Environmental Engineering Reference
In-Depth Information
5. Actions against ozone depletion
The Convention for the Protection of the Ozone Layer, agreed upon in Vienna in
1985, was the start of further efforts among countries to analyse global environmental
problems. Following the publication in Nature by Farman and co-workers 2 the
Montreal Protocol on Substances that Deplete the Ozone Layer was signed in 1987, and
has been adjusted and amended by subsequent meetings including those held in London
(1990), Copenhagen (1992), Vienna (1995) and Beijing (1999). The broad aim of The
Parties to the Montreal Protocol is the protection of the environment and human health
from anthropogenic activities which may modify the ozone layer. The Montreal
Protocol includes provision for developing countries to delay their compliance for up to
10 years based on economics. The main goal of the protocol is to phase out the use of
CFCs in the next few decades.
6. Conclusions
While the international agreements have reduced production of ozone-destroying
compounds, high concentrations are still present in the stratosphere mainly due to their
longevity, and thus ozone depletion will likely continue for several decades 3 .
Monitoring networks are continuously being set up to study biological effects of ozone
depletion and to determine correlations between ozone reduction and UV increases and
to couple these to the biological impact.
References
1. SORG (1999) Stratospheric Ozone, United Kingdom Stratospheric Ozone Review Group. HMSO,
London, UK.
2. Farman, J.C., Gardiner, B.G. & Shanklin, J.D. 1985. Large losses of total ozone in Antarctica reveal
seasonal ClO x /NO x interaction. Nature 315, 207 - 210.
3. WMO (1998) Scientific Assessment of Ozone Depletion. Report 44 . Geneva, Switzerland.
4. Rex, M., Dethloff, K., Handorf, D., Herber, A., Lehmann, R., Neuber, R., Notholt, J., Rinke, A.,
von der Gathen, P., Weisheimer, A. and Gernandt, H. (2000) Arctic and Antarctic ozone layer observations
- chemical and dynamical aspects of variability and long-term changes in the polar stratosphere. Polar
Research , 19: 193-204.
5. Schulz, A., Rex, M., Steger, J., Harris, N., Braathen, G.O., Reimer, E., Alfier, R., Beck, A., Alpers, M.,
Cisneros, J., Claude, H., De Backer, H., Dier, H., Dorokhov, V., Fast, H., Godin, S., Hansen, G., Kondo,
Y., Kosmidis, E., Kyro, E., Molyneux, M.J., Murphy, G., Nakane, H., Parrondo, C., Ravagnani, F.,
Varostos,C., Vialle, C., Yushkov, V., Zerefos, C. and von der Gathen, P. (2000) Match observation in the
Arctic winter 1996/97: High stratospheric ozone loss rates correlate with low temperatures deep inside the
polar vortex. Geophys. Res. Lett. , 27: 205-208.
Further reading
Madronich, S., McKenzie, R.L., Björn, L.O. & Caldwell, M.M. 1998. Changes in biologically active
ultraviolet radiation reaching the Earth's surface. J. Photochem. Photobiol. B:Biol. , 46: 5-19.
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