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salts to the world’s oceans and seas. Whether this Burke, J.J. & Moench, M.H. (2000) Groundwater and Society:
additional salt load would increase the salinity of resources, tensions and opportunities. United Nations
the oceans is uncertain and depends on the balance Department of Economic and Social Affairs and Institute
of water inputs to and from the oceans under an for Social and Environmental Transition, United
intensified hydrological cycle and any volume change Nations, New York.
Cook, H.F. (1998) The Protection and Conservation of Water
in the oceans as a result of thermal expansion and ice
Resources: a British perspective. John Wiley, Chichester.
melting. It should also be considered that these
Hiscock, K.M., Rivett, M.O. & Davison, R.M. (eds) (2002)
effects of changes in direct groundwater flow might
Sustainable Groundwater Development. Geological Society,
only stabilize over timescales of hundreds to thou- London, Special Publications, 193.
sands of years. IPCC (2001) Climate Change 2001. The scientific basis. A
Report of Working Group I of the Intergovernmental
Panel on Climate Change. Cambridge University Press,
8.6 FURTHER READING Cambridge.
Arnell, N. (1996) Global Warming, River Flows and Water Keddy, P.A. (2000) Wetland Ecology: principles and conserva-
Resources. John Wiley, Chichester. tion. Cambridge University Press, Cambridge.
Arnell, N. (2002) Hydrology and Global Environmental Change. Mitsch, W.J. & Gosselink, J.G. (2000) Wetlands, 3rd edn.
Prentice Hall, Harlow. John Wiley, New York.