for. Extended
melt approach was used to account for melting on glaciers where the effects of radiation
are added to a
classic degree-day model. For infiltration, a methodology of Peschke, based
on the approach of Green and Ampt, was used. To calculate the fluxes within the
unsaturated soil zone, the Richards equation was used. The groundwater table was
modelled in both the unsaturated zone module
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