On the origin of the ice ages

Abstract

Ice sheet dynamics provide a possible explanation for the 100 kyr power in climatic records. Some numerical experiments presented here show that even the transition from an essentially ice-free earth to a glacial can be produced by a northern hemisphere ice-sheet model, provided that a slow general cooling on the northern hemisphere continents is imposed. Such a cooling could for example be the result of continental drift

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Utrecht University Repository

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Last time updated on 14/06/2016

This paper was published in Utrecht University Repository.

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