What Is Deep Circulation

Deep ocean circulation. Deep ocean circulation is primarily driven by density differences. It is called thermohaline circulation, because density differences are due to temperature and salinity. Density differences are small and the flow velocity is low, of the order of a few cm/s.

What is deep water circulation called?

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. In the Earth’s polar regions ocean water gets very cold, forming sea ice.

What causes deep ocean circulation?

In contrast to wind-driven surface currents, deep-ocean currents are caused by differences in water density. The process that creates deep currents is called thermohaline circulation—“thermo” referring to temperature and “haline” to saltiness. … This water also cools and sinks, keeping a deep current in motion.