Abstract
Two globally extensive forms of atmospheric pollution (carbon dioxide and particulate loading) are each considered from the viewpoint of long-term changes in their total abundance, and the impact of such changes on the equilibrium temperature of the Earth.
A comparison of the observed levels of atmospheric CO2 since 1958 with estimates of the fossil CO2 input to the atmosphere from human activities indicates that between 50 and 75% of the latter has remained in the atmosphere. The present-day CO2 excess (referred to 1850) is estimated at 11%; the excess is conservatively projected to increase to 15% by 1980, 22% by 1990, and 32% by 2000 A.D. Changes of mean atmospheric temperature due to C02, calculated by Manabe et al. [20] as about 0.3°C per 10% change of CO2, are sufficient to account for only about one-third of the observed warming of the Earth between 1880 and 1940, but would appear capable of contributing a further warming of about 0.6°C between the present time and the end of the century.
The total global atmospheric loading by small particles is estimated at about 4 × 107 tons at present, of which about 1 × 107 tons is derived directly or indirectly from human activities. If the anthropogenic fraction should grow in the future at about 4% yr-1, the total loading would increase to a level at the end of this century about double that of the 19th century, and 60% above present-day levels. At present, the total anthropogenic loading is estimated to exceed the average stratospheric loading by volcanic dust during the past 120 yr, and to equal about one-fifth of the stratospheric loading following the 1883 eruption of Krakatoa. The impact of anthropogenic particle loading changes on mean temperature cannot be reliably determined from present information although a cooling effect is likely.
Of the two forms of pollution, it appears that the carbon dioxide increase is more influential in raising planetary temperatures than the anthropogenic particle increase is in lowering planetary temperatures. (If, however, both the CO2 and particle inputs to the atmosphere should grow at equal rates in the future, the relative importance of particle effects will increase and could eventually become dominant.) In balance, the net thermal impact of all global-scale pollution (including thermal pollution) is likely to be one of warming, perhaps increasingly so after 2000 A.D. It is concluded that the cooling of climate since 1940, apparently still in progress, is a natural phenomenon plausibly related to an enhanced stratospheric loading by volcanic dust in the period. Natural variations of climate have been larger than those probably induced by human activities during the past century, but the rapidity with which human impacts on atmospheric quality threaten to grow in the future has disturbing climatic overtones that demand better understanding.
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References
U.S. Public Health Service: Air Over Cities, SEC Tech. Report A62–5, Cincinnati (1962).
U.S. Public Health Service: Air Quality Criteria for Particulate Matter, NAPCA Publ. No. AP-49, U.S. Government Printing Office (1969).
Robinson, E.: in A. C. Stern (ed.), Air Pollution, Academic Press, N.Y., Vol. I, pp. 349–400 (1968).
Junge, C. E.: Air Chemistry and Radioactivity, Academic Press, N.Y., p. 228 (1963).
Robinson, E. and Robbins, R. C.: Sources, Abundance and Fate of Gaseous Atmospheric Pollutants, American Petroleum Institute, N.Y. (1968).
Lamb, H. H. and Johnson, A. I.: Geogr. Ann. 41, 94–134 (1959)
ibid. 43, 363–400 (1961).
Lamb, H. H.: in H. Flohn (ed.), World Survey of Climatology, Vol. 2, Elsevier Publishing Company, Amsterdam, pp. 173–249 (1969).
Lamb, H. H.: Climate, Present, Past and Future, Vol. 1, Methuen, London/Barnes and Noble, N.Y. (1972).
Mitchell, J. M., Jr.: in H. E. Wright and D. G. Frey (eds.), The Quaternary of the United States, Princeton University Press, pp. 881–901 (1965).
Mitchell, J. M., Jr.: in R. W. Fairbridge (ed.), Encyclopedia of Atmospheric Sciences and Astrogeology, Reinhold Publishing Co., pp. 211–213 (1967).
Mitchell, J. M., Jr.: Ann. N.Y. Acad Sci. 95, 235–250 (1961).
Mitchell, J. M., Jr.: in Changes of Climate, Arid Zone Research, XX, UNESCO, Paris, pp. 161–181 (1963).
Wilson, C. L. et al. (eds.), Inadvertent Climate Modification (SMIC Report), MIT Press, Cambridge, Mass., pp. 40–45 (1971).
