in the area and the monitoring of the Icelandic Met Office must be
secured before the area is opened for the public.
Countermeasures to reduce risk in the area will be taken and further opening of the area will then be decided.
Status:
Seismic activity in Bárðarbunga continues to diminish. Since last Tuesday about 80 earthquakes were detected in
the caldera. The strongest one was M2.5
/media/jar/Factsheet_Bardarbunga_20150310.pdf
climate changes between the CMIP3 and ENSEMBLES
simulations 15
4. Impact of RCM data on forecasts of climate change 18
5. Probabilistic projections of temperature and precipitation change 24
5.1 Best estimates and uncertainty ranges of temperature and precipitation change 24
5.2 How probably will temperature increase (precipitation change) by at least X°C (Y%)?
28
6. Conclusions 34
References
/media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf
) storage coefficient of interflow ki; (3) drainage
density d; (4) the fraction of surface runoff from snowmelt; and (5) the recession constant
krec for the decreasing saturated hydraulic conductivity with increasing depth. For the
groundwater flow, adjusted parameters (6–7) are the hydraulic conductivity in the X and Y
direction. The hydraulic conductivity is adjusted in distributed grids unlike
/media/ces/2010_017.pdf
+ x−k) (1)
Public Choice (2012) 151:91–119 95
with k = 1,2, and −k = 1 if k = 2, −k = 2 if k = 1. The variables xik and x−k are the
contributions to the public good of subject i as mover k and mover −k, respectively. The
contribution of the first mover is an integer x1 ∈ [0,10] and that of the second mover takes
one of the two values x2 ∈ {0, x1}.
2.2 Theoretical predictions
As noted
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf