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A 1000-year climate simulation is run with the ocean-atmosphere coupled model developed at the Institute Pierre-&#13; Simon Laplace (IPSL, Paris). No flux adjustment is used. The drift of the model is analyzed in terms of the seasurface&#13; temperature and deep ocean temperature. When the model's own equilibrium is reached, it is found that&#13; the Antarctic bottom water production experiences large-amplitude variation, oscillating between strong and weak&#13; episodes. This can yield oceanic temperature variation in the Southern Hemisphere and for the global mean

A 1000-year simulation with the IPSL ocean-atmosphere coupled model