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
Water and Carbon Cycles
Deficit in the water cycle and aquifer recharge
- 2 things to know
- Component 2
Overview
Water deficit, meteorological and hydrological drought and agricultural drought.
What you need to know
Answer each one before you reveal it.
Distinguish between meteorological and hydrological drought.
Questions from this subtopic
Each one with the model answer underneath.
- 1
Define a water deficit.
Model answer
A water deficit occurs when outputs and demand exceed the water available in a system. Soil moisture, river flows and groundwater levels all fall.
- 2
Distinguish between meteorological and hydrological drought.
Model answer
Meteorological drought is a sustained shortfall of precipitation below the long-term average. Hydrological drought is the resulting shortfall in river flow, reservoir level and groundwater.
- 3
What is agricultural drought?
Model answer
Agricultural drought is a shortage of soil moisture during the growing season. Crops suffer even where total annual rainfall appears close to normal.
- 4
How does seasonal variation produce a water deficit?
Model answer
Climates with a marked dry season deliver almost no rain for several months. Evapotranspiration continues throughout, so stores run down until the rains return.
- 5
Give an example of a region with a strongly seasonal deficit.
Model answer
The Sahel receives its rain in a short summer season and is dry for the rest of the year. Failure of that single wet season causes severe drought.
- 6
How can longer-term climate change deepen a deficit?
Model answer
Rising temperatures raise potential evapotranspiration even where rainfall is unchanged. Shifts in circulation can also reduce rainfall totals in already dry regions.
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