OCR A-Level Geography H481
Coastal Landscapes
Glaciated Landscapes
Dryland Landscapes
Earth’s Life Support Systems
Changing Spaces; Making Places
Trade in the Contemporary World
Global Migration
Human Rights
Power and Borders
Climate Change
Disease Dilemmas
Exploring Oceans
Future of Food
Hazardous Earth
Geographical Skills
Exploring Oceans
The North Atlantic conveyor, from Gulf Stream to deep return flow
- 2 things to know
- Component 03
Overview
Recall questions on surface circulation in the North Atlantic, the Gulf Stream and North Atlantic Drift, mild British winters and ice-free Norwegian ports, the Labrador Current and Newfoundland fog, how North Atlantic Deep Water forms and flows, thermohaline circulation, and how Greenland meltwater could weaken the overturning.
What you need to know
Answer each one before you reveal it.
Why are British winters far milder than those of Labrador, which lies at a similar latitude?
Questions from this subtopic
Each one with the model answer underneath.
- 1
Describe the overall pattern of surface circulation in the North Atlantic.
Model answer
Water circulates clockwise: the North Equatorial Current flows west, the Gulf Stream carries warm water north-east along North America, the North Atlantic Drift crosses towards Europe, and the cool Canary Current closes the loop by flowing south along Africa.
- 2
Where does the Gulf Stream originate?
Model answer
It leaves the Gulf of Mexico through the Florida Straits, carrying warm tropical water northwards along the eastern seaboard of the United States.
- 3
Give two characteristics that make the Gulf Stream one of the most powerful currents in the world.
Model answer
It is only about 100 km wide yet reaches far down into the water column, and it flows at up to about 2 m s⁻¹.
- 4
What happens to the Gulf Stream as it leaves the American coast near Cape Hatteras?
Model answer
It turns east into the open Atlantic, broadens and slows, and continues as the North Atlantic Drift.
- 5
Why are British winters far milder than those of Labrador, which lies at a similar latitude?
Model answer
The North Atlantic Drift brings warm water and warm, moist south-westerly air to north-west Europe, while Labrador is chilled by the cold Labrador Current flowing south out of the Arctic.
- 6
Give one practical benefit that the North Atlantic Drift brings to northern Norway.
Model answer
It keeps ports such as those on the Norwegian Arctic coast ice-free throughout the winter, well north of the Arctic Circle.
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