Edexcel A-Level Geography 9GE0
Tectonic Processes and Hazards
Glaciated Landscapes and ChangeLandscape
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Globalisation
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The Water Cycle and Water Insecurity
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The Water Cycle and Water Insecurity
Meteorological and hydrological drought, ENSO and human causes
- 3 things to know
- Papers 1 and 3
Overview
Meteorological and hydrological drought and why one lags the other, short and longer-term precipitation deficits, ENSO and the regions affected in its El Niño and La Niña phases, and human causes such as over-abstraction, with the Sahel and the Murray-Darling Basin as examples.
What you need to know
Answer each one before you reveal it.
What is the definition of meteorological drought?
What are the immediate effects of a short-term precipitation deficit on the hydrological cycle?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What is the definition of meteorological drought?
Model answer
A period of below-average precipitation relative to the long-term mean for a region.
- 2
How is hydrological drought defined?
Model answer
It occurs when water availability in rivers, reservoirs, and aquifers falls below normal levels, often lagging behind meteorological drought.
- 3
Why does hydrological drought typically lag behind meteorological drought?
Model answer
Because it takes time for reduced precipitation to translate into lower water levels in rivers, reservoirs, and aquifers.
- 4
What are the immediate effects of a short-term precipitation deficit on the hydrological cycle?
Model answer
Immediate soil moisture reduction and decreased surface water availability.
- 5
How can longer-term precipitation trends establish persistent drought conditions?
Model answer
Through cumulative water budget deficits that accumulate over months or years.
- 6
What is ENSO?
Model answer
El Niño-Southern Oscillation — periodic variations in sea surface temperatures and atmospheric pressure across the equatorial Pacific Ocean.
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