Ozone-depleting substances and substitutes, global use, 1980-2000

Developments relating to CFCs and halons
The worldwide production and use of chlorofluorocarbons (CFCs) and halons fell sharply between the end of the 1980s and 1997 (AFEAS, 2001). However, after 1997, the production of chlorofluorocarbons remained virtually constant at 15% of the level in the peak year of 1988.
Large volumes of chlorofluorocarbons are stored around the world in products (cooling systems, insulation systems). Annually, some of the cooling or insulation agent leaks from these systems and this leads to emissions are still higher than use levels. The recovery or destruction of chlorofluorocarbons and halons from existing appliances could considerably reduce the volume of these emissions.
Developments in chlorofluorocarbon substitutes
Remarkably, the worldwide use of hydrochlorofluorocarbons (HCFCs), which can be temporarily used as substitutes, has remained constant since 1997. By contrast, the use of hydrofluorocarbons (HFCs) has been growing by about 20% per year since 1996. They have no effect on ozone but do contribute to the greenhouse effect.
Chlorofluorocarbons and halons are also being replaced by perfluorocarbons (PFCs) and sulphur hexafluoride (SF6). However, these are substances that are not used solely as substitutes for chlorofluorocarbons or halons.
Policy
International policy aims to restrict or stop the production and use of ozone-depleting substances. A large number of countries have signed the Montreal Protocol and therefore undertaken to use no more chlorofluorocarbons from 1996 onwards (from 2010 onwards in developing countries).
Relevance
Nitrogen, chlorine and bromine compounds reduce the concentration of ozone in the stratosphere. The ozone layer prevents high levels of ultraviolet (UV) radiation reaching the earth.



