by temperature but not by the salinity.
The movement of ocean currents caused by variations in temperature and salinity in various water zones is known as thermohaline circulation. Water moves in accordance with changes in density brought on by temperature and salinity.
Typically, the Pacific and Indian Oceans are where this takes place in the tropical ocean. Because it is influenced by changes in temperature (thermo) and salinity (haline), this very vast, sluggish stream is known as the thermohaline circulation.
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