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CFA Institute Sustainable Investing Certificate Climate System Science: practice questions

CFA Institute Sustainable Investing Certificate (formerly Certificate in ESG Investing) · International · CFA Institute

Original practice questions written to the published syllabus · not past papers
10worked here, free
18written to this exam in this subject
11syllabus units

About CFA Institute Sustainable Investing Certificate

CFA Institute Sustainable Investing Certificate (formerly Certificate in ESG Investing) is a professional certification run by CFA Institute, for candidates worldwide. Self-study with a 6-month access period and one exam taken in person or online; about 100+ hours of study recommended. Question count and duration were not on the page read.

Source: cfainstitute.org.

Checked against the exam body's published information. Formats and fees change; confirm the current edition there before you book.

Climate System Science in CFA Institute Sustainable Investing Certificate

Conceptual understanding of greenhouse gases, CO2-equivalence, carbon budgets and net zero, physical risk drivers such as sea level rise and extremes, and correct citation of IPCC confidence language.

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.

Our 18 CFA Institute Sustainable Investing Certificate questions in this subject: 1 easy, 14 medium, 3 hard, across 11 units.

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.

These 10 were written to CFA Institute Sustainable Investing Certificate and are not shown on any other exam's page.

Question 1 · medium

AR6 assessed the Earth's energy imbalance for 2006–2018. Which statement correctly describes it and where the extra energy has gone?

  1. About 0.8 W m⁻², with roughly 60 per cent going into melting ice and the rest into the ocean
  2. About 8 W m⁻², with roughly 91 per cent of the accumulated energy going into the atmosphere
  3. About 2.7 W m⁻², equal to the total human forcing, with most going into warming the land
  4. About 0.8 W m⁻², with roughly 91 per cent of the accumulated energy going into the ocean
Answer and working

D. About 0.8 W m⁻², with roughly 91 per cent of the accumulated energy going into the ocean

AR6 gives 0.79 W m⁻² for 2006–2018, with ~91% of the energy in the ocean, ~5% land, ~3% ice and ~1% atmosphere. The imbalance is smaller than the forcing (2.72 W m⁻²) because the climate has already warmed and radiates part of the forcing away.

Question 2 · medium

Why does stopping sulphur dioxide emissions produce a near-term warming, while stopping CO₂ emissions does not cause a rapid drop in temperature?

  1. Clean-air rules increase black carbon from replacement fuels, which more than offsets any benefit
  2. Sulphate aerosol washes out in days, removing its cooling at once, while CO₂ persists for centuries
  3. Carbon dioxide is removed within a year, so its warming vanishes even faster than aerosol cooling
  4. Sulphur dioxide is itself a strong greenhouse gas whose removal frees space for water vapour to absorb
Answer and working

B. Sulphate aerosol washes out in days, removing its cooling at once, while CO₂ persists for centuries

Tropospheric sulphate has a lifetime of days to weeks, so its cooling disappears almost immediately; CO2 warming depends on cumulative emissions and persists. SO2 is not a significant greenhouse gas, clean-air rules do not inherently raise black carbon, and CO2 is not removed within a year.

Question 3 · medium

Which statement about observed extremes matches the AR6 assessment?

  1. Tornado frequency has been shown with high confidence to have risen worldwide since the 1950s
  2. Heavy precipitation has grown more frequent and intense since the 1950s over most well-observed land
  3. Cold extremes have become more frequent across most land regions since the 1950s
  4. Global tropical cyclone numbers have been shown with high confidence to have doubled since 1900
Answer and working

B. Heavy precipitation has grown more frequent and intense since the 1950s over most well-observed land

AR6 found with high confidence that heavy precipitation increased in frequency and intensity since the 1950s over most land with good observations, and that hot extremes increased while cold extremes decreased. Evidence for trends in tornadoes and in global cyclone numbers is low-confidence, and cold extremes have declined.

Question 4 · medium

An analysis finds that a heatwave of a given intensity has a 1-in-20 chance per year in today's climate and a 1-in-100 chance in a counterfactual climate without human influence. What are the probability ratio (PR) and fraction of attributable risk (FAR)?

  1. PR = 5; FAR = 0.2
  2. PR = 5; FAR = 0.8
  3. PR = 80; FAR = 0.05
  4. PR = 0.2; FAR = 0.2
Answer and working

B. PR = 5; FAR = 0.8

P1 = 0.05, P0 = 0.01. PR = P1/P0 = 5. FAR = 1 − P0/P1 = 1 − 0.2 = 0.8: 80% of the present risk is attributable to human influence. Inverting the ratio gives 0.2, and FAR is not P0/P1 (0.2).

Question 5 · hard

A newspaper reports that climate change made a recent flood-producing rainfall event 'five times more likely'. Which interpretation is correct?

  1. The rainfall was five times heavier than it would have been without human warming, measured in millimetres
  2. Such floods will now occur every year, five times more often than the single event that has just been studied
  3. Events at least that extreme are now five times as probable as in a counterfactual climate without human warming
  4. The flood was caused entirely by climate change and would not have happened at all in a pre-industrial climate
Answer and working

C. Events at least that extreme are now five times as probable as in a counterfactual climate without human warming

A probability ratio of 5 compares the likelihood of the event class in today's and a counterfactual climate. It does not mean the event could not occur naturally, does not describe a fivefold intensity change (intensity is a separate metric), and does not predict annual recurrence.

Question 6 · medium

Why does stopping CO₂-driven warming require net zero CO₂ emissions rather than merely reducing emissions?

