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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
the com-
plexity of the hydrological processes through modelling, but its application is usually limited to
the short-range. Although the results demonstrated a great potential for this method, its success-
ful application in real-time will strongly depend on the quality and availability of streamflow
observations, which can be poor or simply missing during periods of variable durations, e.g
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf
................................................................................................................................... 88
Melvold, K. and Laumann, T.
A coupled mass-balance and ice-flow model for Midtdalsbreen; projection of glacier length based on climate
scenarios (CES) ..................................................................................................................................................... 90
Thorsteinsson, Th., Sigurðsson, O. and Einarsson, B.
Monitoring changes
/media/ces/ces-oslo2010_proceedings.pdf
við strik
sprungunnar í heild, en þó er hún samhangandi við botninn. Hestvatnssprungan er einnig
nær lóðrétt og um 15,5 km löng og með strikstefnu N179°A. Hún er ólík Holtasprungunni
að því leyti að hún dýpkar til suðurs, úr 6 í 9 km en jafnframt virðist hún mynduð úr
tveimur mishallandi flötum. Rétt sunnan skjálftamiðjunnar er sprungan nær lóðrétt (88°
halli) en norðan upptakanna hallar
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf