ausblenden:
Schlagwörter:
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Zusammenfassung:
We describe results of an experiment in which the Hamburg Large-Scale-
Geostrophic ocean general circulation model was driven by a spatially corre—
lated white noise fresh water flux superimposed on the climatological fluxes.
In addition to the red noise character of the oceanic response, the model
exhibits pronounced variability in a frequency band around 320 years. The
centers of action of this oscillation are the Southern Ocean and the Atlantic.