of events closely.
Photo: Sigurlaug Gunnlaugsdóttir.
Bárðarbunga
Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com-
munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson.
I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4
5
The magma intrusion from Bárðarbunga
to the eruption site at Holuhraun and
related tremor pulses
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
/EPP 2
Stakeholders analysis
26 August 2011 PM/YZ/EPP 3
Stake
h
o
l
d
e
r
s
P
u
b
l
i
c
/
p
r
i
v
at
e
P
o
w
e
r
l
e
v
e
l
(“
n
u
i
s
an
ce”
ca
p
a
c
i
t
y
)
O
r
i
e
n
tat
i
o
n
H
or
s
t
e
n
s
m
uni
c
ipal
i
t
y
(
c
o
m
pe
t
e
n
t
a
u
t
h
ori
t
y
)
P
u
b
l
i
c
S
t
ron
g
Go
v
ernanc
e
N
eighbour mun
i
c
i
p
ali
t
y
P
u
b
l
i
c
S
t
ron
g
Go
v
ernanc
e
Poli
c
y
/media/loftslag/Group5-Stakeholders_involvement.pdf
on the homogenised ERA-40 / ERA-Interim
data, are shown in Figure 3. As found in earlier studies (e.g., Serreze, Box, Barry, & Walsh,
1993; Serreze, Carse, Barry, & Rogers, 1997), the Icelandic Low is the dominant feature of the
seasonal low-level circulation across the northern North Atlantic. It is situated southwest of Ice-
land, downstream of a well-developed mean upper-level trough during
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
support
)
Improv
e
mode
l
(integration)
;
socia
llea
rnin
g
Farmers
,loca
l
aut
horities
,
association
s
NO
P
IN
D
Cognitiv
e
mappin
g
HE
T
GM
B
NO
P
HE
T
Simulation
-
by-han
d
OT
:Researcher
s
KA
F
F
Iska
r (Phas
e1
)
Co
n
ce
pt
u
al
m
o
de
l
(D
is
cu
ss
io
n
su
pp
o
rt
;
Com
m
unication
)
Improv
e
mode
l
(integration)
;
socia
llea
rnin
g
Nationa
l
poli
cy-maker
s
NO
P
IN
D
Cognitiv
e
mappin
g
HE
/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
series analysis
Regional series are compiled based on regions
having similar climatological characteristics and
streamflow regimes. These series are also useful
for evaluating patterns and trends, both in time and
by region. Regional series for precipitation,
temperature and runoff are being compiled,
updated and analysed within the CES project.
-
4
0
-
2
0
0
2
0
4
0
6
0
W
S
P
S
U
M
A
Q
,
%
-
4
0
/media/ces/ces_SA_group_flyer_new.pdf
). This can be helpful with respect to
finding a common structure in presenting as well in session reporting (for which angles
mentioned in the opening session statements of the Workshop participants can provide
checkpoints).”
Session rapporteur allocation
M
o
n
d
a
y
2
9
.
8
Y
u
a
n
g
Z
h
e
n
g
A
t
h
a
n
a
s
i
o
s
V
o
t
s
i
s
E
i
v
i
n
d
J
u
n
k
e
r
M
i
c
h
a
e
l
L
a
i
h
o
H
e
c
to
r
/media/loftslag/Guidelines2-for-rapporteurs.pdf
(-33%) during 1970 to 2004 has been smaller than the com-
bined effect of global income growth (77%) and global population
growth (69%); both drivers of increasing energy-related CO2 emis-
sions. The long-term trend of declining CO2 emissions per unit of en-
ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM}
Differences in per capita income, per capita emissions and
energy
/media/loftslag/IPPC-2007-ar4_syr.pdf
to theoretical framework. I do also want to thank him for an
enjoyable time during this work, both in the office and in the field.
This work was carried out as a part of the Skaftá cauldrons research project which
was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja-
sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com-
pany), the National Energy
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf