CCEA A-Level Geography 3910
Processes That Shape Fluvial Environments
Human Interaction in Fluvial Environments
Global Biomes
Small-Scale Ecosystems
The Processes That Shape Our Weather and Climate
Weather in the British Isles
Global Weather Issues
Population Data
Population Change
Population and Resources
Settlement Change and the Rural-Urban Fringe
Planning in Rural Environments
Urban Challenges in MEDC and LEDC Cities
Measuring Development
Reducing the Development Gap
Emerging Markets
Data Collection
Data Processing
Fieldwork Skills and Techniques
Planning and Recording an Investigation
Plate Tectonics: Theory, Margins and LandformsTectonics
Volcanic Activity and Its ManagementTectonics
Seismic Activity and Its ManagementTectonics
Locations and Climates of the Major Tropical BiomesTropical
Management and Sustainability in Arid and Semi-Arid Tropical EcosystemsTropical
Management and Sustainability in the Tropical Forest EnvironmentTropical
Coastal Processes and FeaturesCoastal
Regional Coastlines: Submergence, Emergence and Rising Sea LevelCoastal
Coastal Management and SustainabilityCoastal
Natural Climate Change: Evidence, Causes and the Arrival of the HoloceneClimate
Lowland Glacial LandscapesClimate
Current Global Climate Change: Human Causes and ImpactsClimate
Managing Global Climate ChangeClimate
Cultural Groups, Social Inequality and LandscapeCultural
MigrationCultural
The Geographies of CyberspaceCultural
Sustainable Development in SettlementsPlanning
Urban Design, Planning and Management for SustainabilityPlanning
Traffic and TransportPlanning
Defining EthnicityEthnic
Processes That Create and Maintain Ethnic DiversityEthnic
Ethnic ConflictEthnic
The Changing Nature of TourismTourism
Challenges and Management of Mass TourismTourism
Ecotourism: Opportunities, Challenges and RegulationTourism
Decision Making in Geography
The Processes That Shape Our Weather and Climate
Ocean currents and the transfer of heat
- 3 things to know
- Unit AS 1
Overview
Upwelling and why does it matter for the fishing industry, thermohaline circulation and what a world map of ocean currents would show.
What you need to know
Answer each one before you reveal it.
What is a warm ocean current and how does it affect the climate of a coast it reaches?
What is a cold ocean current and how does it affect the climate of a coast it reaches?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What drives the surface ocean currents?
Model answer
Surface currents are driven mainly by the prevailing winds dragging on the water, so the pattern of currents largely mirrors the pattern of global winds. The Coriolis effect deflects the moving water, and the shape of the continents forces the flow into closed loops within each ocean basin. Differences in water density caused by temperature and salinity drive the deeper circulation.
- 2
What is a gyre, and which way does one rotate in each hemisphere?
Model answer
A gyre is a large closed loop of surface currents that circulates around an ocean basin. In the Northern Hemisphere gyres rotate clockwise and in the Southern Hemisphere anticlockwise, because the Coriolis effect deflects moving water to the right of its path north of the equator and to the left south of it. Each gyre therefore carries warm water polewards along the western side of the ocean and cool water equatorwards along the eastern side.
- 3
What is a warm ocean current and how does it affect the climate of a coast it reaches?
Model answer
A warm current carries water that is warmer than the average for the latitude it is flowing into, usually moving polewards along the western side of an ocean basin. Air passing over it is warmed and moistened from below, which makes the air unstable and encourages uplift, so coasts washed by warm currents have mild winters, a small annual temperature range and reliable precipitation. Examples are the Gulf Stream and North Atlantic Drift, the Kuroshio off Japan, the Brazil Current and the East Australian Current.
- 4
What is a cold ocean current and how does it affect the climate of a coast it reaches?
Model answer
A cold current carries water that is colder than the average for the latitude, typically moving equatorwards along the eastern side of an ocean basin, where upwelling of cold water from depth often reinforces it, although cold currents also run equatorwards on western margins in the high latitudes. Air passing over it is chilled from below, which makes the lower air stable and suppresses uplift, so coasts washed by cold currents are cooler than their latitude suggests, very dry, and prone to persistent sea fog. Examples are the Labrador Current, the Canary Current, the Benguela Current, the Peru or Humboldt Current and the California Current.
- 5
How does the North Atlantic Drift affect the climate of the British Isles?
Model answer
It is the north-eastward continuation of the Gulf Stream and brings water from the Gulf of Mexico across the Atlantic to north-west Europe. The prevailing south-westerly winds blow across this warm water and arrive already warmed and moistened, so British and Irish winters are several degrees milder than the average for 50 to 60 degrees North, ports stay ice-free all year, frost is uncommon on western coasts and rainfall is reliable. Its influence is strongest in winter and weakest in summer, which is one reason the annual temperature range is so small in the west.
- 6
Two places lie at almost the same latitude, one on the Atlantic coast of Ireland and one on the coast of Labrador in Canada. Why is January so much colder in Labrador?
Model answer
Ireland is washed by the warm North Atlantic Drift and receives onshore south-westerly winds that have crossed that warm water, so January means stay around 5 to 7 degrees Celsius. Labrador is washed by the cold Labrador Current flowing south from the Arctic and receives offshore winds that have crossed the frozen interior of Canada, so January means fall well below freezing and the sea ices over. The contrast shows that ocean currents and wind direction can matter more than latitude.
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