)] [Report (low resolution 4 MB)]
Carlsson, B., Graham, L. P., Andréasson, J., & Rosberg, J. (2005). Exploring the range of uncertainty in climate change impacts on runoff and hydropower for the Luleälven River. Presented at the 15th International Northern Research Basins Symposium and Workshop, Luleå to Kvikkjokk, Sweden, Aug 29 - Sept 2. 9-20. [Paper]
Demers, D., & Roy, R. (2006). Impacts of climate
/climatology/research/ce/publications/
maps for 1971-2000
Daily precipitation maps are available on request and further information on the making of the maps. IMO's contacts for this project are Philippe Crochet and Tómas Jóhannesson.
Reference:
Crochet, P., T. Jóhannesson, T. Jónsson, O. Sigurðsson, H. Björnsson, F. Pálsson and I. Barstad (2007): Estimating the spatial distribution of precipitation in Iceland using a linear model
/weather/articles/nr/1625
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Ensemble approach for probabilistic
hydrological projections
Catchment
/media/ces/Lawrence_Deborah_CES_2010.pdf
located events to invert for a new 1D minimum velocity model for both
P- and S-waves using VELEST. A depth region of a lower vpvs ratio down to 20 km depth is revealed.
We perform relocation of the whole dataset using the new velocity model and the double-difference
relocation technique. We look into details of the depth distribution of the events and how the relocation
procedure affects
/media/norsem/norsem_buhcheva.pdf
will occasionally have to deal with
spurious events. At SNSN we are therefore investigating the feasibility to construct an event verifier.
The basic idea is to emulate the decision made by a seismologist viewing a section of recorded traces,
sorted by epicentral distance, and expecting to see direct P-phase arrivals on most traces out to the
most distant phase pick. Here we will report
/media/norsem/norsem_schmidt.pdf
most of the Suðurbotnahraun lava field and it reached the
Kvíslahraun lava, but the eruptive fissure of the Suðurbotnahraun lava is beside the rockslide
and therefore intact. The slide triggered a tsunami in the lake that washed up on the
lakeshores all around the lake, reaching up to 20–30 m elevation above the water level and
even higher in places. The wave travelled farthest around 400 m
/media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf
). The brittle-plastic transition and depth of seismic faulting, Geol.
Rundsch., 77, 319–328.
Scholz, C. H. (2002). The Mechanics of Earthquakes and Faulting, 2nd ed., Cambridge
Univ., Cambridge.
Sibson, R. H. (1984). Roughness at the Base of the Seismogenic Zone: Contributing
Factors.J. Geophys. Res., 89, B7, 5791–5799.
Sigmundsson, F., P. Einarsson, R. Bilham, and E. Sturkell (1995). Rift-transform
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf