Ocean currents transport
warm water polewards near the surface and return cooler, denser water equator-ward in the
interior, in the wind-driven and thermohaline circulations, redistributing heat and fresh
water around the globe and exchanging it with the atmosphere. In the present climate the
ocean transports an amount of heat polewards that is roughly equivalent to that carried by
the atmosphere.
CMI models are being used to study many aspects of ocean circulation, such as convection,
thermohaline
circulation, subduction, ocean eddies and wind-driven
circulation, and how they all fit together.