on the European level [e.g.
Water Framework Directive (Directive 2000/60/EC),
Common Agricultural Policy, etcetera], except for the
Ukrainian part of the Tisza. However, the Ukraine shows
strong incentives to enter the EU community and thus the
EU acquis communautaire is used as key reference for the
development of its water management principles. It was
nevertheless decided to select two case-studies
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
for Iceland were made. The CE
project used an ensemble of six GCMs and RCMs from the PRUDENCE project for four different
emissions scenarios (B1, B2, A2, and A1FI) developed by the Intergovernmental Panel on Climate
Change (IPCC). The GCMs used by the CE project showed more warming during winter than
summer. During winter, the median projected warming from 1961–90 to 2070–99 ranged from
3–6 K, and from 2
/media/ces/2010_005_.pdf
is on the northern North Atlantic and the Nordic Seas. With the southern
boundary at 47 N, the study domain covers Newfoundland, but excludes various marginal and
inland seas with significant independent storm activity, such as the Mediterranean and Adriatic
Seas, as well as the Black and Caspian Seas. The northern boundary at 80 N takes the domain
up to Fram Strait, including Svalbard, but excluding
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
and review of some methods for regional flood frequency anal-
ysis. J. Hydrol., 186, 63–84.
GREHYS. (1996b). Inter-comparison of regional flood frequency procedures for Canadian rivers.
J. Hydrol., 186, 85–103.
Grover, P.L., Burn, D.H. & Cunderlik, J.M. (2002). A comparison of index flood estimation
procedures for ungauged catchments. Can. J. Civ. Eng., 29, 734–741.
Hosking, J.R.M. & Wallis, J.R. (1993
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
stage
)Suppor
t
an
d
ski
lls
n
ee
de
d
Har
e
et
a
l.
(2003
)
X
X
An
aly
se
lin
ks
be
tw
ee
n
participator
y
structur
e
an
d
proces
s
implementatio
n
Ba
rr
et
ea
u
et
a
l.
(2010
)
X
X
X
Pr
o
vid
e
cle
ar
de
sc
rip
tio
n
o
fproces
s
(m
an
ag
e
ex
pe
ct
at
io
n
s);
monitorin
g
an
d
evaluatio
n
Bot
s
an
d
va
n
Daale
n
(2008
)
X
X
X
X
X
Su
pp
o
rt
pr
o
ce
ss
de
sig
n
Ad
ap
te
d
fra
m
ew
o
rk
u
se
d
in
th
/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
it will be one of the main aspects
of this paper.
2.3. Properties
The elements of a Fuzzy Cognitive Map are as follows:
Concepts: C1, C2, . . ., Cn. These represent the drivers and
constraints that are considered of importance to the issue under
consideration.
State vector: A = (a1, a2, . . ., an), where ai denotes the state of the
node Ci. The state vector represents the value of the concepts
/media/loftslag/Kok_JGEC658_2009.pdf
level, surveys commissioned by the European Com-
munity/the European Union provide an indication of trends in concern about cli-
mate change. Since 1992, such surveys have been undertaken among representative
samples of citizens in its Member States, and specifically on topics related to the
environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB
in 2002). These have included
/media/loftslag/Lorenzoni_Pidgeon_2006.pdf
for ice, ocean and land applications
Snævarr Guðmundsson, Hrafnhildur Hannesdóttir and Helgi Björnsson ....................... 15
Post-Little Ice Age (1891–2011 AD) volume loss of Kotárjökull glacier, southeastern Iceland,
as established from historical photograph and lidar
Sverrir Guðmundsson, Eyjólfur Magnússon, Helgi Björnsson, Finnur Pálsson, Tómas
Jóhannesson and Etienne Berthier
/media/vatnafar/joklar/Reykholt-abstracts.pdf
wide and
1000 m long shelf called Þófi, terminating at 80–100 m a.s.l., see Map 4. The inclination of
the shelf is 15 on average. The surface of Þófi is covered with unconsolidated glacial till and
landslide deposits and marked with five gullies. The brook called Þófalækur near the middle of
the shelf divides it into an inner and outer part. On the outermost part of the shelf, there is a small
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf