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snow albedo feedback, i'm, that explains the difference i n — i fjo, first increasing the ice volume from 120 to 106 kvr BP, and then decreasing it from 106 to 70 kvr BP. (During a a this whole time interval, both Fpi and V\ \ are negligible except slightly after 110 kyr

BP where Vqi is positive and counterbalanced bv V\\,} After 70 kyr BP, the situation

becomes more complex. The pure contribution of sea level change, / ou increases continuously up to the LGM, reaching a maximum of-16x 106 km3 at 17 kvr BP. This increase is slowed by the negative effect of both the VSAF and the synergism between

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