Jökull


Jökull - 31.12.2001, Side 80

Jökull - 31.12.2001, Side 80
Helgi Björnson et al. accumulation there is fairly sensitive to the winter temperature and position of the paths of the North Atlantic lows pressure weather fronts passing Iceland. No simple relationship can be seen between the win- ter balance on Langjökull and the winter precipitation at a nearby meteorological station (Hveravellir). The minimum winter balance in 2001. however, coincided with a minimum winter precipitation at the station. The net balance has been negative over the entire sur- vey period from 1996 to 2001 and the accumulation area has varied from 10% to 40% of the glacier area. The total mass loss over the period 1996-2001 was 5.73 m (5.36 km3 water equivalent), or 3% of the total ice mass of Langjökull. Acknowledgments The work was carried out in collaboration between the National Power Company and the Science Institute, University of Iceland. Since 1996 the work has been supported by EU-funds (TEMBA 1996-1997, ENV4- CT95-0105, and ICEMASS 1998-2001, ENV4- CT97-0490). Support from the Research Fund of the University of Iceland is acknowledged. Some of the data were collected during expeditions of the Iceland Glaciological Society. ÁGRIP Afkoma Vatnajökuls (1991-2001) og Langjökuls (1996-2001) Raunvísindastofnun Háskólans hefur á hverju ári 1991 til 2001 mælt afkomu Vatnajökuls í samstarfi við Landsvirkjun, og frá 1996 með styrkjum frá Evrópu- sambandinu. Á sama hátt hefur afkoma Langjökuls verið mæld frá 1996 til 2001. Afkoman var mæld vor og haust í punktum, sem voru dreifðir með hæð frá sporðum til hæstu svæða, 40-50 á Vatnajökli og 22 á Langjökli. Fyrstu þrjú árin var afkoma Vatnajök- uls jákvæð, nálægt jafnvægi fjórða árið en hefur síðan verið neikvæð. Alls rýrnaði Vatnajökull um 19,4km3 frá 1991 (2,37 m af vatni jafndreift yfir jökulinn) og missti um 0,6% af ísmassa sínum. Afkomutölur ein- staka skriðjökla eru í töflu I. Afkoma Langjökuls hef- ur verið neikvæð öll þau fimm ár sem hún hefur verið mæld, 1996-2001, samtals um 5,36 km3 (5,73 m), og ísforði hans rýrnaði um 3%. REFERENCES Björnsson, H., F. Pálsson, M. T. Guðmundsson and H. H. Haraldsson, 1999. Mass balance of western and northern Vatnajökull, Iceland, 1991-1995. Jökull 45, 35-58. 78 JÖKULLNo. 51
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