/ design,
availability, materials, ICT,
modal split)
26.8.2011Adriaan Perrels/IL 5
Categorising stages of adaptation
Passive Adaptation
- automatic in nature
and economy
- only ex post measures
(no anticipation)
Active Adaptation
- automatic in nature
and economy
- ex ante and ex post
policies
Emission scenario dependent
baseline (A1-T, B1, A2, etc.)
Reference costs and benefits
/media/loftslag/Perrels-CBA.pdf
bodies of management,
decision-support, risk, and participation literature.
d’Aquino (2008)
Patrick d’Aquino relies on 20 years of
implementation and evaluation experience, mostly
in a natural resource management context and in
developing countries. His approach is, at this point,
the least conceptually developed design method of
the guides presented here, although it is linked to a
theoretical
/media/loftslag/vonKorff_etal-2010.pdf
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
Neotectonics in Nordland; NEONOR 2
C. Lindholm, O. Olesen, I. Janutyte, S. Gradman, M. Keiding, H. Kierulf,
M. Ask, J. Dehls, Y. Maystrenko, F. Riis, L. Rise and other project partners
The Nordland shore region is known to be seismically active with deep local sediment basins on the
continental shelf that stretches some 200 km west of the coastline. The offshore areas west of Nordland
have
/media/norsem/norsem_lindholm.pdf
tg
ui
da
n
ce
fo
rt
ra
ns
bo
un
da
ry
w
at
er
s,
pr
ep
ar
ed
an
d
P. van der Keur et al.
(floo
dmanag
ement
)an
d
wat
er
qualit
y
ag
re
ed
u
po
n
in
co
m
m
o
n
u
n
de
rs
ta
nd
in
g,
creat
ed
th
e
bas
is
fo
rth
e
formul
atio
n
o
f
joi
nt
m
ea
su
re
s
(Fr
ijte
rs
an
d
Le
en
tv
aa
r
200
3)
Mo
del
s
(na
tural
,te
chnica
l
an
d
so
ci
al
sy
ste
m
s):
Uncert
aint
y
ha
s
to
be
incorp
orated
:
1:
Ep
ist
/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
approximately centred around Iceland: the outer domain with
43 42 grid points spaced at 27 km (1134 1107 km), the intermediate domain with 9590 grid
points spaced at 9 km, and the inner domain with 196 148 grid points spaced at 3 km. The
northwest corner of the outer domain covers a part of the southeast coastal region of Greenland.
Otherwise, the only landmass included in the model domain
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
A. (2010b). 21st century changes in the European climate: uncertainties derived from an ensemble of regional climate model simulations. Tellus, published online. DOI: 10.1111/j.1600-0870.2010.00475.
Ólafsson H, & Rögnvaldsson Ó. (2010). Regional and Seasonal Variability in Precipitation Scenarios For Iceland. Hydrology Research, in revision.
Peltonen-Sainio, P., Hakala, K., Jauhiainen, L/ces/publications/nr/1680
Reykjavík, 139 pp.
Paterson, W.S.B. 1994. The Physics of
Glaciers (Third Edition). Pergamon. 480
pp.
Vogt, P.R., G.L. Johnson and L. Kristjánsson
1980. Morphology and magnetic anomalies
north of Iceland. J. of Geophysics 47, 67-80.
Walker, G.P.L. 1974. Eruptive mechanisms in
Iceland. In L. Kristjánsson, ed. Geodynamics
of Iceland and the North Atlantic Area. D.
Reidel, Dordrecht
/media/jar/Jokull-guidlines.pdf