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Small-scale variation of snow in a regional permafrost model

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Table 1. The three regression models for CV sd with in increasing number of predictors are cal- cal-ibrated with observed snow distributions from the ALS snow survey (left columns)
Table 2. The model performance is evaluated with respect to the mean annual ground surface temperatures (MAGST) and the mean annual temperature at the depth of the active layer or seasonal freezing layer (MAGT)
Figure 1. Modelled distribution of permafrost in Norway. Sites mentioned in the text: (1) Finse, south of Hallingskarvet, (2) Juvvasshøe in Jotunheimen, (3) Dovrefjell, (4) The Lyngen Alps and (5) Finnmark.
Figure 2. The figure illustrates the area accounted for in each of the 8 runs of the Winstral terrain-based parameter, each of them with a prevailing wind direction d n
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