The Global Environment-II: The Ozone Layer

Alok B Guha

The Global Environment Facility (GEF) supports the Small Grants Programme to initiate small grassroots activities in various developing countries. Development Alternatives is the National Host Institution and houses the small secretariat which processes and assists NGOs to develop project proposals. The thematic areas include climate change, ozone layer depletion, biodiversity conservation and international waters’ protection. For the benefit of grassroots NGOs, we are serialising five short articles on what these thematic areas imply to help NGOs develop valid ideas for projects. This is the second article in the series and draws from material prepared by GEF, UNDP and the United Nations Environment Programme (UNEP).

The ozone layer, comprising a protective layer of gas some 10 to 50 kms above the earth’s surface, is responsible for absorbing most of the solar ultraviolet radiation and  preventing it from  reaching the earth’s surface.  The ozone in the stratosphere is continuously formed and destroyed by chemical reactions triggered by sunlight.  However, release of ozone depleting chemicals - mainly Chloro Fluoro Carbons (CFCs) and halons - is eroding the ozone layer, thereby increasing the amount of ultra-violet radiation reaching the earth’s surface. In effect, CFCs are raising the global temperature and augmenting the detrimental impact of ultra-violet rays on human health.

It is well established that ultra-violet rays cause skin cancers and other diseases.  Besides permitting more ultra-violet radiation into the earth’s atmosphere, these chemicals prevent infra-red radiation from escaping  the earth’s atmosphere, thereby trapping the heat being radiated out of the atmosphere. Actually, these are highly effective greenhouse gases complementing the build up of carbon dioxide in raising the temperature of the earth and accounting for an estimated 20 to 25 per cent share in the cause for global warming.

CFCs and halons are being produced at record levels even though their deleterious effects were recognised some 15 to 20 years ago.  These chemicals are used in aerosol spray cans, for artificial cooling (refrigeration, air-conditioning), manufacturing soft seat cushions and foam-insulation.

In the 1930s, when CFCs were first used as refrigerants in the cooling cycle of refrigerators, nobody imagined that these chemicals could damage the ozone layer.  The fact that solar radiation breaks down CFCs, releasing chlorine radicals which in turn disintegrate the ozone  molecule, was discovered only during 1970s and 1980s.  Depletion of ozone levels increases the amount of ultra-violet radiation reaching the earth’s surface.  One form of this radiation, UV-B, causes eye cataract, melanoma and non-melanoma skin cancers, suppression of the immune systems in humans, interferes with natural growth rates in ecosystems and degrades some kinds of plastics.  CFCs, (used in refrigeration, as aerosol propellants, as cleaning fluids and in the blowing of plastic foams), are the main cause of ozone depletion but many other chemicals are also implicated, including carbon tetrachloride used in dry-cleaning, methyl chloroform used as a solvent, halons used in fire extinguishers and methyl bromide used in fumigating the soil and crops against pests. 

Even though, initially, just a few countries took the threat seriously, there was sufficient concern to enact the Vienna Convention on the Protection of the Ozone Layer in 1985.  Only a few months later, the British confirmed that severe ozone layer depletion was occurring over the Antarctica during the spring every year.  The evidence pointed to ozone depleting substances (ODS) as a cause of this ozone hole.  This was followed by the Montreal Protocol (1987) and then a series of ever stricter adjustments and amendments made to it at various international meetings.  The ODS originally planned to be controlled under the Montreal Protocol included 5 CFCs and 3 halons.

The London amendment (1990) added methyl chloroform, carbon tetrachloride and some other range of CFCs to be phased out, while the Copenhagen Amendment (1992) added Hydro Chloro Fluoro Carbons (HCFCs), Hydro Bromo FluoroCarbons (HBFCs) and methyl bromide.  The developed countries were required to phase out the production and consumption of halons by 1994, and of CFCs, carbon tetrachloride, methyl chloroform and HBFCs by 1996.   Methyl bromide is to be phased out by 2005 and HCFCs by 2030. 

The developing countries have a longer phase-out period. They phased out the HBFCs in 1996.  The developing countries are required to take the first step in eliminating ODS by freezing the production of CFCs at average 1995-97 levels on July 1, 1999.  Some developing countries are  already well ahead of their commitments under the Montreal Protocol, having effectively reduced CFC production and consumption even before the Montreal deadlines.  Prospects of attaining the ‘1999 Freeze’  are good for other developing countries.

Without the Montreal Protocol, ozone depletion would have become a substantial environmental hazard to the well being of humankind.  Without the phase-out of ODS substances, it is estimated that in the United States and North West Europe alone, an additional 1.5 million and 5,50,000 people, respectively, would have become victims of skin cancer.  The  Montreal Protocol does reduce these figures to 4,40,000 and 1,70,000, respectively.  While with the Copenhagen amendments, it is now likely to result in only 8,000 more cases of skin cancer in the United States and 4,000 more in North West Europe by 2100.

On the negative side, statistics show that CFC use is still increasing in many developing countries and more attention needs to be paid to small and medium sized enterprises and to countries that consume only very low volumes of ODS.  Growth of illegal trade in CFCs is also a problem, with the Institutional Trade Information Service estimating that as much as one quarter of global CFC production in 1996 was produced for illegal export to developed countries.

While action to reduce release of ODS in the atmosphere has been impressive, it has produced very little difference to the ozone layer itself due to the long life of already released CFCs.  Ozone levels will return to normal only after all the CFCs have disappeared from the atmosphere, a process expected to take upto 2050.  Nothing can change the fact that the average lifetime of a CFC-11 molecule in the atmosphere is 50 years and that of a CFC-12 molecule is 100 years.  Thus globally, average ozone levels continue to fall by about 5 per cent a decade over mid-latitudes.

Thus, in the Antarctic spring of 1997, total ozone levels were about 33 per cent less than in the late 1970s - similar to previous record-lows in 1993 and 1996.  In the 12-20 km layer, ozone was almost completely annihilated for more than 40 continuous days.  The hole extended to more than 20 million square kms, reaching well within the southern tip of South America.

Substantial depletion has also been observed in the northern hemisphere, with ozone levels being reduced to 64 per cent of their normal values in some places in the winter of 1996-97.  Record-highs have recently been discovered in both ozone destruction and  UV-B radiation levels over populated areas at middle and high latitudes in the Northern hemisphere during the winter and early spring.  While levels of chlorine in the atmosphere are still increasing, the annual rate of increase is now much slower.  Chlorine concentrations are now expected to peak about 2000 parts per billion by volume and then decline slowly.

What is obvious is the fact that small grassroots NGOs can not do much to reduce the ODS-promoted problems of stratospheric ozone depletion under the Small Grants Programme.  What they could perhaps still do is build public awareness and provide education to the lay public with regard to problems arising out of the present day technologies using ODS and raise public concern and demand for a quick change-over of technology (in refrigeration, sprays, cushions, etc.) which does not affect the ozone layer.

This article is based on a previous article by the author and published in the Deccan Herald some time ago.  It also draws on material published by the United Nations Environment Programme titled “Where We Stand: A State of the Environment Overview of the Global Environment Facility”, which is essentially a report from the Global Environment Outlook Programme. q

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