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Dryland Landscapes

Relief, aspect and desert microclimates

  • 3 things to know
  • Component 01

Overview

Recall questions on desert microclimates, how aspect and slope angle change temperature, moisture, vegetation, weathering and runoff, orographic rain on the Tibesti Mountains, albedo, the large daily temperature range and the world's highest recorded temperature, canyon microclimates, and dew.

What you need to know

Answer each one before you reveal it.

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Key term

How does aspect affect slope conditions in a northern hemisphere desert?

Key term

Why is vegetation often denser on a pole-facing desert slope?

Process

How does aspect alter the weathering processes operating on a desert slope?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Define the term microclimate.

    Model answer

    A microclimate is the climate of a very small area close to the ground, which can differ markedly from the general climate of the wider region.

  2. 2

    How does aspect affect slope conditions in a northern hemisphere desert?

    Model answer

    South-facing slopes receive far more direct sunlight and become hotter and drier, while north-facing slopes are shaded, stay cooler and hold their moisture for longer; the pattern is reversed south of the Equator.

  3. 3

    Why is vegetation often denser on a pole-facing desert slope?

    Model answer

    Lower insolation means less evaporation, so soil moisture survives for longer and plants can establish where the opposite, sunlit slope stays bare.

  4. 4

    How does aspect alter the weathering processes operating on a desert slope?

    Model answer

    Sunlit slopes experience greater thermal stress and more salt crystallisation as moisture evaporates, whereas shaded, moister slopes see more chemical weathering and, in cold deserts, more freeze–thaw.

  5. 5

    How does slope angle influence runoff and infiltration in a dryland?

    Model answer

    Steep slopes shed water rapidly as overland flow with little time for it to soak in, so both moisture and sediment become concentrated at the foot of the slope.

  6. 6

    Why are upland areas within a desert often wetter than the plains around them?

    Model answer

    Air forced to rise over high ground cools and condenses, giving orographic rainfall, so massifs receive noticeably more precipitation than the lowlands surrounding them.

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