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Dryland Landscapes

Dryland landscape systems: inputs, stores, flows and outputs

  • 3 things to know
  • Component 01

Overview

Recall questions on the dryland as an open system: its energy and material inputs, outputs and sediment stores, why its water store is small, geomorphic processes, positive and negative feedback, dynamic equilibrium, and why drylands respond so quickly to change.

What you need to know

Answer each one before you reveal it.

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Key term

Name three energy inputs into a dryland landscape system.

Key term

Identify three material inputs to a dryland landscape system.

Key term

What are the main outputs from a dryland landscape system?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What is meant by describing a dryland as an open system?

    Model answer

    It is an area of the Earth's surface that exchanges both energy and matter with its surroundings, so material and energy can cross its boundaries.

  2. 2

    Name three energy inputs into a dryland landscape system.

    Model answer

    The main energy inputs are solar radiation, the kinetic energy of the wind, and the potential energy held by sediment resting on slopes.

  3. 3

    Identify three material inputs to a dryland landscape system.

    Model answer

    Material inputs include precipitation, weathered bedrock and regolith produced in place, and sediment blown or washed in from outside the area.

  4. 4

    What are the main outputs from a dryland landscape system?

    Model answer

    The main outputs are water lost by evaporation and transpiration, dust exported by the wind, and sediment carried away by ephemeral or exotic rivers.

  5. 5

    Give four sediment stores found in a desert landscape.

    Model answer

    Dune fields, alluvial fans, playa deposits and the regolith mantling hillslopes are all sediment stores.

  6. 6

    Why is the water store in a dryland system usually very small?

    Model answer

    Precipitation is low and infrequent while potential evaporation is extremely high, so most water leaves the system almost at once and little is retained in soil or channels.

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AThe lower quartile is the 2nd value, 11 cm.
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