were carried out to obtain the flow and
sliding parameters for Hoffellsjökull that resulted in a good
simulation of the observed 20th century evolution of the
glacier geometry. The obtained values for the rate factor
and the sliding parameter are A= 4.6× 10−15 s−
1 kPa−3 and
C = 10× 10−15 m a−
1 Pa−3, respectively.
The ice divide is kept at a fixed location in the model
com-
putations presented here
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