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Future of Food

Desertification and the drylands of the Sahel

  • 2 things to know
  • Component 03

Overview

Recall questions on desertification and why it is not an advancing desert, its human and climatic causes, overgrazing and albedo feedback, effects on dryland ecosystems, the Sahel's location, rainfall, ITCZ, vegetation, millet and sorghum, hydrology and shrinking Lake Chad, population growth, land acquisition, climate change, and farmer managed natural regeneration.

What you need to know

Answer each one before you reveal it.

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Key term

Explain the albedo feedback that can reinforce desertification.

Key term

Describe the surface hydrology of the Sahel.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Define desertification.

    Model answer

    Desertification is the degradation of land in arid, semi-arid and dry sub-humid areas, brought about by a combination of climatic variation and human activity.

  2. 2

    Explain why desertification does not mean the physical advance of a desert.

    Model answer

    It is a loss of productivity within existing drylands, appearing as patches of degraded land that spread and merge rather than as a desert edge marching forward.

  3. 3

    Give three human causes of desertification.

    Model answer

    Overgrazing by too many livestock, overcultivation without fallow or fertiliser, and the removal of trees and shrubs for fuelwood.

  4. 4

    Explain how overgrazing leads to soil erosion.

    Model answer

    Animals strip away the vegetation cover while their hooves compact and break the surface, so bare loose soil is left exposed to wind and to runoff from intense rain.

  5. 5

    Give two climatic causes of desertification.

    Model answer

    A run of years with below-average rainfall, and rising temperatures that increase evapotranspiration and dry the soil.

  6. 6

    Explain the albedo feedback that can reinforce desertification.

    Model answer

    Loss of dark vegetation raises the surface albedo, so more radiation is reflected, the air above is heated less, convection and rainfall weaken, and the drying intensifies.

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