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Response of the ice cap Hardangerjøkulen in southern Norway to the 20th and 21st century climates

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Figure

Fig. 1. Map showing the location of Hardangerjøkulen (H) in south-ern Norway and the locations of the synoptic weather stations fromwhich records are used in this study.
Fig. 2. Present-day surface topography (contours) and bedrock to-pography (colouring) in the model domain, contours are drawn ev-ery 50 m
Table 1. Parameter values used in this study. The value forlisted here is used for extrapolation over the ice cap, for extrapo-lation of air temperature data to the ice cap, different values are �used (Sect
Fig. 3. Altitudinal profiles of the mean measured and modelledwinter mass balance for Rembesdalsskåka for 33 years in the pe-riod 1963–2005
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