AQA A-Level Geography 7037
Water and Carbon Cycles
Hot Desert Systems and LandscapesLandscape
Coastal Systems and LandscapesLandscape
Glacial Systems and LandscapesLandscape
HazardsHazards or ecosystems
Ecosystems Under StressHazards or ecosystems
Global Systems and Global Governance
Changing Places
Contemporary Urban EnvironmentsHuman option
Population and the EnvironmentHuman option
Resource SecurityHuman option
Population and the Environment
Tropical Wet and Semi-Arid Climates
- 3 things to know
- Component 2
Overview
Recall questions on the temperature, rainfall, global distribution, farming and population densities of tropical wet (Köppen Af) climates, and on the rainfall, temperatures, distribution, human activities and low population densities of semi-arid (Köppen BS) climates.
What you need to know
Answer each one before you reveal it.
What agricultural activities are practised in tropical wet climates?
Describe the temperature characteristics of semi-arid climates.
Questions from this subtopic
Each one with the model answer underneath.
- 1
What temperature characteristics define a tropical wet climate (Köppen Af)?
Model answer
High temperatures throughout the year, with every month averaging above 18°C.
- 2
Describe the precipitation characteristics of a tropical wet climate.
Model answer
High annual rainfall exceeding 2000mm with no dry season, and consistently high humidity.
- 3
Where are tropical wet climates distributed globally?
Model answer
Within approximately 10° of the equator, including the Amazon Basin, Congo Basin, and Southeast Asian archipelago.
- 4
What agricultural activities are practised in tropical wet climates?
Model answer
Shifting cultivation, plantation agriculture, and rice cultivation.
- 5
How do population densities vary within tropical wet climate regions?
Model answer
Population densities are sparse in rainforest interiors but dense in fertile river valleys.
- 6
What rainfall characteristics define a semi-arid climate (Köppen BS)?
Model answer
Low and unreliable rainfall of 250-500mm annually, with high evapotranspiration rates exceeding precipitation.
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