[1] World Meteorological Orgartization，1975:The physical basis of climate and climate modeling, CARP Publications Series,No. 16, 265pp
[2] Simmons, A. J. and L. bengtsson, 1984:atmospheric general model: their design and use for climate studies, in The Global Climate, J. T. Houghton, Ed.，Cambridge University Press, Cambridge, 37-62
[3] Hunt, B. G. 1979: The effects of past variations of the Earthy’s rotation rate on climate, Nature, 281, 188-191
[4] Kutzbach, J. E.，1985:Modeling of paleoclimate, in Advances in Geophysics, Vol. 28, Part A, S. Manabe Ed.，Academic Press, Inc.159-198
[5] Walker, J. C.，1982:Climate factors on the Archean Earth, Paleogeogr.Paleaclimatol.Paleoecol.，40,1-11
[6] Barron, E. J. and W. M. Washington, 1982:Cretaceous climate:a comparison of atmospheric simulations with the geologic record, Paleogeogr.paleoclimatol. Paleoecol.，40, 103-133
[7] Barron, E. J. and W. M. Washington, 1984:The role of geographic variables in explaining paleocliafates:results from Cretaceous climate model sensitivity studies, J. Geophys. Rea.，89, 1267-1279
[8] Ruddiman, W. F. et al.，1989:Late Cenozoic uplift in southern Asia and the American west: rationale for atmospheric general circulation modeling experiments, J. Geophys. Res，99, 379-392
[9] Manabe, s. and K. Terpstra, 1974:The effects of mountains on the general circulation of the atmosphere as identified by numerical experiments, J. Atmos. Sci, 31，3-42
[10] Hahn, D. G. and S. Manabe, 1975:The role of mountains in the south Asian monsoon ciretlation, J. Atmos.Sci,32,1515-1541
[11] Kutzbach, J. E.，et al.，1989:Sensitivity of climate to late Cenozoic uplift in southern Asia and the American west:Numerical Experiments, J. Geophys. Res.，99, 393-408
[12] Ruddiman, W.F.et al.，1989:Forcing of Late Cenozoic northern hemispheric climate by plateau uplift in southern Asia and the American west, J. Geophys. Res.，94,409-927
[13] CLIMAP Project Members, 1976:The surface of the Ice-Age Earth, Science, 191,1131-1136
[14] CLIMAP Project Members，1981:Seasonal reconstructions of the Earthy s surface at the last glacial maximum, Geol. Soc Am.Map Chart Ser,MC-36
[15] Gates, W. L.，1976:The numerical simulation of the Ice Age climate with a global general circulation model, J. Atmas.Sci, 33, 1844-1873
[16] Gates, W. L.，1976: modeling the Ice Age climate, Science,191，1138-1144
[17] Manabe, S. and Hahn，D. G，1977:Simulation of the tropical calimate吐an Ice Age, J. Geophys. Ras.，82, 3889-3911
[18] Manabe, S. and A. J. Broccoli, 1985: The influence of continental ice sheets on the climate of an Ice Age, J.  Geophys.Res.，90, 2167-2190
[19] Manabe, S. and A. J. Broccoli, 1985:A comparison of climate model sensitivity with data from the last glacial maximum,J. Atmos. Sci, 92,2643-2651
[20] Kutzbach, J. E. and P. J. Guetter, 1986:The influence of changing obital parameters and surface boundary conditions on climate simulations for the past 18000 years, J. Atmos. Sci, 43, 1726-1759
[21] Rind, D.，1987:Components of the Ice Age circulation, J. Geophys. Res.，92, 4241-4281
[22] Cook, K, H. and I. M. Held, 1988:Stationary waves of the Ice Age climate, J. Climate, 1，807-819
[23] Hyde, W. T. et al.，1989:comparison of GCM and energy balance model simulation of seasonal temperature changes over the past 18000 years, J, Climate, 2, 864-887
[24] COHMAP Project Members, 1985:Reconstructions of climate and comparison with general circulation model simulations for 18000 yr to present at 3000yr interval, Climatic Change, 10, 224-251
[25] COHMAP Project Members, 1988:Climatic changes of the last 18000 years:observations and mode(simulation，Science,241, 1043-1052
[26] Kutzbach, J. E.，1981:Monsoon climate of the early Holocene: climatic experiment using the Earthy’s orbital parameters for 9000 year ago, Science, 214, 59-61
[27] Kutzbach, J. E. and Otto-BLiesner, B. L.，1982:The sensitivity of the African-Asian Monsoons(climate to orbital parameter changes for 9000 years BP in a low-resolution general circulation model，J. Atmas. Sci, 39, 1177-1188
[28] Kutzbach, J. E. and P. J. Guetter, 1984:Sensitivity of late-glacial and Holocene climates to the combined effects of orbital parameter changes and law boundary condition change, "Snapshot" simulations with a general circulation model for 18, 9,and 6Ka BP, Ann. Glaciol, 5, 85-87
[29] Washington W. M. and C. L. Parkinson, 1986:An introduction to three-dimensional climate modelling, Oxford University Press, Oxford New York,259-269
[30] Suarez, M. J. and I. M. Held, 1979:The sensitivity of an energy balance clmate model to variations in the orbital parameters,J. Geophys. Res，89, 4825-4836
[31] Manabe, S. and R. J. Stouffer, 1980:Sensitivity of a global climate model to an increase of CO₂ concentration in the atmosphere, J. Geophys. Res.，85, 5529-5554
[32] Gates, W. L. and K. H. Cook, 1980:Preminary analysis of experiments on the climatic effects of increased CO₂ with the OSU atmospheric genegal circulation model, Report No. 14, Climatic Research Institute, Oregon State University, Corvallis,Oregon, 102pp
[33] Berner R. A.，et al.，1983:The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the last 100 million years, Am. J. Sci，283, 641-683
[34] Manabe, S. and K. Bryan, 1985:CO₂-induced change in a coupled ocean-atmosphere model and its paleoclimatic implication , J. Geophys. Res.，90, 11689-11707
[35] Meehl, D. A.et al.，1986:Tropical response to increased CO₂ in a GCM with a simple mixed layer ocean，Mon.  Wea. Rev.，119, 667-674
[36] Broccoli, A. J. and S. manabe, 1987: The influence of continental ice, atmospheric CO₂, and land albedo on climate of the last glacial maximum, Climate Dynamics, 1, 87-99
[37] Rind, D. et al.，1987:Chemistry of the global troposphere:fluoro-carbons as tracers of air motion, 92, 6579-6582
[38] Zhao, Zong-ci and W. W. Kellogg, 1988, Sensitivity of soil moisture to doubling of carbon dioxide in climate model experiments, J. Climate, 1, 367-378
[39] Hunt, B. J.，1982:Large-scale atmospheric models as an experimental tool, Aust. Met. Mag.，30,49-55
[40] 曾庆存，大气科学中的数值摸拟研究——理论和实用相结合，大气科学，9,  186-194