7
1 2 3 4 5 6 7 8 9 10 11 12
Month
M
ea
n
d
is
ch
ar
g
e
(m
3 /
s)
Present: Mean A2: Mean
Station 280001: Upstream Bygholm Lake
0
5
10
15
20
25
30
35
1 2 3 4 5 6 7 8 9 10 11 12
Month
M
ax
im
u
m
d
is
ch
ar
g
e
(m
3 /
s)
Present: Max A2: Max
Station 270045: Upstream Lake Nørrestrand
0
2
4
6
8
10
12
14
16
1 2 3 4 5 6 7 8 9 10 11 12
Month
M
ea
n
d
is
ch
ar
g
e
(m
3 /
s)
Present: Max A2: Max
/media/loftslag/Horsens_case.pdf
(alb: AWS)
MODELLING LONG-TERM SUMMER AND WINTER BALANCES
? The authors 2009
Journal compilation ? 2009 Swedish Society for Anthropology and Geography 241
ed temperatures relative to –20°C to account for de-cay of snow albedo at temperatures below the melt-ing point, following a study by Winther (1993). Wetested both approaches, and chose to use –5°C asthe minimum for the accumulated temperature
/media/ces/GA_2009_91A_4_Andreassen.pdf
(see e.g.
Steg, 2003). In studies from several countries, push
measures are perceived as less acceptable compared to
pull measures (e.g. Ho¨lzer, 2003; Rienstra, Rietveld, &
Verhoef, 1999; Steg & Vlek, 1997). For example, in a
European study, over 90% of the car users supported
improved public transport and park-and-ride schemes,
while less than 20% approved of reduced parking space
and cordon
/media/loftslag/Eriksson_Garvill_Nordlund_2006.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
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
................................................................................................................................... 88
Melvold, K. and Laumann, T.
A coupled mass-balance and ice-flow model for Midtdalsbreen; projection of glacier length based on climate
scenarios (CES) ..................................................................................................................................................... 90
Thorsteinsson, Th., Sigurðsson, O. and Einarsson, B.
Monitoring changes
/media/ces/ces-oslo2010_proceedings.pdf
On the northern side a tephra wall rises 20 meters above the water. The ice walls at the southwestern corner of the crater are melting, i.e. at the site of the vent that was active 4 - 6 June. The rate of melting is assumed to be about one cubic meter per second.
Details on the volume of the lake, and possible flooding from it, in a status report issued collectively by the Icelandic Meteorological
/earthquakes-and-volcanism/articles/nr/1884