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Earth’s Life Support Systems

Stores, flows and seasonal change in the Arctic tundra

  • 3 things to know
  • Component 01

Overview

Recall questions on the precipitation and temperatures of the Arctic tundra, permafrost and the active layer, its slow water cycle, the permafrost carbon store and tundra vegetation, the short growing season, spring melt and seasonal carbon exchange, and the effects of bedrock, relief and albedo.

What you need to know

Answer each one before you reveal it.

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Key term

Describe the precipitation regime of the Arctic tundra.

Key term

State the typical summer and winter temperatures of the Arctic tundra.

Key term

What is permafrost, which underlies the Arctic tundra?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Describe the precipitation regime of the Arctic tundra.

    Model answer

    Totals are very low, usually under 250 mm a year and mostly falling as snow, which makes the tundra a cold desert.

  2. 2

    State the typical summer and winter temperatures of the Arctic tundra.

    Model answer

    Winter means fall to about −20°C to −30°C, and even the warmest month averages below 10°C.

  3. 3

    What is permafrost?

    Model answer

    Permafrost is ground that remains at or below 0°C for at least two consecutive years.

  4. 4

    What is the active layer?

    Model answer

    The active layer is the shallow surface layer above the permafrost that thaws each summer and refreezes in winter, typically between 0.3 and 1 m deep.

  5. 5

    Why are tundra soils waterlogged in summer despite the low rainfall?

    Model answer

    The permafrost beneath is impermeable so meltwater cannot percolate away, and low temperatures mean very little of it evaporates.

  6. 6

    Why is the tundra water cycle described as slow?

    Model answer

    For most of the year water is locked up as ground ice and snow so flows almost cease, and only during the brief summer does liquid water move through the system at all.

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