ANN−10
−5
0
5
10
15
20
delta w (%
)
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17C
h
a
n
g
e
i
n
g
e
o
s
t
r
o
p
h
i
c
w
i
n
d
s
p
e
e
d
(
%
)
Change in wind over the Baltic Sea in 70 years time at the time of CO2-doubling
Chen and Aschberger, 2006
17
CM
IP
G
CM
s
A need for regional ensemble simulations
head2right Changes are uncertain
head2right Size and sometimes even sign
/media/ces/Kjellstrom_Erik_CES_2010.pdf
including, for example, ensuring dam safety. The
goal of the new Climate and Energy Systems project is to look at climate impacts closer in time and assess the
a n o ect ves o t e ro ect
An evaluation of risk under increased uncertainty in
order to improve decision making in a changing
climate was carried out through the following steps:
development of the Nordic electricity system for the next
/media/ces/ces_risk_flyer.pdf
≤
≤
>−
0
00
0
)(
TTif
TTifTTDDFsnow
≤
>−
0
00
0
)(
TTif
TTifTTDDFice
Mean annual temperature difference
Difference relative to 1971-2000
Difference between 25% warmest and 25% coldest years
barb2right +1°C (25% warmest)
barb2right -0.7°C (25% coldest)
barb2right +1.7°C
Catchment elevation (m.a.s.l)
Catchment elevation (m.a.s.l)
s
n
o
w
m
e
l
t
(
m
m
/
d
)
g
l
a
c
i
a
l
m
e
l
t
/media/ces/Crochet_Philippe_CES_2010.pdf
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
study and location of catchments. Catchment vhm278 is embedded
within vhm148 and catchment vhm277 is embedded within vhm149.
9
l
l l l
l
l
ll
l
l
l
l
l
l l l
l
l l
l
ll l l l
l
l
l ll
l
ll
l
l l
l l
l
0 100 200 300
10
0
20
0
30
0
40
0
Day since 1st Sept.
Q
m³
/s
VHM 148
S O N D J F M A M J J A
l
l
ll l l
l
ll
l
l
l
ll
l
l
ll l
l
0 100 200 300
15
0
25
0
35
0
45
0
Day since 1st Sept.
Q
m³
/s
VHM
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf
aversion should influence the first mover’s decision. The
98 Public Choice (2012) 151:91–119
Fi
g.
1
O
pt
im
al
co
n
tr
ib
u
tio
n
de
pe
nd
in
g
o
n
α
,
r
an
d
p
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
[Abstract]
Aðalgeirsdóttir, G., Jóhannesson, T., Björnsson, H., Pálsson, F., & Sigurðsson, O. (2006). The Response of Hofsjökull and southern Vatnajökull, Iceland, to climate change. Journal of Geophysical Research, 111 (F03001), doi:10.1029/2005JF000388.
Andreassen, L. M., Elvehøy, H., Jóhannesson, T., Oerlemans, J., & Beldring, S. (2006). Changes in run-off from glaciated areas due
/climatology/research/ce/publications/
: Impacts, risks and adaptation, Oslo, 31 May-2 June 2010.
Ólafsson, H. & Rögnvaldsson, Ó. (2008). Regional and seasonal variability in precipitation scenarios for Iceland. In O. G. B. Sveinsson, S. M. Garðarsson & S. Gunnlaugsdóttir (Eds.), Northern hydrology and its global role: XXV Nordic hydrological conference, Nordic Association for Hydrology, Reykjavík, Iceland August 11-13, 2008, pp 623-629
/ces/publications/nr/1680
to get highly
accurate results in photogrammetric processing of historical photographs.
REFERENCE
Jóhannesson, T., H. Björnsson, F. Pálsson, O. Sigurðsson and Þ. Þorsteinsson. 2011. Lidar
mapping of the Snæfellsjökull ice cap, western Iceland, Jökull, 61,19–32.
Lidar measurements of the cryosphere
Reykholt, Iceland, June 20–21, 2013
12 Csatho and others
The ICESat-2 mission: design
/media/vatnafar/joklar/Reykholt-abstracts.pdf
et al., 2013). Based on satellite altimetry, the trend in absolute sea
level in the North Sea was about 1-3 mm/yr in 1992-2014, depending on location (EEA, 2017).
In the Baltic, the mean sea level rose 1.5 mm/yr in the 20th century (Nerheim et al., 2017). The
absolute sea level rise for the Scandinavian coast of the Baltic in period 1891-1990 was found to
be 1.8 mm/yr (O. Vestøl, 2006). In 1992
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf