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Earth’s Life Support Systems

Stores, flows and physical controls in the tropical rainforest

  • 3 things to know
  • Component 01

Overview

Recall questions on the rainfall and temperature of the Amazon rainforest, its fast water cycle, interception and recycled rainfall, where its carbon is stored, rapid decomposition and latosols, and how temperature, rock permeability, relief and mineral composition control both cycles.

What you need to know

Answer each one before you reveal it.

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Key term

State the typical annual rainfall of the Amazon rainforest.

Key term

Describe the temperature regime of a tropical rainforest.

Key term

Why is the water cycle of a tropical rainforest described as fast?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    State the typical annual rainfall of the Amazon rainforest.

    Model answer

    Around 2,000 to 3,000 mm a year, averaging roughly 2,300 mm across the basin.

  2. 2

    Describe the temperature regime of a tropical rainforest.

    Model answer

    Mean monthly temperatures stay between about 26°C and 28°C all year, so the daily range is larger than the annual range.

  3. 3

    Why is the water cycle of a tropical rainforest described as fast?

    Model answer

    High temperatures, heavy rainfall and dense vegetation drive rapid interception, evapotranspiration and runoff, so water passes through the system in days rather than years.

  4. 4

    What share of rainforest precipitation is returned to the atmosphere by evapotranspiration?

    Model answer

    Roughly half of it, and much of this recycled moisture falls again as rain further inland.

  5. 5

    How much rainfall is intercepted by the rainforest canopy?

    Model answer

    Typically between 10% and 25%, much of which evaporates directly from the leaf surfaces without ever reaching the ground.

  6. 6

    How does a single emergent tree influence the water cycle around it?

    Model answer

    Its canopy intercepts rain and evaporates part of it, its roots draw soil moisture from depth, and it transpires several hundred litres of water back to the atmosphere on a hot day.

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AThe lower quartile is the 2nd value, 11 cm.
BThe upper quartile is the 6th value, 16 cm.
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