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Projected Twenty-First-Century Changes in Temperature, Precipitation, and Snow Cover over North America in CCSM4
Publisher: American Meteorological Society
Abstract: esults from a suite of ensembles of twenty-first-century climate projections made using the Community Climate System Model, version 4 (CCSM4) are analyzed to document model bias and to explore possible future changes in ...
Transit-Time Distributions in a Global Ocean Model
Publisher: American Meteorological Society
Abstract: Results from a simulation of the ocean ?transit-time distribution? (?TTD?) for global and regional ocean surface boundary conditions are presented based on a 5000-yr integration using the Parallel Ocean Program ocean general ...
Twentieth-Century Oceanic Carbon Uptake and Storage in CESM1(BGC)
Publisher: American Meteorological Society
Abstract: cean carbon uptake and storage simulated by the Community Earth System Model, version 1?Biogeochemistry [CESM1(BGC)], is described and compared to observations. Fully coupled and ocean-ice configurations are examined; both ...
Subtropical Mode Water Variability in a Climatologically Forced Model in the Northwestern Pacific Ocean
Publisher: American Meteorological Society
Abstract: climatologically forced high-resolution model is used to examine variability of subtropical mode water (STMW) in the northwestern Pacific Ocean. Despite the use of annually repeating atmospheric forcing, significant ...
True to Milankovitch: Glacial Inception in the New Community Climate System Model
Publisher: American Meteorological Society
Abstract: he equilibrium solution of a fully coupled general circulation model with present-day orbital forcing is compared to the solution of the same model with the orbital forcing from 115 000 years ago. The difference in snow ...
The CCSM4 Ocean Component
Publisher: American Meteorological Society
Abstract: he ocean component of the Community Climate System Model version 4 (CCSM4) is described, and its solutions from the twentieth-century (20C) simulations are documented in comparison with observations and those of CCSM3. The ...