Reitan, C. H.: An Assessment of the Role of Volcanic Dust in Determining Modern Changes in the Temperature of the Northern Hemisphere, Ph.D. Thesis, Univ. of Wis.-Madison, Xerox University Microfilms, Ann Arbor, Mich. (1971).
Emiliani, C.: in K. K. Turekian (ed.), The Late Cenozoic Glacial Ages, Yale University Press, New Haven, pp. 183–197 (1971).
Machta, L.: in D. Dyrssen and D. Jagner (ed.), ‘The Changing Chemistry of the Oceans’, Nobel Symp. 20, Almqvist and Wiksell, Stockholm, John Wiley and Sons, N.Y., pp. 121–145 (1972).
Machta, L. and Telegadas, K.: in W. N. Hess (ed.), Weather Modification, John Wiley and Sons, N.Y. (in press) (1973).
Callendar, G. S.: Tellus 10, 243–248 (1958)
C. E. Junge in [2].
Keeling, C. D.: personal communication.
Pales, J. C. and Keeling, C. D.: J. Geophys. Res. 70, 6053–6075 (1965).
Brown, C. W. and Keeling, C. D.: J. Geophys. Res. 70, 6077–6085 (1965).
Machta, L.: personal communication.
Kelly, J. J., Jr.: An Analysis of Carbon Dioxide in the Arctic Atmosphere near Barrow, Alaska, 1961 to 1967, Scientific Report, Dept. of Atmospheric Sciences, University of Washington (1969).
Bolin, B. and Bischof, W.: Tellus 22, 431–442 (1970).
Bischof, W.: Summary of Recent Carbon-Dioxide Measurements in the Atmosphere, Summary Letter 11/1813, Institute of Meteorology, University of Stockholm (1971).
Keeling, C. D., Adams, J. A., Ekdahl, C. A., and Guenther, P. R.: Atmospheric Carbon Dioxide Variations at the South Pole, 1957–1970 (in preparation) (1972).
Revelle, R. and Suess, H. E.: Tellus 9, 18–27 (1957).
Keeling, C. D.: Industrial Production of Carbon Dioxide from Fossil Fuels and Limestone (to appear in Tellus) (1973).
Rotty, R. M.: personal communication.
Pytkowicz, R. M.: Fossil Fuel Burning and Carbon Dioxide — A Pessimistic View (to appear in Comments on Earth Sciences: Geophysics, Gordon and Breach, N.Y.) (1973).
Keeling, C. D., Bacastow, R., and Ekdahl, C. A.: Diminishing Role of the Oceans in Industrial CO 2 Uptake During the Next Century (in preparation) (1973).
Bolin, B. and Eriksson, E.: in B. Bolin (ed.), The Atmosphere and Sea in Motion, Rockefeller/Oxford Press, pp. 130–142 (1959)
C. E. Junge in [2].
Manabe, S. and Strickler, R. F.: J. Atmos. Sci. 21, 361–385 (1964).
Manabe, S. and Wetherald, R. T.: J. Atmos. Sci. 24, 241–259 (1967).
Wetherald, R. T.: personal communication.
Rasool, S. I. and Schneider, S. H.: Science 173, 138–141 (1971).
Barrett, E. W.: Solar Energy 13, 323–337 (1971).
Bryson, R. A. and Wendland, W. M.: in S. F. Singer (ed.), Global Effects of Environmental Pollution, Springer-Verlag N.Y./D. Reidel Publ. Co., Dordrecht, pp. 130–138 (1970).
Budyko, M. I.: Tellus 21, 611–619 (1969).
McCormick, R. A. and Ludwig, J. H.: Science 156, 1358–1359 (1967).
Peterson, J. T.: The Climate of Cities, A Survey of Recent Literature, National Air Pollution Control Admin., Publ. No. AP-59 (1969).
Ludwig, J. H., Morgan, G. B., and McMullen, T. B.: Eos. 51, 468–475 (1970).
Davitaia, F. F.: Trans. Soviet Acad. Sci., Geogr. Ser., No. 2, pp. 3–33 (1965).
Cobb, W. E. and Wells, H. E.: J. Atmos. Sci. 27, 814–819 (1970).
McCormick, R. A. and Ludwig, J. H.: Science 156, 1358–1359 (1967).
Ellis, H. T. and Pueschel, R. F.: Science 172, 845–846 (1971).
