In collaboration with Ragnar Slunga, his most important contributions were in automatic estimation of fault-plane solutions for microearthquakes by inverting observed polarities and spectral amplitudes of P- and S-waves, and in relative locations of microearthquakes. Sigurður’s research thus demonstrated that microearthquakes contain information about large-scale tectonic processes.
During his student years
/earthquakes-and-volcanism/conferences/jsr-2009/sigurdur
Reference list:
Thomé- Scmidt, P. “Sea level change affecting the spatial development in the Baltic Sea Region.”
Geological Survey of Finland, special edition paper 41. pp. 51-59.
Van Roosmallen L., Christensen, B.S.B, Sonnenborg, T.O. “Regional difference in climate change
impacts on groundwater and stream discharge in Denmark”, 2007. Vadose Zone Journal 6: 554-571.
/media/loftslag/Rolf_Johnsen_(Region_Midt,_Dk).pdf
ANNUAL REPOR T 2014
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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
?Veðurstofa Íslands 2015
Bústaðavegur 7–9, 108 Reykjavík, Iceland
The annual report was drafted by the IMO sta?.
Editor: Sigurlaug Gunnlaugsdóttir
Design and layout: Hvíta húsið
Printing: Oddi
ISSN 2251-5607
Cover photo: Gro Birkefeldt Møller Pedersen
I N D E X
4 Bárðarbunga
7 Rockslide
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
EA Analyse A/S and Optensys
Energianalys will forecast energy system variables, while SINTEF Energy Research will make
assumptions for the energy system in different cases, include new inputs in the EMPS model and
carry out simulations.
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/media/ces/esa_flyer_new.pdf
Grin’s work on this article was part of the programme of the
Dutch Knowledge network on System Innovations (KSI).
P. Huntjens (&) C. Pahl-Wostl
Institute for Environmental Systems Research,
University of Osnabruck, Barbarastraße 12, Geb. 66,
49069 Osnabruck, Germany
e-mail: patrickhuntjens@yahoo.com
J. Grin
Amsterdam School for Social Science Research,
University of Amsterdam, Amsterdam
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
eruptions close to populated areas
and/or international airports
International Strategy for Disaster
Reduction (www.unisdr.org)
WMO (1999) Comprehensive Risk Assessment for Natural
Hazards WMO/TD No. 955, 92 p.
Living with Risk: A global review of disaster reduction initiatives
(2004)
Global assessment report on disaster risk reduction (2009)
Terminology
www.unisdr.org/eng/terminology
/media/loftslag/Karlsdottir-Risk_analysis_IMO_SK.pdf
The applied glacier mass balance model is a simplified version of the energy balance approach.
An abstract of the model is given in the following, for a comprehensive model description we
refer to Machguth et al. (2009). The model requires air temperature (Ta), global radiation
(Sin) and precipitation (P ) for meteorological input. The model runs at daily steps, and the
cumulative mass balance bc on day t
/media/ces/ces_geus_paakitsoq_full_report.pdf
in Finland. Water Resour Management (2010) 24:3437-3459. DOI 10.1007/s11269-010-9614-z.
Veijalainen N., Lotsari, E., Alho, P., Vehviläinen, B., Käyhkö, J. (2010). National scale assessment of climate change impacts on flooding in Finland. Journal of Hydrology 391 (2010) 333-350.
Yang, W., Andréasson, J., Graham, L.P., Olsson, J., Rosberg, J. & Wetterhall, F. (2010). Distribution-based scaling
/ces/publications/nr/1938
place in the same area on 5
December in 1968 (Tryggvason, 1973; Erlendsson and Einarsson, 1996; Halldórsson,
2004). A quite large event also occurred on the RP on 10 June 1933. Its best known
location is near to Fagradalsfjall, at 63.9°N and 22.2°W, and it was probably of magnitude
M 5.5 (Tryggvason, 1973; Halldórsson, 2004).
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/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf