From a warning in 1974 to the Montreal Protocol in 1987, and the recovery since
Source: Molina and Rowland, Nature 249 (1974); British Antarctic Survey October ozone at Halley (Shanklin 2001); Montreal Protocol 1987; Decision XXI/1 of the Parties (UNEP, 2009).
Source: Molina and Rowland, Nature 249, 810–812 (1974); BAS, October ozone at Halley (Shanklin 2001) and BAS bulletin 95/96 (1957–72 mean 300 DU); Montreal Protocol (16 Sep 1987); UNEP Decision XXI/1 (2009); WMO/UNEP Scientific Assessment of Ozone Depletion 2022 (2066 projection).
In 1987 nobody had fully proven that CFCs were punching the hole in the ozone layer. Why did almost the whole world agree to cut them anyway? Because waiting cost more than being wrong: an ozone layer, once lost, cannot be bought back.
The answer is Mark's view, based on the sourced milestones in Parts 2 and 3.
The first picture is real data: mean October ozone (Antarctic spring) at the British Antarctic Survey's Halley station.
Source: Molina and Rowland, Nature 249 (1974); FDA and EPA, 43 FR 11301 (17 Mar 1978) and EPA release on the ban from 15 Oct 1978; Vienna Convention 1985 (UNEP Ozone Secretariat); Farman, Gardiner and Shanklin, Nature 315, 207–210 (1985), "a third" per UKRI (secondary source); Stolarski et al. (1986), Nimbus-7 satellite; Montreal Protocol 1987, cuts per Britannica (secondary source); entry-into-force condition from the Protocol text (Article 16), via Wikipedia (secondary source); London Amendment 1990; Nobel Foundation (1995); NASA/NOAA 2025; UNEP Decision XXI/1 (2009); Kigali Amendment 2016; WMO Ozone and UV Bulletin No. 4 (16 Sep 2026); WMO/UNEP Scientific Assessment 2022, years per AP 9 Jan 2023 (secondary source).
Five decisions, seen through the eyes of the time: who decided, what they knew, what they chose, what followed.
Source: FDA and EPA, 43 FR 11301 (17 Mar 1978); EPA release "Government Ban on Fluorocarbon Gases in Aerosol Products Begins October 15" (1978); CPSC 1977 (via search excerpts, full text not opened).
Source: Vienna Convention 1985 (UNEP Ozone Secretariat); Farman et al., Nature 315 (May 1985). The "table already existed" point is Mark's view.
Source: Montreal Protocol 1987; number of signatories per Nature and UNEP (some sources such as Britannica say 46, counting countries that signed later); memorandum to President Reagan, FRUS 1981–88 vol. XLI, doc. 375 (Europe, Japan, the Soviet Union signed); four-yearly assessments per UNEP/WMO 2022.
Source: London Amendment 1990 and Article 5 of the Protocol (UNEP Ozone Secretariat); BAS, October ozone at Halley (Shanklin 2001); UNEP Decision XXI/1 (2009).
Source: Kigali Amendment 2016 (UNEP); WMO/UNEP Scientific Assessment 2022, the 0.3–0.5 °C figure per Al Jazeera/AP 9 Jan 2023 and IIFIIR (secondary sources).
What changed after the event: laws, institutions, habits.
14 things often said about the ozone layer, checked against measurements and scientific reports. Tap each line for the reasoning.
Molina and Rowland, Nature 249, 810–812 (1974): CFCs are long-lived, rise to the stratosphere, ultraviolet light frees chlorine, and chlorine destroys ozone in a chain. In 1995 both, with Paul Crutzen, won the Nobel Prize in Chemistry.
Farman, Gardiner and Shanklin used a Dobson spectrophotometer at Halley (Nature, May 1985). Stolarski et al. (1986) confirmed it with TOMS and SBUV data from the Nimbus-7 satellite.
By September 1987 the hole had been measured, but the chlorine explanation still competed with hypotheses about polar meteorology. A NASA assessment in 1988, after the signing, clearly tied the loss to CFCs.
On 16 Sep 2009, with 196 parties, the Vienna Convention and the Montreal Protocol became the first treaties in UN history to achieve universal ratification (UNEP, Decision XXI/1).
About 99%, according to the WMO/UNEP Scientific Assessment 2022 (as summarised by UNEP).
CFCs are also strong greenhouse gases. Velders et al. (PNAS, 2007): Montreal's climate benefit is "far larger" than Kyoto's first commitment target; the authors presented it as about 5–6 times in 2010.
The EPA's 443 million cases is a model estimate, only for people born in the US between 1890 and 2100, against a no-controls scenario. The large benefit is real, but it is not a count and not global.
This is the "world avoided" model scenario of Newman et al. (ACP, 2009): if CFCs had grown 3% a year, 17% of global ozone would be lost by 2020 and 67% by 2065. Useful to see the scale, not a certainty.
Two different problems: the ozone hole is about ultraviolet light, warming is about greenhouse gases. But they are linked: CFCs and HFCs are greenhouse gases, so cutting them also helps the climate (Velders 2007; Kigali Amendment).
Not healed, and not "by itself": the ozone layer is recovering because people cut CFCs. In 2025 the hole still averaged 18.71 million km² (NASA/NOAA). Return to 1980 levels is projected around 2066 over Antarctica (2022 Assessment).
Continuous measurements at Halley since 1956: October mean 300 DU (1957–72), down to 150 DU in 1987 and 122 DU in 1993. Satellites confirmed it independently. The chemistry earned a Nobel Prize in 1995.
At Halley: 150 DU (1987), 216 DU (1988), 150 DU (1989). WMO says year-to-year swings are mainly meteorological; the long-term trend is what shows recovery.
Winds and convection mix the atmosphere, so heavy and light gases alike are carried up. CFCs have been measured directly in the stratosphere (WMO/UNEP, "Twenty Questions and Answers About the Ozone Layer").
Volcanic chlorine mostly dissolves in water and is rained out in the lower atmosphere. Stratospheric chlorine comes mainly from human-made substances (WMO/UNEP, "Twenty Questions and Answers About the Ozone Layer").
Source: as noted in each line; full list in Part 9.
Scores are Mark's assessment based on the sources in Part 9, not data from a study.
One of the rare times the whole world got it right: it did not wait for 100% certainty, and it did not sign once and stop. The minus is speed, and that slowness is paid for with more than half a century of waiting to heal.
Some conditions helped: few chemicals to cut, few producing companies, substitutes already available, and a danger (skin cancer) that is easy to picture. This is Mark's view, not the finding of a study.
But helpful conditions do not turn into a treaty by themselves. What made the difference was the design: frame first, cut small first, review regularly, and pay the slow. That design works at work too.
For any team that has to decide before the data is complete: a spreading bug, a customer about to leave, a risk that keeps growing.
1. The last decision your team postponed "to wait for more data": what data, and when will it arrive?
2. When the team reports a risk, does it state a confidence level (low, medium, high), or just "not sure yet"?
3. Which running decision has no review date? Write one today.
4. At what threshold does the team tighten, and at what threshold does it relax? Is it written down?
5. Who in the team (or which partner team) will be slowest to change, and what have you done to help them?
Peer-reviewed papers, original measurements and documents from UNEP, WMO, NASA and EPA come first. The working environment blocked most of these sites, so apart from the Halley measurement table (obtained in full), sources were checked through excerpts of the original pages in search results, without opening the full text. Press sources are marked as secondary.