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A set of 2,000-year simulations of moraine building by a glacier flowing through a synthetic alpine landscape forced by interannual variability in weather imposed on an otherwise stable climate. Moraine relief is shown for a standard deviation in mean annual air temperature (dT) of 0.5��C, 1.5��C, and 3.0��C around a long-term mean of 7.0��C. Simulations were made using the ice-flow model iSOSIA (Egholm et al., 2011, Geomorphology).
Quaternary, Moraine, Sediment transport, Glacier model
Quaternary, Moraine, Sediment transport, Glacier model
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