Pueschel, R. F., Machta, L., Cotton, G. F., Flowers, E. C., and Peterson, J. T.: Nature 240, 545–547 (1972).
Peterson, J. T. and Bryson, R. A.: Science 162, 120–122 (1968).
Hodge, P. W., Laulainen, N., and Charlson, R. J.: Science 178, 1123–1124 (1972).
Cobb, W. E.: J. Atmos. Sci. 30, 101–106 (1973).
Wilson, C. L. et al. (eds.), Man’s Impact on the Global Environment (SCEP Report), MIT Press, Cambridge, Mass. (1970).
Wilson, C. L. et al. (eds.), Inadvertent Climate Modification (SMIC Report), MIT Press, Cambridge, Mass. (1971).
Matthews, W. H., Kellogg, W. W., and Robinson, G. D. (eds.), Man’s Impact on the Climate, MIT Press, Cambridge, Mass. (1971).
Flohn, H.: personal communication; Machta, L.: personal communication; see also [9].
Englemann, R. J. and Slin, W. G. N.: (eds.), Precipitation Scavenging (1970), U.S. Atomic Energy Comm., Oak Ridge, Tenn./National Technical Information Center, Springfield, Va.
Poet, S. E., Moore, H. E., and Martell, E. A.: J. Geophys. Res. 77, 6515–6527 (1972).
Dyer, A. J. and Hicks, B. B.: Quart. J. Roy. Meteorol. Soc. 94, 545–554 (1968)
C. E. Junge in [2].
Lamb, H. H.:Phyl. Trans. Roy. Soc. London, A 266, 425–533 (1970).
Deirmendjian, D.: Global Turbidity Studies. I. Volcanic Dust Effects — A Critical Survey, Report R-886-ARPA, Rand Corp., Santa Monica (1971).
Cronin, J. F.: Science 172, 847–850 (1971).
Volz, F. E.: Appl. Optics 8, 2505–2517 (1969).
Mitchell, J. M., Jr.: in S. F. Singer (ed.), Global Effects of Environmental Pollution, Springer-Verlag N.Y./D. Reidel Publ. Co., Dordrecht, pp. 139–155 (1970).
Ellis, H. T. and Pueschel, R. F.: Science 172, 845–846 (1971).
Bullrich, K.: 1964, in H. E. Landsberg (ed.), Advances of Geophysics, Academic Press, N.Y., pp. 99–260 (1964).
Deirmendjian, D.: Electromagnetic Scattering on Spherical Poly dispersons, American Elsevier, N.Y. (1969).
Van de Hulst, H. C.: Light Scattering by Small Particles, John Wiley and Sons, N.Y. (1957).
Plass, G. N.: Appl. Optics 5, 279–285 (1966).
Braslau, N. and Dave, J. V.: Effect of Aerosols on the Transfer of Solar Energy through Realistic Model Atmospheres (to appear in J. Appl. Meteorol.), (1973).
Robinson, G. D.: Long-Term Effects of Air Pollution — A Survey, Center for the Environment and Man, Inc., Hartford, pp. 21–24 (1970).
Eiden, R.: Appl. Optics 5, 569–575 (1966)
ibid. 10, 749–754.
Fischer, K.: Beitr. Physik Atmosphäre 43, 244–254 (1970).
Ensor, D. S., Porch, W. M., Pilat, M. J., and Charlson, R. J.: J. Appl. Meteorol. 10, 1303–1306 (1971).
Mitchell, J. M., Jr.: J. Appl. Meteorol. 10, 703–714 (1971).
Mitchell, J. M., Jr.: in Proc. Internat. Symposium on Physical and Dynamical Climatology, Leningrad, 1971, World Meteorological Organization, Geneva (in press) (1973).
Yamamoto, G. and Tanaka, M.: J. Atmos. Sci 29, 1405–1412 (1972).
Rasool, S. I. and Schneider, S. H.: Science 173, 138–141 (1971).
Dwyer, H. A. and Petersen, T.: J. Appl. Meteorol. 12, 36–42 (1973).
Bryson, R. A. and Wendland, W. M.: this volume, pp. 139–147.
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Mitchell, J.M. (1975). A Reassessment of Atmospheric Pollution as a Cause of Long-Term Changes of Global Temperature. In: Singer, S.F. (eds) The Changing Global Environment. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-1729-9_12
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