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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.

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Key term

Which regions can experience intensified drought during the La Niña phase of ENSO?

Key term

What is the definition of meteorological drought?

Key term

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. 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. 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. 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. 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. 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. 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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