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Atmospheric general circulation model

Ocean-Atmosphere Interactions. To determine how the ocean responds to a C02-induced climate forcing, it will be necessary to develop a combined ocean and atmospheric general circulation model. It will take 10-20 years to develop a model with appropriate chemistry and biology to the level of confidence necessary to make valid projections. In the interim, two approaches can be pursued in parallel with this model development. [Pg.408]

Bonan, G. B. (1995a). Land-atmosphere CO2 exchange simulated by a land surface process model coupled to an atmospheric general circulation model, j. Geophys. Res. 100,2817-2831. [Pg.310]

Dorman, J. L. and Sellers, P. J. (1989). A global climatology of albedo, roughness length and stomatal resistance for atmospheric general circulation models as represented by the simple biosphere model (SiB), /. Appl. Meteorol. 28, 833-855. [Pg.312]

Roeckner, E., Arpe, K., Bengtsson, L., Christoph, M., Claussen, M., Dumenil, L., Esch, M., Giorgetta, M., Schlese, U., and Schulzweida U. (1996) The atmospheric general circulation model ECHAM-4 Model description and simulation of present-day climate, Rep. 218, Max-Planck-Institute for Meteorology, Hamburg, Germany. [Pg.42]

Roeckner E. Arpe K. Bengtsson L. Christoph M. Claussen M. Dumenil L. Esch M. Giorgetta M. Schlese U. and Schulzweida U. (1996). The Atmospheric General Circulation Model ECHAM-4 Model Description and Simulation of Present-Day Climate. Max-Planck-Institut fur Meteorologie Report No. 218, Hamburg, Germany, 90 pp. [Pg.549]

The global chemistry transport model (CTM) part is based on the CHASER model, which is based on CCSR/NIES/FRCGC atmospheric general circulation model (AGCM) version 5.7b. The basic features of the model have been already described in Sect. 2. The regional CTM part is based on WRF/Chem (Grell et al. 2005). The databases used are the following ... [Pg.190]

Numaguti A, Takahashi M, Nakajima T, Sumi A (1997) Development of CCSR/NIES atmospheric general circulation model, no. 3 in CGER s Supercomput. Monogr. Rep., CGER, Tsukuba, Ibaraki, pp 1 8... [Pg.193]

Russell, G., and J. Miller. 1990. "Global river runoff calculated from a global atmospheric general circulation model." Journal of Hydrology 117 241-254. [Pg.40]

Andersen U. (1997) Modeling the stable water isotopes in precipitation using the LMD.5.3 atmospheric general circulation model. PhD Thesis, NBIAPG, University of Copenhagen, 100pp. [Pg.2151]

Hoffmann G., Werner M., and Heimann M. (1998) Water isotope module of the ECHAM atmospheric general circulation model a study on time scales from days to several years. J. Geophys. Res. 103, 16871-16896. [Pg.2153]

Hoffmann G., Masson V., and Jouzel J. (2000) Stable water isotopes in atmospheric general circulation models. Hydrol. Process. 14, 1385-1406. [Pg.2153]

Joussaume S. and Jouzel J. (1993) Paleoclimatic tracers an investigation using an atmospheric General Circulation Model under ice age conditions 2. Water isotopes. J. Geophys. Res. 98, 2807-2830. [Pg.2153]

The snow collected 33 km from Dumont d Urville was found to contain a ° Pb/ ° Pb ratio significantly lower than the background showing that it was polluted by base emissions, probably from leaded fuel which was purchased in Australia ( Pb/ ° Pb as low as 1.07). An alternative mechanism for lowering the ratio in the coastal snow was the transfer of Australian emissions through the atmosphere which was consistent with atmospheric general circulation models (54). Snow at the South Pole was also polluted by emissions from the Amundsen-Scott base, located only 7.3 km away. [Pg.99]

Cess R.D., ZhangM.-H., Potter G.L., Barker H.W., Coleman R.A. 25 others (1993) Uncertainties in carbon dioxide radiative forcing in atmospheric general circulation models. Science 262, 1252—5. [Pg.330]

Schlesinger, M.E., and Y. Mintz, Numerical simulation of ozone production, transport and distribution with a global atmospheric general circulation model. J Atmos Sci 36, 1325, 1979. [Pg.147]

Cubasch, U., Voss, R., Hegerl, G. C., Waszkewitz, J., and Crowley, T. J. (1997). Simulatkrn of the influence of solar radiation variations on the global climate with an ocean-atmosphere general circulation model. Climate Dynamics 13, 757-767. [Pg.28]

Lorenz, S., Grieger, B., Helbig, P, and Herterich, K. (1996). Investigating the sensitivity of the Atmospheric General Circulation Model ECHAM 3 to paleoclimatic boundary conditions. Geol. Rundschau 85, 513-524. [Pg.85]

Vettorctti, G., Peltier, W. R., and McFarlane, N. A. (1998). Simulations of mid-Holocene climate using an atmospheric general circulation model. / Climate 11, 2607-2627. [Pg.86]

Hydrodynamic models of the atmosphere on a grid or spectral resolution that determine the surface pressure and the vertical distributions of velocity, temperature, density, and water vapor as functions of time from the mass conservation and hydrostatic laws, the first law of thermodynamics, Newton s second law of motion, the equation of state, and the conservation law for water vapor. Abbreviated as GCM. Atmospheric general circulation models are abbreviated AGCM, while oceanic general circulation models are abbreviated OGCM. geomorphology... [Pg.183]


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Atmosphere general circulation

Atmospheric Oceanic General Circulation Models

Atmospheric circulation models

Atmospheric general circulation model AGCM)

Atmospheric models

Circulation model

Circulation, atmospheric

Circulation, general

General circulation models

Generalization model

Model, generalized

Modeling atmospheric

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