sjáanleg.
Við vesturjaðar hraunsins sást afgasandi op með brennisteins útfellingum og mjög greinilegum,
brúnleitum gufustrók. Opið er um 50 metra inn í hrauninu sem var mjög úfið og seinfarið. Mælingar á
Gasi voru gerðar með tveim mælum (Handmæli og mælum frá alphasens)
Hæðstu gildi sem fundust í opinu voru 7ppm SO2 og 9 ppm CO.
Gasmælingar úr þyrlu voru gerðar á nokkrum stöðum yfir hrauninu (við
/media/jar/field_report_03032015.pdf
tance ◊
energy losses
hot w e ather
decre ase s the
lifetim e of
tra nsform ers
increas ing
w ater capa city
V ery like ly,
the
pro bability
tha t the next
decad e is
w arm er is
90%.
Phe nom ena
1.1 - higher
te m peratures, espe cially
during winter
Sc en ario 1. war mer clim ate
Conseque nce
categ ory
acc ording to
own ra nking
Lik elihood
according to
own rank in g
Th e op/media/ces/Keranen_Jaana_CES_2010.pdf
the NAO-index and bw is weak-er at Storbreen (r=0.61) than at more maritime gla-
ciers such as Nigardsbreen (r=0.71) and Ålfotbreen(r=0.78) located further west (Nesje et al. 2000).
Meteorological observations at StorbreenAn automatic weather station (AWS) has been op-erating in the ablation zone of Storbreen at c. 1570
m a.s.l. since September 2001 (Fig. 1). The stationis part of the Institute
/media/ces/GA_2009_91A_4_Andreassen.pdf
s
fro
m
climat
e
ch
ang
e
an
d
cr
o
ss
bou
ndar
y
adaptatio
n
measu
res
.
In
th
e
Netherl
and
s
fo
r
hyd
rodyna
m
ic
mod
el
syst
em
s
lik
e
SOB
EK-
W
AQ
UA
(loca
lleve
l)
an
d
e.g
.
fo
rR
hi
ne
flo
w
(ba
sin
wi
de
)c
o
n
sid
er
ab
le
u
n
ce
rta
in
tie
s
ex
ist
(W
ee
rts
et
al
.200
3)
D
ev
el
op
m
en
to
fi
nt
eg
ra
te
d
ba
sin
m
o
de
l(
flo
od
ing
an
d
poll
ution)
.
2:
St
at
ist
ic
al
/q
ua
lit
/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
Testing the method with data from the winter months only
gives a higher correlation of 0.58 (using different data for op-
timization and testing). This regression method reconstructs
the long term variability in the precipitation, but the resulting
annual variability is smaller than the observed.
4 Future climate scenarios
In total 13 future climate scenarios from the Nordic Project
Climate
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf