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
)(L)
Rel. RMSE= 1.1
NS= 0.48
MAE= 124
l
l
l
l
l
l
l
ll
ll
0 400 800 1200
0
50
0
100
0
150
0
Pred. (m³/s)
R
ef
. (m
³/s
)
µ(D)=(θ0) + (θ1)(A L)
Rel. RMSE= 0.96
NS= 0.92
MAE= 58
l
l
l
l
l
l
l
ll
ll
0 400 800 1200
0
50
0
100
0
150
0
Pred. (m³/s)
R
ef
. (m
³/s
)
µ(D)=(θ0) + (θ1)(A Z)
Rel. RMSE= 1.2
NS= 0.84
MAE= 90
l
l
l
l
l
l
l
ll
l
ll
0 500 1000 1500
0
50
0
100
0
150
0
Pred. (m³/s)
R
ef
. (m
³/s
)
µ(D
/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
in July 2016 on a Delta II rocket from
Vandenberg Air Force Base in California.
ICESat-2 will carry the Advanced Topographic Laser Altimeter System (ATLAS) and collect
data to a latitudinal limit of 88 degrees. In contrast to Geoscience Laser Altimeter System
(GLAS) on ICESat, ATLAS employs a 6-beam micro-pulse laser photon-counting approach.
It uses a high repetition rate (10 kHz; 70 cm
/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
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
) ................. 89
Figure 61 Tephra accumulation rate on the ground on 8 October 1982 (Öræfajökull) ............ 90
Figure 62 Tephra accumulation rate on the ground in Skaftafell (Öræfajökull) ...................... 91
Figure 63 Preliminary intersectional map ................................................................................ 93
Figure 65 Initial user-interface of the public web-site
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf