Environment

Ozone depletion

Also: ozone hole, Montreal Protocol, Kigali Amendment

Definition
The thinning of the ozone layer in the stratosphere, mainly caused by man-made chlorine and bromine compounds such as CFCs and halons, which allows more harmful ultraviolet-B radiation to reach the Earth's surface.
Deep-dive lesson: Pollution, Climate Change and International Conventions. This page is a quick reference that connects the term across subjects; read the lesson for the full treatment.
Summary card: Ozone depletion. Ozone layer: mainly in the stratosphere, about 15–35 km up. Culprits: CFCs, halons, carbon tetrachloride, methyl chloroform. Vienna Convention 1985; Montreal Protocol 1987. Kigali Amendment 2016 phases down HFCs. 16 September: International Day for the Preservation of the Ozone Layer
Summary card © UPSCPrep.in

Background and evolution

Ozone is a molecule of three oxygen atoms. Close to the ground it is a harmful pollutant, but high in the stratosphere it forms a thin shield that absorbs most of the sun's ultraviolet-B rays, which damage DNA, cause skin cancer and cataracts, and harm plants and plankton. In 1974 the chemists Mario Molina and Sherwood Rowland warned that chlorofluorocarbons (CFCs), then widely used in refrigerators, aerosol sprays and foams, could rise to the stratosphere and destroy ozone. In 1985 scientists of the British Antarctic Survey reported a dramatic seasonal fall in ozone over Antarctica, the so-called "ozone hole".

The international response was unusually fast. The Vienna Convention for the Protection of the Ozone Layer (1985) set a framework, and the Montreal Protocol (1987) set binding phase-out schedules. Over time, amendments added more chemicals and sped up timelines. The Montreal Protocol became the first UN treaty to achieve universal ratification.

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Last reviewed: 23 October 2026 · Original UPSCPrep.in content.