  1. The ocean releases stored heat whenever emissions fall, so cuts raise temperature
  2. CO₂ is removed within a decade, so emissions must stop before sinks can act
  3. Warming tracks the annual emission rate, so it stops once emissions fall by half
  4. Warming tracks cumulative CO₂, so any positive net emission keeps adding to it
Answer and working

D. Warming tracks cumulative CO₂, so any positive net emission keeps adding to it

Because warming is near-linear in cumulative emissions, temperature keeps rising as long as net emissions are positive; it stabilises only at net zero (with ZEC close to zero). Halving the rate slows the rise but does not stop it.

Question 7 · hard

Two companies each plan to emit 1 MtCO₂ more over the next decade. Company A says this is acceptable because it will buy credits from a methane-capture project. Why is this not climate-equivalent in the long run under the cumulative-emissions framework?

  1. Methane has a GWP100 below one, so each tonne avoided is worth less than a tonne of carbon dioxide
  2. Avoided methane cuts a short-lived forcing, but the CO₂ adds to the cumulative total setting long-term warming
  3. The cumulative-emissions framework applies only to methane, so carbon dioxide emissions are ignored
  4. Methane capture projects always fail, so any credits bought from them have no climate value whatever
Answer and working

B. Avoided methane cuts a short-lived forcing, but the CO₂ adds to the cumulative total setting long-term warming

TCRE links warming to cumulative CO2; methane reductions lower near-term forcing but do not offset the permanent addition from CO2. This is why many standards treat CO2 and short-lived gases separately. Methane projects can deliver value, methane's GWP100 is about 27–30, and the framework is about CO2.

Question 8 · medium

For a risk manager, what is the most defensible way to treat climate tipping points given current science?

  1. As purely speculative ideas with no physical basis, which can be safely ignored in planning
  2. As events that only matter after 2300, beyond any business or policy planning horizon
  3. As events at precisely known thresholds, such as exactly 1.5 °C for every tipping element
  4. As tail risks whose likelihood rises with each increment of warming, with uncertain thresholds
Answer and working

D. As tail risks whose likelihood rises with each increment of warming, with uncertain thresholds

Threshold estimates differ between studies, so tipping points are best treated as low-likelihood, high-impact risks that become more probable with more warming. They have physical basis, are not at precisely known thresholds, and some (such as warm-water coral loss) are relevant this century.

Question 9 · medium

According to the IPCC Special Report on Global Warming of 1.5 °C, how much further would warm-water coral reefs decline at 1.5 °C and at 2 °C of global warming?

  1. No further decline at 1.5 °C and 50 per cent at 2 °C
  2. 70–90 per cent at 1.5 °C and more than 99 per cent at 2 °C
  3. 10–20 per cent at 1.5 °C and 30–40 per cent at 2 °C
  4. More than 99 per cent at 1.5 °C and recovery at 2 °C
Answer and working

B. 70–90 per cent at 1.5 °C and more than 99 per cent at 2 °C

SR1.5 projected a further decline of 70–90% at 1.5 °C (high confidence) and more than 99% at 2 °C (very high confidence). The smaller declines understate the projection, and higher warming cannot produce recovery.

Question 10 · medium

A coastal resort's planners ask whether a solar-radiation-modification programme would protect their coral reef. What is the key physical point?

  1. It would raise dissolved oxygen enough to offset any loss of carbonate ions in seawater
  2. It would reverse acidification fully by cooling the water and so increasing its pH value
  3. It would stop both warming and acidification, provided it continues for at least a century
  4. It might limit warming, but it would not stop acidification, which follows directly from CO₂
Answer and working

D. It might limit warming, but it would not stop acidification, which follows directly from CO₂

Reflecting sunlight does not change seawater carbonate chemistry; acidification is set by atmospheric CO2. Cooling slightly changes pH but cannot reverse the CO2-driven decline, and oxygen does not substitute for carbonate saturation.

A study plan for Climate System Science in CFA Institute Sustainable Investing Certificate

This plan follows where our questions actually fall, so the time goes where the marks are likely to be. It is our reading of the syllabus, not the exam body's weighting.

  1. First, the heavy units (56% of the 18 questions): Carbon budgets and the link between cumulative emissions and warming (3, 17%); Radiative forcing and global warming potential (GWP, GTP, GWP*) (3, 17%); Detection and attribution, including extreme-event attribution (2, 11%); IPCC assessment process and confidence language (2, 11%).

    Read the manual chapters for these first and do every worked question you can find on them.

  2. Then the middle band: Tipping points and irreversibility (2, 11%); Aerosols and their climate effects (1, 6%); Climate feedbacks and equilibrium climate sensitivity (1, 6%); Observed changes: temperature, precipitation, sea level, cryosphere (1, 6%).

    Aim for one sitting per unit, then mixed questions across them.

  3. Then the lighter units: Ocean warming, deoxygenation and acidification (1, 6%); The global carbon cycle: pools, fluxes and the airborne fraction (1, 6%); The natural greenhouse effect and the energy budget (1, 6%).

    Learn the definitions, classifications and standard numbers; these units are more often recalled than worked.

  4. Leave time for the hard ones: Detection and attribution, including extreme-event attribution (1 hard of 2), Carbon budgets and the link between cumulative emissions and warming (1 hard of 3), Radiative forcing and global warming potential (GWP, GTP, GWP*) (1 hard of 3).

    Come back to these after a first pass, untimed, and read every explanation, including for the options you rejected.

  5. Bank the easy marks: Radiative forcing and global warming potential (GWP, GTP, GWP*) (1 easy of 3).

    Do these early in revision so they are fast on the day.

  6. Finish timed. Sit the subject as a timed set without notes, mark it, and send each wrong answer back to its unit above.

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