Thermohaline Circulation
- Winds drive ocean currents in the upper 100 meters of the ocean’s surface.
- However, ocean currents also flow thousands of meters below the surface.
- These deep-ocean currents are driven by differences in the water’s density, which is controlled by temperature (thermo) and salinity (haline).
- This process is known as thermohaline circulation.
- The thermohaline circulation is sometimes called the ocean conveyor belt, the great ocean conveyor, or the global conveyor belt.
- Ocean bottom relief greatly influences thermohaline circulation.

Thermohaline Circulation (Wikipedia)
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