We review numerical modeling studies of long- period oscillations which are Inherent in ice-sheet physics. Such studies are relevant to the 100 ka component found in proxy ice volume time series. We show the best numerical ice sheet/climate model does not that earlier results which were suggestive of low frequency oscillations now appear to be an artifact sustained oscillations, of nonlinear numerical instabilities in the models. Some specific sources of such numerical instabilities arising from the integration of the highly nonlinear equations in ice sheet models are mentioned. At present,the best numerical ice sheet/climate model does not appear to display a tendency to low frequenty self- sustained oscillations.
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