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CUET-PG Climate System Science: practice questions

CUET-PG — Environmental Sciences · India · National Testing Agency

Original practice questions written to the published syllabus · not past papers
10worked here, free
43written to this exam in this subject
13syllabus units

What this subject covers

The physical basis of climate change as assessed by the IPCC: the greenhouse effect, radiative forcing, the global carbon cycle, feedbacks, climate sensitivity, and the evidence for observed change. It goes well beyond the 'climate change and livestock' unit of veterinary environmental hygiene.

In the exams: GATE ES Section 8 (greenhouse gases, global warming); UGC NET Environmental Sciences Unit 10; GARP SCR 'Foundations of Climate Change'; UPSC CSE environment

What CUET-PG asks from it

UGC NET Environmental Sciences (Unit 10) and CUET-PG Environmental Sciences

Recall of IPCC structure and findings, GWP values by assessment report, residence times, ocean acidification chemistry, sea level contributions, Milankovitch cycles and the components of the climate system, usually as assertion–reason and matching items.

Where the 43 questions fall

How our questions for CUET-PG spread across the units of Climate System Science. Difficulty: 22 easy, 20 medium, 1 hard.

Observed changes: temperature, precipitation, sea level, cryosphere6
The global carbon cycle: pools, fluxes and the airborne fraction5
IPCC assessment process and confidence language5
Radiative forcing and global warming potential (GWP, GTP, GWP*)4
Ocean warming, deoxygenation and acidification4
The climate system and its components3
Methane and nitrous oxide budgets3
Carbon budgets and the link between cumulative emissions and warming3
The natural greenhouse effect and the energy budget2
Aerosols and their climate effects2
Climate feedbacks and equilibrium climate sensitivity2
Detection and attribution, including extreme-event attribution2
Tipping points and irreversibility2

10 practice questions, worked

Choose an answer, then open the working. Each explanation says why the right answer is right and why the others are not.

1 · The climate system and its components · medium

Why does orbital (Milankovitch) forcing trigger large glacial–interglacial changes even though it changes the annual global mean sunlight only slightly?

  1. It alters the rotation rate of the Earth, lengthening the night and so cooling the high latitudes for millennia
  2. It redistributes sunlight by season and latitude, and ice-albedo and carbon dioxide feedbacks amplify the response
  3. It shifts the Earth's orbit so far from the Sun in some epochs that the effective temperature drops below freezing
  4. It changes the total solar irradiance by tens of W m⁻², which directly cools or warms the planet by several kelvin
Answer and working

B. It redistributes sunlight by season and latitude, and ice-albedo and carbon dioxide feedbacks amplify the response

Orbital changes mostly redistribute insolation between seasons and latitudes, especially northern summer sunlight that decides whether snow survives. Ice-sheet albedo and CO2 feedbacks then amplify the change. Orbital variation does not change total irradiance by tens of W m⁻², does not move the Earth beyond habitable distance, and does not alter rotation rate in this way.

Further reading: IPCC AR6 WGI (2021) and the IPCC 2006 Guidelines / 2019 Refinement where cited

2 · The global carbon cycle: pools, fluxes and the airborne fraction · medium

For 2010–2019, take fossil CO₂ emissions as 9.6 PgC yr⁻¹, land-use change emissions as 1.6 PgC yr⁻¹ and atmospheric growth as 5.1 PgC yr⁻¹. What is the airborne fraction?

  1. 0.46
  2. 0.53
  3. 0.54
  4. 0.22
Answer and working

A. 0.46

Airborne fraction = growth ÷ total emissions = 5.1 ÷ (9.6 + 1.6) = 0.46. 0.53 leaves out land-use emissions; 0.54 is the fraction taken by sinks; 0.22 is the ocean sink's share.

Further reading: IPCC AR6 WGI (2021) and the IPCC 2006 Guidelines / 2019 Refinement where cited

3 · The global carbon cycle: pools, fluxes and the airborne fraction · medium

Atmospheric CO₂ rises by 2.4 ppm in a year. Taking 1 ppm = 2.124 PgC, what mass of carbon dioxide (not carbon) does this represent?

  1. 18.7 Gt CO₂
  2. 1.4 Gt CO₂
  3. 5.1 Gt CO₂
  4. 8.8 Gt CO₂
Answer and working

A. 18.7 Gt CO₂

Carbon = 2.4 × 2.124 = 5.10 PgC; CO2 = 5.10 × 44/12 = 18.7 Gt CO2. 5.1 is the carbon mass mislabelled; 8.8 drops the ppm factor; 1.4 divides by 44/12 instead of multiplying.

Further reading: IPCC AR6 WGI (2021) and the IPCC 2006 Guidelines / 2019 Refinement where cited

4 · The global carbon cycle: pools, fluxes and the airborne fraction · easy

Which reservoir is the largest pool of carbon that exchanges with the atmosphere on time scales of up to a few thousand years?

  1. The ocean, mostly as dissolved inorganic carbon
  2. Soils, mostly as organic matter in the topsoil
  3. Land vegetation, mostly as wood in tropical forests
  4. The atmosphere, mostly as carbon dioxide gas
Answer and working

A. The ocean, mostly as dissolved inorganic carbon

The ocean holds about 38,000 PgC, overwhelmingly as dissolved inorganic carbon, far more than the atmosphere (~870 PgC), vegetation (~450–650 PgC) or soils (~1500–2400 PgC).

