the contiguous USA. 30th Annual Applied Geography Conference, Indianapolis, October 2007. 10 pp.
Clausen, N.-E., Lundsager, P., Barthelmie, R., Holttinen, H., Laakso, T. & Pryor, S.C. (2007). Wind Power. In: J. Fenger (Ed.) Impacts of Climate Change on Renewable Energy Sources: Their role in the Nordic energy system, Nord 2007:003, 105-128.
Clausen N.E., Pryor S.C., Larsén X.G., Hyvönen R
/ces/publications/nr/1944
2010: Climate Change and Freight Transport. Publications of the Ministry of Transport
and Communications 15/2010. 98 pp. (in Finnish, abstract in English)
[6] Perrels. Adriaan, Himanen, Veli, Lee-Gosselin Martin (2008), Building Blocks for Sustainable Transport –
Obstacles, Trends, Solutions, Emerald publishers.
/media/loftslag/CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction.pdf
at
e
(C
limat
e
models
)
GC
M
s
X
X
XX
X
X
X
X
RCM
s
X
X
XX
X
X
X
X
Initia
lco
n
ditions
/
nat
ura
lva
riabilit
y
X
X
XX
X
D
ow
ns
ca
lin
g/
sta
tis
tic
al
co
rr
ec
tio
n
X
X
X
X
X
X
X
X
X
W
ate
r
syst
em
impact
s
(H
yd
ro
-e
co
lo
gi
ca
lm
o
de
ls)
X
X
X
X
X
XX
X
X
X
X
X
X
X
X
X
Socio
-econo
m
ic
imp
act
s
(So
ci
o-
ec
on
om
ic
to
ol
s)
X
X
X
X
X
X
X
X
X
XX
X
X
X
A
da
pt
ati
on
m
ea
su
re
s
X
X
X
X
/media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf
Nesjum
0-5 5-10 10 15 20-15
2008-2018
1979-1989
Dæmi um ólíkt rennslismynstur.
100
9080
70
60
50
40
30
20
10
0
Júní
mánaðarmeðaltal
Ársmeðaltal
Rennsli
m
3 /s
Sigurvegarinn í getraun Veðurstofunnar á Vísindavöku Rannís hlaut
heimsókn á Veðurstofuna að launum. Salka Elín Sæþórsdóttir ásamt
vinum sínum, Ými og Bjarti. Með þeim á myndinni er Ragnar Heiðar
Þrastarson, fagstjóri landfræðilegra
/media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf
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
water infra-
structure projects begun now are large
enough to push hydroclimate beyond the
range of historical behaviors (19). Some
regions have little infrastructure to buffer the
impacts of change.
Stationarity cannot be revived. Even with
aggressive mitigation, continued warming is
very likely, given the residence time of
atmospheric CO2 and the thermal inertia of
the Earth system (4, 20/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
striking
westwards and a group of N-S-striking pressure axis dipping 45 degrees from the
horizontal and more, suggesting that extensional forces play a large role. Figure 9 includes
the mechanisms of 82 out of the 99 earthquakes in total located between 17 and 26 km
depth and thus shows nearly the same results as described earlier for that interval, that the
tension axis is chiefly horizontal
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf
(alb: AWS)
MODELLING LONG-TERM SUMMER AND WINTER BALANCES
? The authors 2009
Journal compilation ? 2009 Swedish Society for Anthropology and Geography 241
ed temperatures relative to –20°C to account for de-cay of snow albedo at temperatures below the melt-ing point, following a study by Winther (1993). Wetested both approaches, and chose to use –5°C asthe minimum for the accumulated temperature
/media/ces/GA_2009_91A_4_Andreassen.pdf