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................................................................................................................................... 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
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
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
of events closely.
Photo: Sigurlaug Gunnlaugsdóttir.
Bárðarbunga
Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com-
munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson.
I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4
5
The magma intrusion from Bárðarbunga
to the eruption site at Holuhraun and
related tremor pulses
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf