Abstract
In this letter, we present surface mass-balance measurements
carried out by members of the Institute for Marine
and Atmospheric Research of Utrecht University (IMAU)
along the Kangerlussuaq (Sondre Stromfjord, in Danish)
transect (K-transect), located on the western part of the
Greenland ice sheet along 67° N. At present, these measurements
comprise 10 years (1990-2000), which makes
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