Mankind’s Greenhouse Effect: Is It Already Here?
The addition to the atmosphere of infrared-absorbing (greenhouse) gases by the activities of mankind is changing the composition of the atmosphere, and theory tells us that this must cause a global warming. The worldwide burning of fossil fuels and the production of carbon dioxide is currently the single largest influence on our global temperature and climate, and other manmade trace gases are also contributing to the greenhouse effect. As a result of the increase of these greenhouse gases Planet Earth has warmed as a whole by 0. 5 to 0.6 K in this century, and will continue to warm. Other environmental changes are also beginning to take place gradually, such as changes in distribution of rainfall and snowfall. All of these will have an impact on mankind. The community of nations is now debating what action, if any, it is prepared to take to slow the inevitable climate change.
KeywordsBiomass Burning Methane Dioxide Hydrate
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- 1.Post, W.M., T.-H. Peng, W.R. Emanuel, A.W. King, V.H. Dale, and D.L. DeAngelis, 1990: The global carbon cycle. American Scientist, 78, 310–326.Google Scholar
- 7.Kondratyev, K.Ya., 1988: Climate Shocks: Natural and Anthropogenic. Wiley Interscience, New York, 295 pp.Google Scholar
- 12.Arrhenius, S., 1896: On the influence of carbonic acid in the air upon the temperature of the ground. Philosophical Magazine, 41, 237–271;Google Scholar
- 12a.see also S. Arrhenius, 1906: Worlds in the Making. Harper and Brothers, New York and London, 250 pp.Google Scholar
- 15.Kellogg, W.W., 1990: Theory of climate: Transition from academic challenge to global imperative. Chapt in Greenhouse Glasnost: The Crisis of Global Warming, ed. by T.J. Minger, Inst. for Resource Management and Ecco Press, New York, pp. 93–115.Google Scholar
- 17.Kellogg, W.W., 1982: Precipitation trends on a warmer Earth. Chapt. in Interpretation of Climate and Photochemical Models, Ozone and Temperature Measurements, ed. by R.A. Reck and J.R. Hummel, American Inst. of Physics, New York, p. 35–46.Google Scholar
- 18.NRC, 1985: Glaciers, Ice Sheets, and Sea Level: Effect of a CO2-Induced Climatic Change, Polar Research Board, National Research Council, Washington, D.C., 330 pp.; see also Villach/Bellagio Workshops, 1987: Developing Policies for Responding to Climatic Changes. Report of workshops held in Villach, Austria (23 Sept.-2 Oct., 1987) and Bellagio, Italy (9–13 November, 1987), rept. prepared by Jill Jaeger, World Meteorological Organization Rept. WCIP-1, WMO/TD-No. 225, Geneva, Switzerland.Google Scholar
- 21.Keeling, C.D., 1990: Personal communication.Google Scholar
- 22.Kellogg, W.W., and R. Schware, 1981: Climate Change and Society: Consequences of Increasing Atmospheric Carbon Dioxide, Westview Press, Boulder, Colorado, 178 pp.;Google Scholar
- 23.Schneider, S.H., 1989: Global Warming: Are We Entering the Greenhouse Century? Sierra Club Books, San Francisco, 275 pp.Google Scholar
- 24.Marland, G., 1989: Fossil fuels CO2 emissions: Three countries account for 50% in 1986. Carbon Dioxide Information Analysis Center (CDIAC), Oak Ridge National Laboratory, Oak Ridge, Tenn., p. 1–3.Google Scholar
- 25.MacKenzie, J.J., 1988: Breathing Easier: Taking Action on Climate Change, Air Pollution, and Energy Insecurity. World Resources Inst., Washington, D.C., 23 pp.Google Scholar