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Practice questionsIB Environmental Systems and SocietiesAtmosphere and climate change
IB Environmental Systems and Societies

Atmosphere and climate change practice questions.

58 exam-style questions on Atmosphere and climate change with answers and explanations. Six real samples below — the full set is free with an account.

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Sample questions

Which set of values best describes the composition of dry air in the troposphere by volume?

  • nitrogen 21 %, oxygen 78 %, argon 0.93 %, carbon dioxide about 0.04 %
  • nitrogen 78 %, oxygen 21 %, argon 0.93 %, carbon dioxide about 0.04 %
  • nitrogen 78 %, oxygen 21 %, carbon dioxide 0.93 %, argon about 0.04 %
  • nitrogen 65 %, oxygen 21 %, water vapour 13 %, carbon dioxide about 0.9 %

Answer: nitrogen 78 %, oxygen 21 %, argon 0.93 %, carbon dioxide about 0.04 %

Dry air is overwhelmingly nitrogen and oxygen, argon is the third most abundant gas, and carbon dioxide is a trace gas despite its climatic importance. Water vapour is excluded from these figures because it varies from almost nothing to about 4 % of the air.

In one layer of the atmosphere the temperature rises with increasing altitude because ozone there absorbs ultraviolet radiation. That layer is

  • the troposphere, 0-12 km
  • the mesosphere, 50-85 km
  • the stratosphere, 12-50 km
  • the thermosphere, above 85 km

Answer: the stratosphere, 12-50 km

Absorption of UV by ozone creates a temperature inversion in the stratosphere, which makes the layer very stable and is why substances that reach it, such as CFCs, remain there for decades. The troposphere below is heated from the surface, so its temperature falls with height.

Sea ice with an albedo of about 0.6 melts and is replaced by open ocean with an albedo of about 0.06. The consequence for the local radiation budget is that

  • more shortwave radiation is reflected, so the surface cools further
  • less longwave radiation is emitted, so the surface temperature stabilises
  • more shortwave radiation is absorbed, so the warming is reinforced
  • less shortwave radiation reaches the surface, so warming slows down

Answer: more shortwave radiation is absorbed, so the warming is reinforced

Dark water absorbs almost all of the shortwave radiation that bright ice previously reflected, so melting drives further melting. That is a positive feedback, and positive here means amplifying, not beneficial.

Greenhouse gases raise the mean surface temperature of the Earth because they

  • reflect incoming shortwave solar radiation back towards the surface
  • absorb the ultraviolet radiation that would otherwise be lost to space
  • reduce the planetary albedo by darkening the upper atmosphere
  • let shortwave radiation in but absorb outgoing longwave radiation

Answer: let shortwave radiation in but absorb outgoing longwave radiation

The selective absorption is the whole mechanism: solar radiation passes through, the warmed surface re-emits at longer wavelengths, and those wavelengths are absorbed and re-radiated in all directions, including downwards. Reflecting incoming radiation would cool the surface, not warm it.

Sulphate aerosols released alongside carbon dioxide when coal is burned reflect incoming sunlight. A country fits flue-gas desulphurisation to its power stations while continuing to burn the same quantity of coal. The most likely short-term effect on regional temperature is

  • a rise, because a cooling influence has been removed
  • a fall, because the filters also cut carbon dioxide output
  • no change, because the aerosols and the carbon dioxide cancel out
  • a fall, because cleaner air lets more longwave radiation escape

Answer: a rise, because a cooling influence has been removed

Sulphate aerosols scatter incoming shortwave radiation and have masked part of the warming caused by greenhouse gases, so removing them unmasks that warming. Desulphurisation removes sulphur compounds and not carbon dioxide, so the greenhouse forcing itself is unchanged.

Tonne for tonne, methane released today warms the climate far more over the next twenty years than carbon dioxide does, yet carbon dioxide is treated as the greater long-term problem because

  • methane absorbs only shortwave radiation coming from the Sun
  • methane has a much shorter residence time in the atmosphere
  • carbon dioxide is released from far fewer separate sources
  • carbon dioxide is removed from the atmosphere within a few years

Answer: methane has a much shorter residence time in the atmosphere

Methane is oxidised over roughly a decade, whereas a large share of any carbon dioxide pulse stays in the atmosphere and ocean for centuries, so its warming accumulates. Global warming potential therefore depends on the time horizon chosen, not on the gas alone.

58 Atmosphere and climate change questions — free with an account. Spaced repetition, streaks and full exam simulations included.

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