nostaa,
m utta
oh ijuoksutu
ksia tulee
Sähkönvas tus kasvaa
-> energ iahäv iö ita
Muuntajien
elinikä lyhenee
Jääkannen
m uodostaminen
h idastuu
Very likely,
the
probab ility
that the next
decade is
warmer is
90% .
Ilm iö
1 .1 – korkeammat
läm pötilat etenkin talvella
Skenario
1. Lä mpimäpi i lmasto
O ma luokitteluOma luokit te lu
Nykyiset t ai
tuleva t
varautumiskahdo
llisuudet
/media/ces/Keranen_Jaana_CES_2010.pdf
Email: SR: sahar@hi.is, BH: skykkur@hi.is
In earthquake engineering the estimation of the impact of subsoil characteristics on site effects, and
modeling the distribution of ground motion amplitudes are known as key elements in accurate seismic
hazard assessment programs. Recently, the deployment of Icelandic strong-motion arrays, ICEARRAY
I in the SISZ and ICEARRAY II in the TFZ, has
/media/norsem/norsem_sahar.pdf
E
l
b
e
i
n
D
r
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s
d
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n
,
A
p
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i
l
2
0
0
7
CES conference, Oslo, Norway, 31 May - 2 June 2010
Typical features
• develop slowly,
• become severe when they cover a large region and persist for an
extended period.
E
l
b
e
i
n
D
r
e
s
d
e
n
,
A
p
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2
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7
(
s
p
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g
e
l
.
d
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)
Anne K. Fleig et al. “Regional hydrological droughts and weather types in north
/media/ces/AnneFleig_May2010_CES.pdf
the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits
were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes
evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob-
servations
/media/ces/GA_2009_91A_4_Andreassen.pdf
...................................................................................... 31
7 References .................................................................................................. 32
Appendix I - Daily Index flood models for Region 1. .......................................... 35
Appendix II - Daily Index flood models for Region 2. ........................................ 36
Appendix III - Comparison between
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf
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
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d
s
p
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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
and their interactions with sustainable develop-
Figure I.1. Schematic framework representing anthropogenic drivers, impacts of and responses to climate change, and their linkages.
Schematic framework of anthropogenic climate change drivers, impacts and responses
ment. Topic 5 assesses the relationship between adaptation and
mitigation on a more conceptual basis and takes a longer-term per-
spective. Topic 6
/media/loftslag/IPPC-2007-ar4_syr.pdf
and sustainable society. The main vision of the European Plate
Observing System (EPOS) is to address the three basic challenges in Earth Sciences: (i) unravelling the
Earth's deformational processes which are part of the Earth system evolution in time, (ii) understanding
the geo-hazards and their implications to society, and (iii) contributing to the safe and sustainable use
of geo
/media/norsem/norsem_atakan_norway.pdf
...................................................................................... 30
7 References .................................................................................................. 31
Appendix I - Identification of homogeneous groups of catchments obtained with
the ROI technique and associated growth curves .............................................. 33
Appendix II - WaSiM daily flow simulations: Best run verification for the cali-
bration
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf