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/
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
At 2250 UTC, the plume was detected by the
weather radar at ~8 km height over Vatnajökull,
reaching ~12 km four hours later (Figure 1c).
Lightning over Grímsvötn, which accompanied
the rising plume (Figure 3d), was eventually
seen at ~0300 UTC, but darkness and weather
conditions prevented visual observation of the
eruption site until the following day.
Over the next two days, the strength
/media/jar/myndsafn/2005EO260001.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
Brunt and Roseanne
Dominguez ............................................................................................................................... 26
Validation of NASA laser altimeters at Summit, Greenland
Hans-Gerd Maas and Ellen Schwalbe .................................................................................. 27
3D velocity fields at Jacobshavn Isbrae glacier from multi
/media/vatnafar/joklar/Reykholt-abstracts.pdf
stage
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t
an
d
ski
lls
n
ee
de
d
Har
e
et
a
l.
(2003
)
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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
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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
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o
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pr
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/media/loftslag/Hare-2011-ParticipatoryModelling.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
), as well as an updated map showing the extent of the lava (pdf 1.4 Mb) and a series of images showing lava streams superimposed on a 3D view of the area (pdf 2.5 Mb).
Aerial photographs, taken by IMO's staff during flight with the Icelandic Coast guard, and taken by Ólafur Sigurjónsson who lives in Forsæti III nearby, show the progress of events during the first one or two weeks
/about-imo/news/nr/1862
events (download as pdf 0.92 Mb)
Update Bárðarbunga 2015 - February events (download as pdf 1.28 Mb)
Update Bárðarbunga 2015 - March-April-May follow up (see pdf 0.71 Mb)
Earthquakes Bárðarbunga - all earthquakes
Earthquakes Bárðarbunga earthquakes - 3D video
Earthquakes Bárðarbunga earthquakes - 3D interactive model
GPS map
/earthquakes-and-volcanism/articles/nr/2947