/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
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
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
) and changing climate (CC:CC)
1. Current climate (CU)
- varying thinning regimes
(0%, 15%, 30%,45%)
2. Changing climate (CC)
- varying thinning regimes
(0%, 15%, 30%,45%)
3. Current (CU) &
changing climate (CC)
- current thinning regime
4. Current (CU) &
changing climate (CC)
- changed thinning regimes
C
l
i
m
a
t
e
s
c
e
n
a
r
i
o
s
M
ea
s
u
r
e
m
en
t
s
o
f
c
l
i
m
a
t
e
p
/media/ces/CES_BioFuels_Flyer_new.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
activities.
Anne K. Fleig et al. “Regional hydrological droughts and weather types in north-western Europe “
University of Oslo Droughts WTs SummaryRelationsIntroduction Outlook
Hydrological drought in NW-Europe: Data
5
6
5
8
6
0
5
5
.
5
5
6
.
0
5
6
.
5
5
7
.
0
5
7
.
5
-10 -5 0 5 10 15 20 25
3
5
4
0
4
5
5
0
5
5
6
0
6
5
7
0
s
o
u
r
c
e
:
N
a
t
i
o
n
a
l
E
n
v
i
r
o
n
m
e
n
t
a
l
R
e
s
e
a
r
/media/ces/AnneFleig_May2010_CES.pdf
the observed data sets are smaller in SW than in NE
• MMM overestimates precipitation, but is closer to observations in SW than
NE barb2right Better observational coverage in SW
SW
NE
p
r
e
c
i
p
i
t
a
t
i
o
n
s
u
m
(
m
m
)
CES Conference, Oslo 31.5.-2.6.2010
SWNE
• Precipitation trends (mm / 10 yr) in 1961-2000 according to observations
and model simulations (MMM)
• Including the range
/media/ces/TietavainenHanna_CES_2010.pdf