Articles

CLIMATE MODEL AND PALEOCLIMATE SIMULATION

Expand
  • 1.Department of Geograyhy, Sichuan Teachers University;2.Lanzhou Institude of Plateau Atmospheric Physics, Academia Sinica

Received date: 1990-10-11

  Online published: 1991-03-01

Abstract

The definition and development of climate model is summarized in this paper. Several types of climate model which is used for paleoclimate simulation is introduced. The usage of climate model in the research of paleoclimate and main achivements in it is descripted. The wide vista of the climate model in the area of paleoclimate research is explained.

Cite this article

Jiang Zhaoli, Liu Xiaodong . CLIMATE MODEL AND PALEOCLIMATE SIMULATION[J]. Advances in Earth Science, 1991 , 6(2) : 19 -24 . DOI: 10.11867/j.issn.1001-8166.1991.02.0019

References

[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

Outlines

/