are more sensitive toclimate change than continental glaciers (Oerle-
mans 1992). We analysed the static climate sensi-tivity of Storbreen by applying perturbations to theinput data from Fokstua/Fokstugu (Tair) andRøldal/Bulken (P) respectively using the period1968/
69–2005/2006 as the reference period. Themeasured mean bw, bs and bn in this period are 1.44,
–1.61 and –0.14 m w.e., respectively
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