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Climate Change

The enhanced greenhouse effect and the global energy balance

  • 2 things to know
  • Component 03

Overview

Recall questions on the enhanced greenhouse effect, radiative forcing since 1750 and the share from CO₂, climate sensitivity, incoming and reflected solar radiation, Earth's energy imbalance, aerosols masking warming and the effect of cleaning the air, land use change and albedo, black carbon, and the urban heat island.

What you need to know

Answer each one before you reveal it.

Your recallNot started
Key term

Why can cleaning up air pollution briefly accelerate warming?

Key term

Which single gas is responsible for the largest share of human radiative forcing?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Define the enhanced greenhouse effect.

    Model answer

    It is the additional warming that occurs when human emissions raise greenhouse gas concentrations above their natural levels, so that more longwave radiation is trapped than the natural effect alone would trap.

  2. 2

    What is radiative forcing?

    Model answer

    It is the change in the balance between incoming and outgoing energy at the top of the atmosphere caused by a factor such as added CO₂, measured in watts per square metre.

  3. 3

    Give the approximate total radiative forcing caused by human activity since 1750.

    Model answer

    It is roughly 2.7 W m⁻².

  4. 4

    Which single gas is responsible for the largest share of human radiative forcing?

    Model answer

    Carbon dioxide is responsible for the largest share.

  5. 5

    Explain what climate sensitivity means.

    Model answer

    It is the amount of global warming expected once the climate system has fully adjusted to a doubling of atmospheric CO₂.

  6. 6

    State the best estimate of equilibrium climate sensitivity.

    Model answer

    The best estimate is about 3 °C of warming for a doubling of CO₂.

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