100
15 17 19 21 23 25
Mean annual peak runoff (mm/day)
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g39g72g79g87g68g3g70g75g68g81g74g72g3
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Percentage change in 200-year flood
Uncertainty – Relative magnitude of
sampled s urces
N = 115
GCM/RCM = 50
EA/DC = 38
HBV = 27
• Differences in GCM/RCM
tend to be more significant
in inland
/media/ces/Lawrence_Deborah_CES_2010.pdf
catchments. Hydrology Research (Accepted - In press).
Olsson, J., Yang, W., Graham, L.P., Rosberg, J., & Andréasson, J. (Submitted to Tellus, 2009) Hydrological climate change impacts on inflows to Lake Vänern, Sweden: An ensemble approach.
Veijalainen, N., Dubrovin, T., Marttunen, M. & Vehviläinen, B. (2010). Climate Change Impacts on Water Resources and Lake. Regulation in the Vuoksi Watershed
/ces/publications/nr/1938
to theoretical framework. I do also want to thank him for an
enjoyable time during this work, both in the office and in the field.
This work was carried out as a part of the Skaftá cauldrons research project which
was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja-
sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com-
pany), the National Energy
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
are located on the north and south coasts of the estuary. The average
annual nutrient input to the Fjord from freshwater is 1503 tons N and 37 tons P (average from 1985 to
2006). The two main streams and the waste water treatment plant for Horsens town, which is located
close to mouth of Bygholm stream, accounts for approximately 75% and 65% of the nitrogen and
phosphorous discharges, respectively
/media/loftslag/Horsens_case.pdf
The
role of orography was found to be crucial in determining the precipitation dis-
tribution and amount.
Atmospheric flow over Iceland was simulated for the period January 1961
through June 2006 using version 3–7–3 of the PSU/NCAR MM5 mesoscale
model (Grell et al., 1995). The domain used is 123× 95 points, centered at
64◦ N and 19.5◦ W, with a horizontal resolution of 8 km. There are 23 vertical
/media/ces/Paper-Olafur-Rognvaldsson_91.pdf
the Hestvatn-fault. ............................................................................................ 37
Figure 3.9. Mapped fault segments in boxes O and N. ........................................................ 40
Figure 3.10. Map of Reykjanes Peninsula. .......................................................................... 41
Figure 3.11. Left: Aftershocks mapped on the Kleifarvatn
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
exist that reach
back to early 19th century but most series are much shorter (Hamlington and Thompson, 2016). In
contrast, satellite altimetry has only been available since the early 1990’s. Satellite altimetry mea-
sures the sea surface height, namely the sea level compared to a fixed reference frame (the center of
the earth, the geoid or a reference ellipsoid) for latitudes up to 66 N and S (ESA
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
aversion should influence the first mover’s decision. The
98 Public Choice (2012) 151:91–119
Fi
g.
1
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Public Choice (2012) 151:91–119 99
Table 1 The predicted effect of
intrinsic preferences on first and
second movers’ contributions
1st mover 2nd mover
Disadvantageous Negative None
inequity aversion
Advantageous None Positive
inequity
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
and insignificant
crustal movements north of Vatnajökull around the dyke.
Air quality in urban areas in the East of Iceland:
o High air pollution was detected yesterday in Egilsstaðir and Reyðarfjörður.
Forecasts indicate that the gas cloud will blow towards the north in the next
24 hours. High concentrations of sulphuric gases can be expected in
Mývatnssveit, Kelduhverfi, Tjörnes, Húsavík
/media/jar/myndsafn/Factsheet_Bardarbunga_140914.pdf