Further reading: IPCC AR6 WGI (2021) and the IPCC 2006 Guidelines / 2019 Refinement where cited

5 · The global carbon cycle: pools, fluxes and the airborne fraction · medium

Which evidence shows that the rise in atmospheric CO₂ since industrialisation comes mainly from fossil carbon?

  1. Higher CO₂ in the Southern Hemisphere than in the industrial Northern Hemisphere
  2. A rising ¹³C/¹²C ratio in atmospheric CO₂ together with rising ocean pH values
  3. A rising ¹⁴C content of atmospheric CO₂ together with rising atmospheric oxygen
  4. A falling ¹³C/¹²C ratio in atmospheric CO₂ together with falling atmospheric oxygen
Answer and working

D. A falling ¹³C/¹²C ratio in atmospheric CO₂ together with falling atmospheric oxygen

Fossil carbon is depleted in ¹³C and free of ¹⁴C, so its addition lowers ¹³C/¹²C (the Suess effect), and combustion consumes oxygen. Ocean pH is falling, not rising, and CO2 is higher in the Northern Hemisphere where most emissions occur.

Further reading: IPCC AR6 WGI (2021) and the IPCC 2006 Guidelines / 2019 Refinement where cited

6 · Climate feedbacks and equilibrium climate sensitivity · medium

Why is the water vapour feedback positive?

  1. Higher humidity makes the air heavier, so it sinks and compresses, warming the lower atmosphere
  2. Warmer oceans release dissolved carbon dioxide, which raises the greenhouse effect of the air
  3. Warming increases cloud cover everywhere, and clouds always trap more heat than they reflect
  4. Saturation vapour pressure rises about 7 per cent per kelvin and relative humidity stays near constant
Answer and working

D. Saturation vapour pressure rises about 7 per cent per kelvin and relative humidity stays near constant

By Clausius–Clapeyron the air's capacity for water vapour rises about 7% per kelvin; with near-constant relative humidity the amount of this strong greenhouse gas rises with warming. Cloud feedback is a separate term with mixed signs; ocean CO2 release is a carbon-cycle feedback; humid air is lighter, not heavier.

Further reading: IPCC AR6 WGI (2021) and the IPCC 2006 Guidelines / 2019 Refinement where cited

7 · Observed changes: temperature, precipitation, sea level, cryosphere · easy

Global mean sea level rose at 3.7 mm yr⁻¹ over 2006–2018. If that rate held for 30 years, how much would sea level rise?

  1. 0.11 m
  2. 1.11 m
  3. 0.0037 m
  4. 0.37 m
Answer and working

A. 0.11 m

3.7 mm yr⁻¹ × 30 yr = 111 mm = 0.11 m. 1.11 m is a factor-of-ten slip (dividing mm by 100 instead of 1000); 0.0037 m is a single year; 0.37 m is a full century at that rate. Actual rise is accelerating, so a constant rate underestimates.

Further reading: IPCC AR6 WGI (2021) and the IPCC 2006 Guidelines / 2019 Refinement where cited

8 · Ocean warming, deoxygenation and acidification · easy

About what share of the extra energy accumulated in the climate system has gone into the ocean, according to AR6?

  1. 5 per cent
  2. 25 per cent
  3. 50 per cent
  4. 91 per cent
Answer and working

D. 91 per cent

AR6: about 91% to the ocean, 5% to land, 3% to ice and 1% to the atmosphere. 25% is close to the ocean's share of CO2 emissions, a different quantity.

Further reading: IPCC AR6 WGI (2021) and the IPCC 2006 Guidelines / 2019 Refinement where cited

9 · Ocean warming, deoxygenation and acidification · medium

Marine heatwaves are periods of extreme high sea surface temperature. What did AR6 report about their frequency?

  1. They have become less frequent since the 1980s
  2. They are confined to the Arctic Ocean since the 1980s
  3. They occur only during El Niño years and show no trend
  4. They have roughly doubled in frequency since the 1980s
Answer and working

D. They have roughly doubled in frequency since the 1980s

AR6 assessed with high confidence that marine heatwaves have approximately doubled in frequency since the 1980s, with human influence very likely contributing to most since 2006. They occur in all ocean basins and in non-El Niño years.

Further reading: IPCC AR6 WGI (2021) and the IPCC 2006 Guidelines / 2019 Refinement where cited

10 · IPCC assessment process and confidence language · medium

Which publication sequence matches the IPCC Sixth Assessment cycle?

  1. WGI 2014; WGII 2014; WGIII 2014; Synthesis Report 2015
  2. WGI 2018; WGII and WGIII 2019; Synthesis Report 2020
  3. WGI 2023; WGII and WGIII 2024; Synthesis Report 2025
  4. WGI 2021; WGII and WGIII 2022; Synthesis Report 2023
Answer and working

D. WGI 2021; WGII and WGIII 2022; Synthesis Report 2023

AR6: WGI August 2021, WGII February 2022, WGIII April 2022, Synthesis Report March 2023. 2014 belongs to AR5; 2018–2019 was the period of the AR6 special reports.

Further reading: IPCC AR6 WGI (2021) and the IPCC 2006 Guidelines / 2019 Refinement where cited

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Read the subject

Climate System ScienceThe full study manual, free CUET-PGFormat, sections and how it has changed

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