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systematically underestimated. The bias is not as pronounced for the non glacial rivers. Com-
bining synoptic-scale and basin-scale predictors (method 3) leads to a substantial improvement
compared to the use of MSLP fields alone (method 1). Analogue forecasts become similar or
better than persistence, depending on catchment and lead time. Usually, persistence performs
better for T=1 day and then method 3
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf
in
Norway was provided by the Norwegian Water Resources and Energy Directorate (NVE).
TóJ 12 5.12.2009
Memo
References
Bahr, D. B., M. F. Meier and S. D. Peckham. 1997. The physical basis of glacier volume–area
scaling. J. Geophys. Res., 102(B9), 20,355–20,362.
Björnsson, H., and F. Pálsson. 2008. Icelandic glaciers. Jökull, 58, 365–386.
Fenger, J. (Ed.). 2007. Impacts of Climate Change on Renewable
/media/ces/ces-glacier-scaling-memo2009-01.pdf
Icelandic glaciers. Jo¨kull 58,
365386.
Bjo¨rnsson H., Pa´lsson F. & Haraldsson H.H. 2002. Mass balance
of Vatnajo¨kull (19912001) and Langjo¨kull (19962001),
Iceland. Jo¨kull 51, 7578.
Bouillon A., Bernard M., Gigord P., Orsoni A., Rudowski V. &
Baudoin A. 2006. SPOT 5 HRS geometry performance: using
block adjustments as a key issue to improve quality of DEM
generation. ISPRS Journal
/media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf