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Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article

Classified by OpenAIRE into

arxiv: Physics::Atmospheric and Oceanic Physics
A seasonal, zonally averaged, climate model is developed using a hypothetical meridional circulation, which reproduces the atmospheric dynamical heating of a two-level general circulation model. In order to simulate the seasonal temperature cycle, prognostic equations for the land and ocean temperatures are included in the model. The horizontal heat transport in the ocean is modelled as ordinary diffusion. Small-scale vertical transport of sensible and latent heat is described by simple linear terms. For the long-wave radiation calculations, a simple but efficient emissivity approximation scheme is developed. The short-wave radiation treatment is based on an early version of the Mintz-Arakawa general circulation model. The meridional and seasonal variation of the surface temperature as well as the temperature at the two tropospheric levels are simulated quite well by the model. Concerning surface albedo and planetary albedo, the model gives results which are in good agreement with observed values. Radiative fluxes of the model also compare well with observed values. The sensitivity of the model to changes in incoming solar radiation and carbon dioxide content is in accordance with results obtained from other models. The model, with variation of the Earth's orbital parameters, has also been used for some preliminary experiments.DOI: 10.1111/j.2153-3490.1982.tb01840.x
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    • Berger, A. L. 1978. Long-term variation of daily insolation and quaternary climatic changes. J. Amos. Sci. 35,2362-2361.
    • Eliasen, E. 1982. Climate modeling using an equivalent meridional circulation. Tellus 34,228-244.
    • Eliasen, E., Machenhauer, B. and Rasmussen, E. 1970. On a numerical method for integration of the hydrodynamical equations with a spectral representation of the horizontal fields. Report No. 2, Institute of Theoretical Meteorology, University of Copenhagen, Denmark.
    • Ghil, M. and Bhattachary, K. 1979. An energybalance model of glaciation cycles. GARP Publications Series No. 22, 886-916, WMO/ICSU, Geneva, Switzerland.
    • Hays, J. D., Imbrie, J. and Shackleton, N. J. 1976. Variations in the Earth's orbit: pacemaker of the ice ages. Science 194, 1121-1 132.
    • Katayama, A. 1972. A simplified scheme for computing radiative transfer in the troposphere. Technical report No. 6. Department of Meterology, University of California, Los Angeles, USA.
    • Lacis, A. A. and Hansen, J. E. 1974. A parameterization for the absorption of solar radiation in the Earth's atmosphere. J. Atmos. Sci. 31, 118-133.
    • Langlois, W. E. and Kwok, C. W. 1969. Description of the Mintz-Arakawa numerical general circulation model. Technical report No. 3. Department of Meterology, University of California, L o s Angeles, USA.
    • Manabe, S. and Muller, F. 1961. On the radiative equilibrium and heat balance of the atmosphere. Mon. Wea.Rev. 89,503-552.
    • Manabe, S . and Stouffer, S. J. 1979. A C0,-climate sensitivity study with a mathematical model of the global climate. Nature 282,491-493.
    • Manabe, S . and Strickler, R. F. 1964. Thermal equilibrium of the atmosphere with a convective adjustment. J. Atmos. Sci.21, 361-385.
    • Robert, A. 1966. The integration of a low order spectral form of the primitive meteorological equations. J. Ueteorol. SOCJ.apan 44,231-245.
    • Robock, A. 1979. The performance of a seasonal global climate model. GARP Publications Series No. 22, 766-799, WMO/ICSU, Geneva, Switzerland.
    • Rodgers, C. D. 1967. The radiative heat budget of the troposphere and lower stratosphere. Rept. No. A2, Planetary Circulations Project, Dept of Meteorology, Massachusetts Institute of Technology, Cambridge, U.S.A., 99 pp.
    • Sasamori, T. 1968. The radiative cooling calculation for application to general circulation experiments.J . Appl. Ueteorol. 7,721-729.
    • Schlesinger, M. E. and Gates, L. W. 1979. Performance of the Oregon State University two-level atmospheric general circulation model. GARP Publication Series No. 22,139-206, WMO/ICSU, Geneva, Switzerland.
    • Schneider, S. H. 1975. On the carbon dioxide-climate confusion. J. Atmos. Sci. 32,2060-2066.
    • Sellers, W. D. 1965. Physical climatology. Chicago and London: The University of Chicago Press.
    • Sellers, W. D. 1973. A new global climate model. J. Appl. Meteorol. 12,241-254.
    • Thompson, S. L. 1979. Development of a seasonallyverified planetary albedo parameterization for zonal energy balance climate models. GARP Publication Series No. 22, 1002-1023, WMO/ICSU, Geneva, Switzerland.
    • Thompson, S. L. and Schneider, S. H. 1979. A seasonal zonal energy balance climate model with an interactive lower layer. J. Geophys. Res. 84, 2401- 2414.
    • Warren, S. G. and Schneider, S. H. 1979. Seasonal simulations as a test for uncertainties in the parameterizations of a Budyko-Sellers zonal climate model. J. Atmos. Sci. 36, 1377-1391.
    • Wetherald, R. T. and Manabe, S. 1975. The effect of changing the solar constant on the climate of a general circulation model. J. Amos. Sci. 32, 2044- 2059.
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