magnitudes. (b) Seismic tremor amplitude in three different frequency bands. (c) Volcanic plume
height. (d) Number of lightning. Lightning and tremor amplitude roughly correlate with plume
height.
Intensifi ed human activity and a growing
population have changed the climate and the
land biosphere. One of the most widely recog-
nized human perturbations is the emission of
carbon dioxide (CO2
/media/jar/myndsafn/2005EO260001.pdf
i
s
c
h
a
r
g
e
m
3
/
s
Observed 1961-90
MetNo-HIRLAM-HadCM3 A1B 2021-50
DMI-HIRLAM-ECHAM5 A1B 2021-50
SMHI-RCA3-BMC A1B 2021-50
Observed and modeled runoff , Aiviekste
0.00
20.00
40.00
60.00
80.00
100.00
120.00
Observed Modeled Reference
mod SMHI
1961-90
mod SMHI
2021-50
Reference
mod DMI 1961-
90
mod DMI
2021-50
Reference
mod MetNO
1961-90
mod MetNO
2021-50
MAM JJA
SON DJF
m3/s
Monthly
/media/ces/Kurpniece_Liga_CES_2010.pdf
-2050
30-year flood
XX
Flood frequency estimation applied
to annual maximum flood series
% change in
200-year
flood
Projected change in 200-yr. flood
between 1961-1990 and 2021-2050
Change (%)
90th percentile
of 150 models
Median of
150 models
Change (%)
Range of uncertainty in projections
Median of
150 models
Change (%) Range (%)
Range
10 to 90%
Downscaling method
0
10
20
30
40
50
60
70
8090/media/ces/Lawrence_Deborah_CES_2010.pdf
A (A1, A2, A3). ........................................................................................... 89
Figure B.2. Rake distribution for mapped faults/clusters in box B, Fagradalsfjall-W. ...... 90
Figure B.3. Rake distribution for mapped faults/clusters in box C, Fagdaralsfjall-E. ....... 90
Figure B.4. Rake distribution for mapped faults/clusters in box D, Kleifarvatn
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.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
aversion should influence the first mover’s decision. The
98 Public Choice (2012) 151:91–119
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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
M A M J J A l
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0 100 200 300
60
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80
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100
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Days since Sept. 1st
Q
(m
³/s
)
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S O N D J F M A M J J A
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0 100 200 300
30
40
50
60
70
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vhm116
S O N D J F M A M J J A
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0 100 200 300
20
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30
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0
50
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(m
³/s
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
Resources and Energy Directorate
Edited by: Heidi H. Pikkarainen
Print: Norwegian Water Resources and Energy Directorate
Number printed: 130
Cover design: Rune Stubrud
Prepared for: The CES project
Norwegian Water Resources and Energy Directorate
Middelthunsgate 29
P.O. Box 5091 Majorstua
N-0301 OSLO
NORWAY
Telephone: +47 22 959595
Fax: +47 22 9590 00
/media/ces/ces-oslo2010_proceedings.pdf