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The Carbon Cycle and Energy Security

Uncertainty, feedback loops and tipping points

  • 3 things to know
  • Papers 1 and 3

Overview

Recall questions on carbon sinks, peatland and permafrost feedbacks, forest dieback and thermohaline change.

What you need to know

Answer each one before you reveal it.

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Evaluation

Why does the variable role of carbon sinks create uncertainty in future climate warming projections?

Evaluation

How does the future mix of energy sources contribute to uncertainty in emissions projections?

Key term

How do rates of economic growth contribute to uncertainty in future emissions projections?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Why does the variable role of carbon sinks create uncertainty in future climate warming projections?

    Model answer

    Carbon sinks such as oceans and forests absorb varying amounts of atmospheric carbon depending on temperature, ecosystem health, and other conditions, making it difficult to predict how much emitted CO₂ will remain in the atmosphere.

  2. 2

    How do rates of economic growth contribute to uncertainty in future emissions projections?

    Model answer

    Higher economic growth typically increases energy demand and industrial activity, raising emissions, while slower growth reduces them; future growth rates are unpredictable, creating uncertainty.

  3. 3

    Why does population change make future climate projections uncertain?

    Model answer

    Population growth increases resource consumption and emissions, while population decline or stabilisation reduces them; future demographic trends are difficult to predict accurately.

  4. 4

    How does the future mix of energy sources contribute to uncertainty in emissions projections?

    Model answer

    The proportion of fossil fuels versus renewables in the global energy mix determines emission levels; future energy transitions depend on policy, technology, and investment decisions that are uncertain.

  5. 5

    Explain how carbon release from peatlands acts as a positive feedback mechanism.

    Model answer

    As peatlands warm and dry, organic matter decomposes aerobically, releasing stored carbon as CO₂; this adds to atmospheric greenhouse gases, causing further warming and more peatland degradation.

  6. 6

    How does thawing permafrost create a positive feedback loop that increases climate uncertainty?

    Model answer

    Warming thaws permafrost, releasing stored methane and CO₂; these greenhouse gases enhance warming, which thaws more permafrost, amplifying the original warming in a self-reinforcing cycle.

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