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The influences of El Nin o-Southern Oscillation (ENSO) events in the tropical Pacific on interannual variability of the coupled ocean-atmosphere systems in the North Pacific and North Atlantic have been studied using a suite of experiments with a rhomboidal 30-wavenumber, 14-layer general circulation model (GCM). Observed month-to-month fluctuations of the sea surface temperature (SST) in the tropical Pacific during the 1950-95 period were prescribed as the lower boundary condition for the GCM. The SST conditions outside of the tropical Pacific were predicted by a simple ocean mixed layer model with a constant depth. Four independent integrations under this ''Tropical Ocean-Global Atmosphere-Mixed Layer (TOGA-ML)'' scenario were conducted.
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Lau et al. (2001) studied this question.
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