CFA Institute Sustainable Investing Certificate (formerly Certificate in ESG Investing) · International · CFA Institute
Original practice questions written to the published syllabus · not past papersCFA 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.
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.
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.
AR6 assessed the Earth's energy imbalance for 2006–2018. Which statement correctly describes it and where the extra energy has gone?
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.
Why does stopping sulphur dioxide emissions produce a near-term warming, while stopping CO₂ emissions does not cause a rapid drop in temperature?
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.
Which statement about observed extremes matches the AR6 assessment?
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.
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)?
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).
A newspaper reports that climate change made a recent flood-producing rainfall event 'five times more likely'. Which interpretation is correct?
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.
Why does stopping CO₂-driven warming require net zero CO₂ emissions rather than merely reducing emissions?
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.
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?
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.
For a risk manager, what is the most defensible way to treat climate tipping points given current science?
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.
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?
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.
A coastal resort's planners ask whether a solar-radiation-modification programme would protect their coral reef. What is the key physical point?
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.
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.
Read the manual chapters for these first and do every worked question you can find on them.
Aim for one sitting per unit, then mixed questions across them.
Learn the definitions, classifications and standard numbers; these units are more often recalled than worked.
Come back to these after a first pass, untimed, and read every explanation, including for the options you rejected.
Do these early in revision so they are fast on the day.
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