Mass balance measurements started at Storglaciären in the Kebnekaise massif in 1946 (Table 5, #2.1). At present, the measurements comprise a mass balance of 5 glaciers in the area. In calculating one year’s mass balance, measurements are taken twice per year (in winter and summer) and mass balances are calculated annually by the Department of Physical Geography and Quaternary Geology at Stockholm University (SU-INK). Measurement of glacier fronts is a simpler alternative to mass balance calculations that could be used as an index for mass balance. Stockholm University (SU-INK) performs such front measurements at 18 glaciers every second year (Table 5, #2.2).
precipitation, wind, temperature, mass balance, terminus mapping
Stockholm University (SU)