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Theoretical and Applied Climatology

, Volume 44, Issue 1, pp 37–41 | Cite as

Surface air temperature response to increasing global industrial productivity: A beneficial greenhouse effect?

  • S. B. Idso
  • R. C. BallingJr.
Article

Summary

Comparisons of trends of global industrial productivity, Northern Hemispheric and United States annual mean temperatures, U.S. annual and summer mean maximum and mean minimum temperatures, and U.S. cloud cover suggest that the net result of the CO2/trace gas greenhouse effect and certain biologically-modulated negative feedbacks related to cloud characteristics may be a moderate increase in nighttime minimum temperatures with no change in daytime maximum values. Such a response, if verified by further studies, would likely be desirable, for it would reduce low temperature stresses on biological and mechanical systems, significantly amplify many of the positive botanical effects of atmospheric CO2 enrichment, and produce few, if any, deleterious climatic effects. In a word, it may well be beneficial.

Keywords

Minimum Temperature Cloud Cover Temperature Response Temperature Stress Climatic Effect 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. Charlson, R. J., Lovelock, J. E., Andreae, M. O., Warren, S. G., 1987: Oceanic phytoplankton, atmospheric surfur, cloud albedo and climate.Nature,326, 655–661.Google Scholar
  2. Henderson-Sellers, A., 1986a: Cloud cover changes in a warmer Europe.Climatic Change,8, 25–52.Google Scholar
  3. Henderson-Sellers, A., 1986b: Increasing cloud in a warming world.Climatic Change,9, 267–309.Google Scholar
  4. Henderson-Sellers, A., 1989: North American total cloud amount variation this century.Global Planet. Change,1, 175–194.Google Scholar
  5. Idso, S. B., 1989:Carbon Dioxide and Global Change: Earth in Transition. Tempe, Arizona: IBR Press.Google Scholar
  6. Idso, S. B., 1990: A role for soil microbes in moderating the CO2 greenhouse effect?Soil Science,149, 179–180.Google Scholar
  7. Idso, S. B., Kimball, B. A., 1989: Growth response of carrot and radish to atmospheric CO2 enrichment.Environ. Exp. Bot.,29, 135–139.Google Scholar
  8. Idso, S. B., Kimball, B. A., Anderson, M. G., Mauney, J. R., 1987: Effects of atmospheric CO2 enrichment on plant growth: the interactive role of air temperature.Agric. Ecosys. Environ.,20, 1–10.Google Scholar
  9. Jones, P. D., Raper, S. C. B., Bradley, R. S., Diaz, H. F., Kelly, P. M., Wigley, T. M. L., 1986: Northern hemispheric surface air temperature variations: 1851–1984.J. Climate Appl. Meteor.,25, 161–179.Google Scholar
  10. Karl, T. R., Kukla, G., Gavin, J., 1984: Decreasing diurnal temperature range in the United States and Canada, 1941 through 1980.J. Climate Appl. Meteor.,23, 1489–1504.Google Scholar
  11. Karl, T. R., Kukla, G., Gavin, J., 1986: Relationship between decreased temperature range and precipitation trends in the United States and Canada, 1941–1980.J. Climate Appl. Meteor.,25, 1878–1886.Google Scholar
  12. Karl, T. R., Kukla, G., Gavin J., 1987: Recent temperature changes during overcast and clear skies in the United Stated.J. Climate Appl. Meteor.,26, 698–711.Google Scholar
  13. Karl, T. R., Steurer, P. M., 1990: Increased cloudiness in the United States during the first half of the twentieth century: fact or fiction?Geophys. Res. Lett.,17, 1925–1928.Google Scholar
  14. Karl, T. R., Williams, C. N., Jr., 1987: An approach to adjusting climatological time series for discontinuous inhomogeneities.J. Climate Appl. Meteor.,27, 1744–1763.Google Scholar
  15. MacCracken, M. C., Luther, F. M. (Eds.), 1985:Projecting the Climatic Effects of Increasing Carbon Dioxide. Washington, D.C.: U.S. Department of Energy.Google Scholar
  16. Mayewski, P. A., Lyons, W. B., Spencer, M. J., Twickler, M. S., Buck, C. F., Whitlow, S., 1990: An ice-core record of atmospheric response to anthropogenic sulfate and nitrate.Nature,346, 554–556.Google Scholar
  17. National Research Council, U.S., 1983:Changing Climate. Washington, D.C.: National Academy Press.Google Scholar
  18. Plantico, M. S., Karl, T. R., Kukla, G., Gavin, J., 1990: Is recent climate change across the United States related to rising levels of anthropogenic greenhouse gases?J. Geophys. Res.,95, 16617–16637.Google Scholar
  19. Quinlan, F. T., Karl, T. R., Williams, C. N., Jr., 1987: United States historical climatology network (HCN) serial temperature and precipitation data, NDP-019. Oak Ridge, Tennessee: Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory.Google Scholar
  20. Ramanathan, V., Barkstrom, B. R., Harrison, E. F., 1989a: Climate and the Earth's radiation budget.Physics Today,42(5, 22–32.Google Scholar
  21. Ramanathan, V., Cess, R. D., Harrison, E. F., Minnis, P., Barkstrom, B. R., Ahmad, E., Hartman, D., 1989b: Cloud-radiative forcing and climate: results from the earth radiation budget experiment.Science 243, 57–63.Google Scholar
  22. Rotty, R. M., Masters, C. D., 1985: Carbon dioxide from fossil fuel combustion: trends, resources, and technological implications. In: Trabalka J.R. (ed.),Atmospheric Carbon Dioxide and the Global Carbon Cycle. Washington, D.C.: U.S. Department of Energy, 63–80.Google Scholar
  23. Schwartz, S. E., 1988: Are global cloud albedo and climate controlled by marine phytoplankton?Nature,336, 441–445.Google Scholar
  24. Seaver, W. L., Lee, J. E., 1987: A statistical examination of sky cover changes in the contiguous United States.J. Climate Appl. Meteor.,26, 88–95.Google Scholar
  25. Slama, C. C., 1980:Manual of Photogrammetry, 4th Ed. Falls Church, Virginia: Amer. Soc. Photogrammetry.Google Scholar
  26. Staubes, R., Georgii, H.-W., Ockelmann, G., 1989: Flux of COS, DMS and CS2 from various soils in Germany.Tellus,41B, 305–313.Google Scholar
  27. Warren, S. G., Hahn, C. J., London, J., Chervin, R. M., Jenne, R., 1988: Global Distribution of Total Cloud Cover and Cloud Type Amounts over the Ocean. Boulder, Colorado: U. S. Depart. Energy and Nat. Center Atmos. Res.Google Scholar

Copyright information

© Springer-Verlag 1991

Authors and Affiliations

  • S. B. Idso
    • 1
  • R. C. BallingJr.
    • 1
  1. 1.Laboratory of Climatology and Department of GeographyArizona State UniversityTempeUSA

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