9.2 - Reducing Ozone Depletion
Learning Objectives
The main objective is to discuss the reduction of stratospheric ozone depletion by looking at substitutes for CFCs. The associated skill is describing an environmental concept or process.
I. The Montreal Protocol (Policy Solution)
- The main way to solve anthropogenic stratospheric ozone depletion is to limit the release of CFCs.
- The Montreal Protocol is a global agreement signed in 1987 (in force since 1989) to phase out CFCs and other ozone-depleting chemicals. It was strengthened several times as the science improved, and in 2009 it became the first UN treaty ratified by every country in the world (198 parties as of 2026). It's often called the most successful environmental treaty ever.
- Results: CFC production ended in developed countries in 1996 and worldwide in 2010. Chlorine in the stratosphere peaked around 2000 and is slowly falling. The 2025 Antarctic ozone hole was the fifth smallest since 1992 (NASA and NOAA). The last full UN assessment (2022) projects that ozone will return to 1980 levels around 2040 over most of the world, around 2045 over the Arctic, and around 2066 over Antarctica; the next assessment is due at the end of 2026. The hole's size still changes from year to year with stratospheric temperatures, so scientists judge recovery by the long-term trend.
II. CFC Substitutes and the Phase-Out
- Two numbers for comparing substitutes: ozone-depleting potential (ODP) measures how much ozone a chemical destroys compared with CFC-11 (ODP = 1). Global warming potential (GWP) measures how much heat it traps compared with the same mass of (GWP = 1, see 9.3). The ideal substitute has an ODP of 0 and a low GWP.
Substitute Iteration | Chemical Name | Characteristics | Status and Goal |
1st Generation | CFCs (Chlorofluorocarbons) | High Ozone Depleting Potential (ODP). Very high Global Warming Potential (GWP): CFC-12's is about 12,500. | Phased out under the Montreal Protocol (1987). Production ended in developed nations in 1996 and worldwide in 2010. |
2nd Generation | HCFCs (Hydrochlorofluorocarbons) | CFCs with added hydrogens. Less ozone depleting (HCFC-22's ODP is 0.055, about 5% of CFC-11's), but still a high GWP (about 1,960 for HCFC-22). | Considered a transition solution. Developed nations like the U.S. cut production 99.5% by 2020 (only enough is left to service old equipment) and end it in 2030. Developing nations cut 97.5% by 2030 and end it by 2040. |
3rd Generation | HFCs (Hydrofluorocarbons) | Zero Ozone Depleting Potential, because the ozone-breaking chlorine atom was taken out of the chemical equation. Still a high GWP (about 1,530 for HFC-134a, long used in car air conditioners). | Widely used since the 1990s. Now being phased down under the Kigali Amendment (2016). |
4th Generation | HFOs (Hydrofluoroolefins) | HFCs with a carbon-carbon double bond. That double bond shortens their atmospheric lifetime (days instead of years) and dramatically lowers their GWP. HFO-1234yf, which replaced HFC-134a in many new cars, has a GWP below 1. | The most recent evolutionary step. |
III. The Kigali Amendment (Phasing Down HFCs)
- Why it was needed: HFCs solved the ozone problem but created a climate problem. That's the CED's point that some replacements are strong greenhouse gases: HFC-134a traps about 1,530 times as much heat as the same mass of over 100 years, and HFC use was growing fast as air conditioning spread in hot, developing countries.
- What it does: the Kigali Amendment to the Montreal Protocol (adopted in Kigali, Rwanda, in October 2016, in force since 2019) phases HFCs down by about 80 to 85% by the late 2040s. Developed countries began cutting in 2019 and must reach an 85% cut by 2036. Most developing countries froze their HFC use in 2024, and a few very hot countries, like India, freeze in 2028.
- Who's in (as of 2026): more than 170 parties have ratified it. The US ratified it in 2022 and carries out its phasedown through the EPA under the AIM Act (2020).
- Payoff: the 2022 UN ozone assessment estimated that following the Kigali Amendment avoids about 0.3 to 0.5°C of warming by 2100.
IV. Other Substitutes: Natural Refrigerants
- Some uses skip fluorinated chemicals entirely. Most home refrigerators sold in Europe use isobutane (a hydrocarbon with a GWP of about 3), and many supermarket and industrial freezers use ammonia or .
- Trade-offs: hydrocarbons are flammable, ammonia is toxic, and systems have to run at very high pressure, so each needs special equipment and safety rules.
Big picture
Reducing stratospheric ozone depletion has been largely successful thanks to the Montreal Protocol of 1987, which mandated the phase-out of CFCs. Those ozone-destroying chemicals got replaced in sequence, first with HCFCs (less damaging to ozone but still potent greenhouse gases) and then with HFCs (which solved the ozone problem entirely by removing the damaging chlorine atom). The most sustainable evolution is the current use of HFOs, which dramatically lower global warming potential by shortening atmospheric lifetime.