Last updated Tuesday 20 June, 2000 0:33 hrs EST
 



An Assessment Prepared by a Task Group on Behalf of the World Health Organization, the World Meteorological Organization and the United Nations Environment Programme

Edited by A. J. McMichael, A. Haines, R. Slooff and S. Kovats

Climate Change and Human Health
The Concern
Horizontal blue line.

The extent and nature of our industrial and agricultural activities are now so great that the gaseous composition of the lower and middle atmospheres (the troposphere and the stratosphere) has begun to change. This is likely to affect the world's climate, many other of the worldıs natural systems, ground-level exposure to ultraviolet radiation, and indeed, all life on earth.

Climatologists predict that, due to the accumulation of greenhouse gases such as CO2, the climate will change at a rate much greater rate than human societies have experienced since the advent --- approximately 10,000 years ago --- of agriculture and settled living.

Recent increases in temperature and changes in climate variability in numerous parts of the world are regarded by many scientists as the first signals of global climate change caused by human activities.

During the past century, Earth's global mean surface temperature has increased by about 0.3 - 0.6 degrees C. Climate simulations, using the most advanced computer models, indicate that global mean surface temperature may have increased by 1-3 degrees C. by the year 2100.

These models also predict changes in precipitation patterns, including a greater frequency of heavy precipitation and a corresponding increase in foods.

Global mean sea level is predicted to rise by between 0.2 meters and 1.0 meter by the year 2100, and would be expected to continue to rise for several centuries even if greenhouse gas levels were to be stabilized. The current "best estimate" predicts a rate of rise in sea level that is two to three times greater than that experienced during the past 100 years.

Various man-made gases (particularly the halocarbons and N20) have reduced stratospheric ozone levels, especially at higher latitudes. As a result, a greater proportion of solar ultraviolet radiation now reaches Earth's surface. Damage to stratospheric ozone continues, and the rate of overall ozone depletion has risen during the 1990s.


About the Book

Work on the report began in 1993 following receipt of a grant from the United States Environmental Protection Agency. Further financial resources were obtained from the government of the Netherlands and the three participating UN agencies (WHO,WMO, and UNEP, with WHO designated the coordinating agency). An international task group of experts was formed under the direction of A. J. Michael, and met three times in two years. The views expressed in the report reflect the consensus reached by this Task Group and do not necessarily reflect the the policies of the participating agencies.


 

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