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Montreal Protocol
The Montreal Protocol on Substances that Deplete the Ozone Layer is an international treaty that is designed to protect the ozone layer. The ozone layer is, in a word, the Earth's “sunscreen” that absorbs ultraviolet radiation, thus allowing life to exist on land. The Montreal Protocol was designed to phase out ozone-depleting substances (ODSs)—substances that had been created for various purposes, most famously for use in aerosols, refrigeration, and other forms of air-conditioning. The treaty was signed in 1987 and entered into force in 1989. Since then, the treaty has been amended four times: the London Amendment (adopted in 1990, entered into force in 1992), the Copenhagen Amendment (adopted in 1992, entered into force in 1994), the Montreal Amendment (adopted in 1997, entered into force in 1999), and the Beijing Amendment (adopted in 1999, entered into force in 2002). These amendments allowed for adjustments in protocol rules to accelerate the phase-out of certain ODSs. The Montreal Protocol now touts 191 signatories—a large increase from the original 46 participating countries.
Early History of the Ozone Layer Issue
Stratospheric ozone layer concentrations are rather small, making up only 8–10 parts per million of air at around 15–35 kilometers in altitude. A healthy ozone layer would average only 3 millimeters in thickness if compressed and measured at the Earth's surface. In the atmosphere, it is much less concentrated. However, this small concentration of ozone buffers ultraviolet radiation and aids in the regulation of the Earth's temperature and air circulation. In short, without the ozone layer, life on Earth could not exist. In 1974, chemists F. Sherwood Rowland and Mario Molina published an article predicting that chlorofluorocarbons (CFCs) would deplete the ozone layer. Molina and Rowland discovered that CFCs would persist long enough in the atmosphere to reach the stratosphere, where they could then be broken down by ultraviolet radiation that would release chlorine from the CFC molecule. These chlorine atoms could then potentially break down large quantities of ozone. Molina and Rowland would be awarded the Nobel Prize in Chemistry for their groundbreaking work on the ozone layer issue. However, early scientific research on the effect of CFCs on the ozone layer was hotly contested by the chemical industry. Yet, after Molina and Rowland testified before the U.S. House of Representatives in 1974, considerable funding was provided to tackle the problem. In 1976, the U.S. National Academy of Sciences confirmed the link between CFCs and ozone layer loss, leading to a flood of research on modeling the exact effect of CFCs on the ozone layer.
Based on this and other scientific evidence, in 1985—the same year that the first ozone hole was discovered in Antarctica—the Vienna Convention for the Protection of the Ozone Layer was established to initiate international cooperation in research on the potential of ozone layer loss resulting from human activity. Although not a legally binding agreement, the Vienna Convention set the stage for creating a framework for an international response to ozone layer protection. As late as 1987, the chemical industry still denied the validity of the scientific findings on CFCs, evidenced by the Alliance for Responsible CFC Policy's testimony before the U.S. Congress. Nevertheless, in 1987, the Montreal Protocol was ratified by 29 countries and the European Community, representing 83 percent of world CFC consumption.
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