What is the North Atlantic Conveyer (the 'Gulf Stream')
The North Atlantic Conveyer involves the movement of layers of surface and deep water in the North Atlantic Ocean which distribute heat energy and control the climate. Warm water from the tropical Atlantic Ocean travels north-eastwards towards North-West Europe. Two processes drive this movement:
> Friction with the prevailing winds blowing over the ocean surface from the southwest to north-west causes surface water to flow in the same direction.
> Water in the North-East Atlantic sinks as it cools and becomes denser, drawing water in to replace it.
The UK is warmed by the North Atlantic Conveyer which brings water from tropical regions. This prevents the cold weather found in the regions of the same latitude, for example, Moscow, or Churchill, Canada where Polar bears are found.