coastal areas(ag)
Location65°31.412', 13°49.004' (65.5235, 13.8167)
Height above sea-level28.0 m a.s.l.
Beginning of weather observations2017
Station owned byVeðurstofa Íslands - Ofanflóð
View the observations on a mapStation list
/weather/stations/
series started in
1911. At Akureyri the sunshine hours were close to the long-term average.
The Greenland Sea ice appeared at the northern and North-eastern coast, closing some
shipping lanes for a few days in March for the first time in the new century.
The average sea level pressure in Reykjavik was 1008.2 hPa, marginally the highest since
1985.
Short comments on the individual months
/media/vedurstofan/utgafa/skylduskil/ved-eng-2005.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
mean, making 2005 the sunniest year since the record year of 1924, the observation series started in 1911. At Akureyri the sunshine hours were close to the long-term average.
The Greenland Sea ice appeared at the northern and North-eastern coast, closing some shipping lanes for a few days in March for the first time in the new century.
The average sea level pressure in Reykjavik was 1008.2 hPa
/about-imo/news/2006
mean, making 2005 the sunniest year since the record year of 1924, the observation series started in 1911. At Akureyri the sunshine hours were close to the long-term average.
The Greenland Sea ice appeared at the northern and North-eastern coast, closing some shipping lanes for a few days in March for the first time in the new century.
The average sea level pressure in Reykjavik was 1008.2 hPa
/about-imo/news/nr/1207
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
Delta Change Method
(correction of observed precipitation)
Transformation of precipitation
cont
fut
obsfut M
M
PP =
Observeret n dbør
0
5
10
15
20
25
30
1-12-99 11-12-99 21-12-99 31-12-99
Dato
N
ed
bø
r
(m
m
/d
ag
)
Observeret
Skal ring af e
5
10
15
20
25
30
35
4
- - - -
t
N
ed
bø
r
(m
m
/d
ag
)
Observeret D lta Change
Critical assumption:
Future dynamics = present dynamics
No change in number
/media/loftslag/Refsgaard_2-uncertainty.pdf
sr
el
at
ed
to
ag
ric
ul
tu
re
in
D
en
m
ar
k
Cl
im
at
e
ch
an
ge
im
pa
ct
Adaptatio
n
Typ
e
o
f
proble
m
Conse
quenc
e
Ris
k
leve
l
Dom
inatin
g
uncertaint
y
Optio
n
Cos
t
leve
l
Inten
t
Actio
n
Tempora
l
scop
e
Spatia
l
scop
e
Additiona
luncertaint
y
Sou
rc
e
Natur
e
Sourc
e
Natur
e
In
cr
ea
se
d
su
m
m
er
drought
san
d
highe
r
w
at
er
re
qu
ire
m
en
ts
caus
e
by
longe
rcro
p
growt
h
durat
io
n
/media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf
days was 95, 22 days less than the annual average.
Bright sunshine
The year 2012 was one of the sunniest on record both in northern and southwestern Iceland. Akureyri measured bright sunshine during 1415 hours, a new record, and exceeding the old by 140 hours. In Reykjavík the number of sunshine hours was 1587. This is the second highest annual total since the measurements started in 1911, only
/weather/articles/nr/2614