Eduqas A-Level Geography A110QS
Coastal LandscapesLandscape
Glaciated LandscapesLandscape
Changing Places
Water and Carbon Cycles
Global Migration
Global Governance of the Oceans
Tectonic Hazards
EcosystemsContemporary theme
Economic Growth and Challenge: IndiaContemporary theme
Economic Growth and Challenge: ChinaContemporary theme
Development in an African ContextContemporary theme
Energy Challenges and DilemmasContemporary theme
Weather and ClimateContemporary theme
Geographical Skills
Weather and Climate
ENSO and short-term climate change
- 3 things to know
- Component 3 Section B
Overview
Consequences of El Niño for South America, consequences of El Niño for Australia and Indonesia and la Niña.
What you need to know
Answer each one before you reveal it.
Describe normal, or Walker circulation, conditions in the Pacific.
What happens to the trade winds during an El Niño event?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What does ENSO stand for?
Model answer
ENSO stands for the El Niño Southern Oscillation. The term covers both the oceanic and the atmospheric parts of the cycle.
- 2
Describe normal, or Walker circulation, conditions in the Pacific.
Model answer
Trade winds push warm surface water westwards, piling it up around Indonesia. Cold water upwells off South America, so the western Pacific is wet and the eastern Pacific dry.
- 3
What happens to the trade winds during an El Niño event?
Model answer
The trade winds weaken or reverse. Warm water flows back eastwards across the Pacific.
- 4
What are the consequences of El Niño for South America?
Model answer
Warm water off Peru and Ecuador suppresses upwelling and brings heavy rainfall and flooding. The anchovy fishery collapses because the nutrient supply is cut off.
- 5
What are the consequences of El Niño for Australia and Indonesia?
Model answer
Drier than normal conditions bring drought and an elevated wildfire risk. Crop yields fall across eastern Australia.
- 6
What is La Niña?
Model answer
La Niña is the opposite phase of the cycle, with unusually strong trade winds. Cold upwelling off South America intensifies and the western Pacific becomes wetter still.
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