we take the corresponding
data from the CMIP5 project.
Table 1. All GCMs and RCMs used in this study. If a model is available for any of the
domains Arctic-44, EURO-44, or EURO-11, it is marked with a v, but with an x if it is
unavailable.
Model name Type EURO-11 EURO-44 Arctic-44
CCCma-CanESM2 GCM x vv
COSMO-CLM4-8-17 RCM vv x
CNRM-CERFACS-CNRM-CM5 GCM vv x
IHCEC-EC-Earth GCM vvv/media/vedurstofan-utgafa-2017/VI_2017_009.pdf
14 0 1 2 3 8 12
15 0 1 2 3 8 12
16 0 1 2 4 8 12
17 0 1 2 4 8 12
18 0 1 2 4 8 12
19 0 1 2 4 8 13
20 0 1 2 4 8 13
21 0 2 3 5 9 13
22 1 2 3 5 9 13
23 1 2 3 4 9 13
MEAN 1 2 2 4 8 13
10
AE
R
OD
R
OM
E
CLIM
A
T
OLOGICA
L
SUMMA
R
Y
-
T
ABL
E
D
AE
R
OD
R
OME
:BIK
F
-
KEFL
A
VÍ
K
/K
efl
avi
k
PERIO
D
O
F
RECORD
:2001–201
0
L
A
TITUDE
:6
3
59’06"
N
LONGITUDE
:2
2
36’20"
W
ELE
V
A
TIO
N
AB
O
V
E
MSL
:5
2
/media/vedur/aerodrome_summaries_20140603.pdf
tance ◊
energy losses
hot w e ather
decre ase s the
lifetim e of
tra nsform ers
increas ing
w ater capa city
V ery like ly,
the
pro bability
tha t the next
decad e is
w arm er is
90%.
Phe nom ena
1.1 - higher
te m peratures, espe cially
during winter
Sc en ario 1. war mer clim ate
Conseque nce
categ ory
acc ording to
own ra nking
Lik elihood
according to
own rank in g
Th e op
/media/ces/Keranen_Jaana_CES_2010.pdf
on the costs of
weather related delays and interruptions. Leviäkangas (2007) mentions an amount of 20 ~ 30
million euro per year. As mentioned before over time road users will start to adapt if they realize
that certain delays occur too frequently. Responses could vary from shifts in departure time to
switching to another mode or even relocation of activities.
A note on service levels
In road
/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
and Torfajo¨kull but not for Eyjafjallajo¨kull, rather than an actual sensitivity difference. Effects
of cold and dry years are ignored in the uncertainty calculation.
(a) (b) Using temperature at Vı´k (c) Using temperature at Hveravellir
AAR (%)
All seasons @bn=@T
(m w. eq. yr1 8C1)
Summer @bn=@T
(m w.eq. yr1 8C1)
All seasons @bn=@T
(m w.eq. yr1 8C1)
Summer @bn=@T
(m w.eq. yr1 8C1)
E 2025
/media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
glacier-scaling-hydrological model. 88-89.
Machguth, H., & Ahlstrøm, A. (2010). Surface Mass Balance of the Greenland Ice Sheet in the Paakitsoq Area, Illulisat, West Greenland - Scenarios and Related Uncertainties. p. 42-43.
Melvold, K. & Laumann, T. (2010). A coupled mass-balance and ice-flow model for Midtdalsbreen; projection of glacier length based on climate scenarios (CES). 90-91.
Radic, V/ces/publications/nr/1940
force winds are forecast in the east parts tonight and during the morning, first in the southeastern parts.
A more detailed forecast
Increasing winds by evening, east strong gale or whole gale (20 - 27 m/s). Becoming southerly later tonight, possibly reaching hurricane force or about 33 m/s in the East-fjords area. Moderating northeast and later north winds in the western parts. Precipitation
/about-imo/news/nr/3255
73–100Ásdís Helgadóttir, Emmanuel Pagneux, Matthew J. Roberts, Esther H. Jensen og Eiríkur GíslasonShort summaryChapter V. Öræfi district and Markarfljót outwash plain: Rating of flood hazards (pdf 2.35 Mb)Pages 101–122Emmanuel Pagneux og Matthew J. RobertsShort summaryChapter VI. Öræfi district and Markarfljót outwash plain: Spatio-temporal patterns in population exposure to volcanogenic floods
/volcanoes/about-volcanoes/oraefajokull/new-research/
a
l
y
(
°
C
)
1900 1920 1940 1960 1980 2000
-20
-10
0
1
0
2
0
R
u
n
o
f
f
a
n
o
m
a
l
y
(
%
)
1900 1920 1940 1960 1980 2000
-40
-30
-20
-10
0
1
0
2
0
3
0
E
v
a
p
o
r
a
t
i
o
n
a
n
o
m
a
l
y
(
%
)
Large-scale atmospheric patterns
and hydroclimatological variables
Large-scale atmospheric circulation patterns,
are more accurately assessed by Global
Climate Models than are local variations
/media/ces/ces_SA_group_flyer_new.pdf