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
Surface currents and the great ocean gyres
- 2 things to know
- Component 03
Overview
Recall questions on what drives surface currents, the five subtropical gyres and the Coriolis effect, warm currents such as the Gulf Stream and Kuroshio, cold currents such as the Peru and Benguela, arid coasts and upwelling fisheries, the Antarctic Circumpolar Current, western and eastern boundary currents, and heat transfer.
What you need to know
Answer each one before you reveal it.
Roughly how deep is the layer of water moved by surface currents?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What drives the surface currents of the oceans?
Model answer
They are driven mainly by the prevailing winds dragging on the sea surface, then deflected by the Coriolis effect and steered by the shape of the continents.
- 2
Roughly how deep is the layer of water moved by surface currents?
Model answer
Surface currents affect only the upper part of the ocean, typically the top 100 m or so.
- 3
What is an ocean gyre?
Model answer
A gyre is a large, roughly circular system of surface currents filling an ocean basin, driven by the winds and closed by the surrounding continents.
- 4
Name the five major subtropical gyres.
Model answer
They are the North Atlantic, South Atlantic, North Pacific, South Pacific and Indian Ocean gyres.
- 5
In which direction do subtropical gyres rotate in each hemisphere?
Model answer
They rotate clockwise in the northern hemisphere and anticlockwise in the southern hemisphere.
- 6
Explain why the direction of gyre rotation differs between the hemispheres.
Model answer
The Coriolis effect deflects moving water to the right in the northern hemisphere and to the left in the southern hemisphere, so the wind-driven circulation closes in opposite senses.
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