pure and applied geophysics

, Volume 113, Issue 1, pp 331–353 | Cite as

The short-term influence of various concentrations of atmospheric carbon dioxide on the temperature profile in the boundary layer

  • Wilford G. Zdunkowski
  • Jan Paegle
  • Falko K. Fye
Article

Summary

A radiative-conductive model is constructed to study short-term effects of various carbon dioxide concentrations on the atmospheric boundary layer for different seasons. The distribution of the exchange coefficient is modeled with the aid of the KEYPS formula. Infrared radiation calculations are carried out by means of the emissivity method and by assuming that water vapor and carbon dioxide are the only radiatively active gases. Global radiation is computed by specification of Linke's turbidity factor.

It is found that doubling the carbon dioxide concentration increases the temperature near the ground by approximately one-half of one degree if clouds are absent. A sevenfold increase of the present normal carbon dioxide concentration increases the temperature near the ground by approximately one degree. Temperature profiles resulting from presently observed carbon dioxide concentration and convective cloudiness of 50% or less are compared with those resulting from doubled carbon dioxide concentrations and the same amounts of cloud cover. Again, it is found that a doubling of carbon dioxide increases the temperature in the lower boundary layer by about one-half of one degree.

The present results are obtained on the basis of fixed temperature boundary conditions as contrasted to the study ofManabe andWetherald (1967). Howeve, the conclusions are not addressed to global climate change, but to the distribution of the temperature of the air layer near the ground.

References

  1. Davis, P. A. (1961), A Re-examination of the Heat Budget of the Troposphere and Lower Stratosphere. Sci. Rpt. No. 3, AF 19(604)-6146, New York University, p. 18.Google Scholar
  2. Feussner, K., andDubois, P. (1930),Trübungsfaktor, precipitable water, Staub., Gerlands Beitr. Geophys.27, 132–175.Google Scholar
  3. Geiger, R.,The Climate Near the Ground (Harvard Univ. Press, Cambridge, Mass. 1966), Chap. 2.Google Scholar
  4. Johnson, J. C.,Physical Meteorology (Tech. Press of M.I.T. and John Wiley and Son, New York 1954), p. 156.Google Scholar
  5. Kaplan, L. D. (1960),The influence of carbon dioxide variations on the atmospheric heat balance, Tellus12, 204–208.Google Scholar
  6. Kondratiev, K. Y., andNiilisk, H. I. (1960),On the question of carbon dioxide heat radiation in the atmosphere, Geofis. Pura. E. Applicata.46, 216–230.Google Scholar
  7. Manabe, S., andMöller, F. (1961).On the radiative equilibrium and heat balance of the atmosphere, Mon. Wea. Rev.89, 503–532.Google Scholar
  8. Manabe, S., andWetherald, R. T. (1967),Thermal equilibrium of the atmosphere with a given distribution of relative humidity, J. Atmos. Sci.24, 241–259.Google Scholar
  9. McDonald, J. E. (1960),Direct absorption of solar radiaton by atmospheric water vapor, J. Meteor.17, 319–328.Google Scholar
  10. Möller, F. (1955),Strahlungsvorgänge in Bodennähe, Z. Meteor.9, 47–55.Google Scholar
  11. Möller, F. (1963),On the influence of changes in the CO 2 concentration in air on the radiation balance of earth's surface and on the climate. J. Geophys. Res.68, 3877–3885.Google Scholar
  12. Newell, R. E., andDopplick, T. G. (1970),The effect of changing CO 2 concentration on radiative heating rates. J. Appl. Meteor.9, 958–959.Google Scholar
  13. Newell, R. E., Herman, G. F., Dopplick, T. G., andBoer, G. J. (1972),The effect of changing CO 2 concentration on radiative heating rates: Further comments. J. Appl. Meteor.11, 864–867.Google Scholar
  14. Philipps, H. (1962),Zur Theorie des Tagesganges der Temperatur in der bodennahen Atmosphäre und in ihrer Unterlage, Z. Meteorol.16, 5.Google Scholar
  15. Pilie, R. J., Eadie, W. J., Mack, E. J., Rogers, C. W., andKocmond, W. C. (1972), Project Fog Drops Part I—Investigation of Warm Fog Drops. Seventh Annual Summary Report, NASW-2126, pp. 106–109.Google Scholar
  16. Plass, G. N. (1959),Carbon dioxide and climate, Scientific American 201, 41–47.Google Scholar
  17. Plass, G. N. (1961),The influence of infrared absoorptive molecules on the climate. Annals of the N.Y. Acad. of Sci. 61–71.Google Scholar
  18. Rasool, S. J., andSchneider, S. H. (1971),Atmospheric carbon dioxide and aerosols: Effects of large increases on global climate. Science173, 138–141.Google Scholar
  19. Richtmeyer, R. D., andMorton, K. W.,Difference Methods for Initial Value Problems (Interscience Publishers, New York, 1967), p. 176.Google Scholar
  20. Rodgers, C. D. (1967),The use of emissivity in atmospheric radiation calculations, Quart. J. Roy. Meteor. Soc.93, 43–54.Google Scholar
  21. Sasamori, T. (1959),The temperature effect on the absorption of 15 microns carbon-dioxide band, Sci. Rep. Tohoku Univ., Ser. 511, No. 3.Google Scholar
  22. Valley, S. A., ed.Handbook of Geophysics and Space Environments (McGraw Hill, New York 1965), Chaps. 2, 3.Google Scholar
  23. Yamamoto, G., andOnishi, G. (1949),Absorption coefficient of water vapor in the far infrared region, Sci. Rep. Tohoku Univ., Ser. 51, No. 1.Google Scholar
  24. Yamamoto, G., andSasamori, T. (1958),Calculation of the absorption of the 15 micron carbondioxide band, Sci. Rep. Tohoku Univ., Ser. 510, No. 2.Google Scholar
  25. Zdunkowski, W. G., andJohnson, F. C. (1965),Infrared flux divergence calculations with newly constructed radiation tables. J. Appl. Meteor.4, 371–377.Google Scholar
  26. Zdunkowski, W. G., andMcQuagé, N. D. (1972),The effect of haze on a radiative, conductive, dynamic model profile of the lower atmosphere Tellus,25, 237–254.Google Scholar

Copyright information

© Birkhäuser Verlag 1975

Authors and Affiliations

  • Wilford G. Zdunkowski
    • 1
  • Jan Paegle
    • 1
  • Falko K. Fye
    • 1
  1. 1.Department of MeteorologyUniversity of UtahSalt Lake City

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