A

V\\ corresponds, at least in part, to the afTorestation/deforestation of the continental

Mi emerged/submerged platforms following a decrease/increase in sea level (I'm also contains many indirect interactions between sea level and vegetation).

Although these results are only from a model that does not take all processes into account, they show clearly (i) the difficulty of explaining the ice volume changes if the number of experiments performed is too limited (e.g., if w e perform only JI a — f^oi or V\\ — Fio) and (ii) the important role played by the dynamics of the forests and, in particular, in high latitudes their associated albedo feedback when they are covered

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