input is often ad hoc
and does not do justice to either the richness of the stories or the
quantitative complexity of the models. The weak link between the
qualitative and quantitative scenarios might well be the most
problematic aspect of the Story-and-Simulation methodology.
The main objective of this paper is to introduce, explain, and
illustrate the potential of a possible improvement
/media/loftslag/Kok_JGEC658_2009.pdf
distance between group centres
DL Dalvík lineament
EVZ Eastern volcanic zone
fps fault plane solution
GL Grímsey lineament
GPS Global Positioning System
HFF Húsavík-Flatey fault
HM Hreppar micro-plate
InSAR Interferometric Synthetic Aperture Radar
J17 the 17 June large Holt earthquake
J21 the 21 June large Hestvatn earthquake
KR Kolbeinsey Ridge
max48 maximum group size of 48 events
NVZ
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
J-17, J-21 and M-29. Locations of seismic stations are also sown
(purple triangles).
High-precision earthquake locations, with optimum achievable location accuracy on the order
of tens of meters are currently obtained through relative relocation (double difference) of
manually located earthquakes (Slunga et al., 1995; Hjaltadóttir and Vogfjörd, 2005). The
objective is to obtain
/media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf
strategies. The most effective form of
AWRM employs management programmes that are designed to experimentally compare
selected policies or practices, by evaluating alternative hypotheses about the system being
managed (Pahl-Wostl 2007). The practised IWRM process itself is very dependent on the
geographical, historical, cultural and economic context of a country or region.
The objective of this paper
/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
are the objective of this report, but not for short-term immediate
planning or evacuation during the first stages of an eruption.
The main inputs of the MrLavaLoba code are topography, eruption volume and vent location.
Lava does not flow like water and does not strictly follow the maximum downhill direction
(steepest descent path), although topography, represented by a Digital Elevation Model (DEM
/media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf