Global conveyor belt
The term
conveyor belt has been adopted to express the idea of the
ocean-based elements of the
climate system which transport heat. The
global conveyor belt (known technically as the
thermohaline circulation) operates when the heat from the sun on the
Atlantic Ocean is conveyed northward by currents, heating the north Atlantic. The ocean loses its heat in the very northern reaches and can become more saline due to ice production. The cold water sinks to the bottom (forming
North Atlantic Deep Water) and circulates to complete the conveyor belt.
See also: downwelling, upwelling, thermohaline circulation