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Accelerating the Convergence to Equilibrium of Ocean-Climate Models
Ocean-Climate Models Accelerating Convergence
2009/1/20
Solutions corresponding to climatic equilibrium are usually obtained from atmospheric general circulation models by extended numerical integration with respect to time. Because the ocean contains a mu...
Computational Efficiency and Accuracy of Methods for Asynchronously Coupling Atmosphere-Ocean Climate Models. Part II:Testing with a Seasonal Cycle
atmosphere–ocean general circulation models Seasonal Cycle
2009/1/10
The asynchronous coupling schemes used in the seasonal, coupled atmosphere–ocean general circulation models (A/O GCMs) of Manabe et al. 1979 and Washington et al. 1980 are tested in the seasonal, coup...
Computational Efficiency and Accuracy of Methods for Asynchronously Coupling Atmosphere–Ocean Climate Models. Part I:Testing with a Mean Annual Model
Computational Efficiency Atmosphere–Ocean Climate Mean Annual Model
2009/1/10
Using the mean annual, globally-averaged, coupled atmosphere–ocean energy balance model of Harvey and Schneider, the effect on the transient climate response to a step function solar constant increase...
Hindcasting Ocean Climate Variability Using Time-Dependent Surface Data to Drive a Model:An Idealized Study
sea surface temperature sea surface salinity Idealized Study
2008/12/12
This paper investigates the hindcasting of interdecadal climate events using an ocean circulation model driven by different combinations of time-varying surface flux, sea surface temperature (SST), an...
Antarctic Bottom Water Formation and Deep-Water Chlorofluorocarbon Distributions in a Global Ocean Climate Model
Antarctic Bottom Water Deep-Water Chlorofluorocarbon Distributions Global Ocean
2008/6/9
The ocean distributions of chlorofluorocarbons (CFCs) have been measured extensively in order to determine the mechanisms, rates, and pathways associated with thermohaline deep-water formation. Model ...