A seasonal global climate model with an equivalent meridional atmospheric circulation

References

• Berger, A. L. 1978. Long-term variation of daily insolation and quaternary climatic changes. J. Atmos. Sci. 35, 2362–2367.
   Google Scholar
• Eliasen, E. 1982. Climate modeling using an equivalent meridional circulation. Tellus 34, 228–244.
   Google Scholar
• Eliasen, E., Machenhauer, B. and Rasmussen, E. 1970. On a numerical method for integration of the hydro-dynamical equations with a spectral representation of the horizontal fields. Report No. 2, Institute of Theoretical Meteorology, University of Copenhagen, Denmark.
   Google Scholar
• Ghil, M. and Bhattachary, K. 1979. An energy-balance model of glaciation cycles. GARP Publica-tions Series No. 22, 886-916, WMO/ICSU, Geneva, Switzerland.
   Google Scholar
• Hays, J. D., Imbrie, J. and Shackleton, N. J. 1976. Variations in the Earth's orbit: pacemaker of the ice ages. Science 194, 1121–1132.
   PubMed Web of Science ®Google Scholar
• 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.
   Google Scholar
• 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.
   Web of Science ®Google Scholar
• 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, Los Angeles, USA.
   Google Scholar
• Manabe, S. and Muller, F. 1961. On the radiative equilibrium and heat balance of the atmosphere. Mon. Wea. Rev. 89, 503–552.
   Google Scholar
• Manabe, S. and Stouffer, S. J. 1979. A CO2-climate sensitivity study with a mathematical model of the global climate. Nature 282, 491–493.
   Web of Science ®Google Scholar
• Manabe, S. and Strickler, R. F. 1964. Thermal equilibrium of the atmosphere with a convective adjustment. J. Atmos. Sci. 21, 361–385.
   Web of Science ®Google Scholar
• Robert, A. 1966. The integration of a low order spectral form of the primitive meteorological equations. J. MeteoroL Soc. Japan 44,237–245.
   Google Scholar
• Robock, A. 1979. The performance of a seasonal global climate model. GARP Publications Series No. 22, 766-799, WMO/ICSU, Geneva, Switzerland.
   Google Scholar
• 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.
   Google Scholar
• Sasamori, T. 1968. The radiative cooling calculation for application to general circulation experiments. J. Appl. MeteoroL 7, 721–729.
   Google Scholar
• 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.
   Google Scholar
• Schneider, S. H. 1975. On the carbon dioxide-climate confusion. J. Atmos. Sci. 32, 2060–2066.
   Web of Science ®Google Scholar
• Sellers, W. D. 1965. Physical climatology. Chicago and London: The University of Chicago Press.
   Google Scholar
• Sellers, W. D. 1973. A new global climate model. J. Appl. Meteorol. 12,241–254.
   Google Scholar
• Thompson, S. L. 1979. Development of a seasonally-verified planetary albedo parameterization for zonal energy balance climate models. GARP Publication Series No. 22, 1002-1023, WMO/ICSU, Geneva, Switzerland.
   Google Scholar
• 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.
   Web of Science ®Google Scholar
• 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.
   Google Scholar
• Wetherald, R. T. and Manabe, S. 1975. The effect of changing the solar constant on the climate of a general circulation model. J. Atmos. Sci. 32, 2044–2059.
   Web of Science ®Google Scholar