an ice strip at 66°42'N and 24°15' W up to 66°59'N and 22°24'W. On the 14th an observation was also received from the weather station „Hraun á Skaga“ on an iceberg 10-11 nm northwest of Skagatá.
On the 22nd an ice strip was observed at 66°49'N and 22°22'W until 66°51'N and 22°09'W.
On the 29th two icebergs were observed in Þverál. IMO issued information and an image of the ice edge 16th June.
Wind
/sea-ice/monthly/2010/nr/2341
An ice edge was observed in the area from 67°31'N and 023°35'W to 66°41'N and 23°43'W. Westerlies were a little more prevailing in the Greenland Strait and north of Iceland than on average
/sea-ice/monthly/2010/nr/2340
reported on a floe on 66°12,67'N 27°38,17'W and on the 30th a ship observed a large iceberg in location 66°56'N 24°44,4'W.
Wind directions were close to the average on the Greenland Strait this month
/sea-ice/monthly/2010/nr/2343
Resources and Energy Directorate (NVE), Norway. Lidar measurements of Norwegian glaciers ‒ an overview
René Forsberg, Henriette Skourup and Sine M. Hvidegaard, DTU Space, Technical University of Denmark. A decade of lidar measurements for ice, ocean and land applications
Allen Pope, Ian C. Willis*, Finnur Pálsson Neil S. Arnold, W. Gareth Rees, Lauren Grey, Scott Polar Research Institute (SPRI
/lidar/lidar-2013/program/
Hare MP, Barreteau O, Beck MB, Letcher RA, Mostert E, Tabara JD, Ridder D, Cogan V, Pahl-Wostl C (2006) Methods for stakeholder participation in water
management. Chapter 8 in Giupponi, C. Jakeman, A.J., Karssenberg, D. & Hare, M. (Eds) Sustainable management of water resources: an integrated approach.
Edward Elgar: Chichester.
Hare MP (2011) Forms of participatory modelling and its potential
/media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf
of magnitude of influence factors
• Model validation; data quality
• Parameter level: adequate estimates of parameters in selected
functions in the models
A
re
w
e
fo
cu
si
ng
o
n
th
e
rig
ht
is
su
es
?
26.8.2011Adriaan Perrels/IL 17
Uncertainty 2
• Natural science related: e.g. limitations to downscaling
of modeled future climate features, inherent chaotic
processes underlying weather & climate
/media/loftslag/Perrels-CBA.pdf
ca
ti
o
n
s
fo
r
th
e
la
rg
est
e
a
rt
h
q
u
a
ke
s
w
it
h
in
t
h
e
S
IS
Z
b
et
w
ee
n
1
7
0
6
a
n
d
2
0
0
8
d
en
o
te
d
b
y
w
h
ite
fil
le
d
c
ir
cles.
E
stim
a
te
d
f
a
u
lt
p
la
n
es
o
f
h
is
to
ric
a
l
ea
rt
h
q
u
a
ke
s
a
re
s
h
o
w
n
a
s
w
h
ite
,
th
ick
li
n
es
(
fr
o
m
R
o
th
,
2
0
0
4
).
F
a
u
lt
p
la
n
es
f
ro
m
1
9
9
8
(
V
o
g
fj
ö
rd
et
a
l.
,
2
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
Forsíðumynd: Svava Björk Þorláksdóttir mælir með öldustilli
niður á festur í Iðu í Hvítá. Ljósmynd: Njáll Fannar Reynisson.
V E Ð U R S T O F A Í S L A N D S / Á R S S K Ý R S L A 2 0 1 8
3
Viðburðaríkt ár er að baki
hjá starfsfólki Veðurstofunnar
enda felast jafnan margar og
fjöl breyttar áskoranir í vöktun
og rannsóknum á náttúru -
öflum landsins.
Loftslagsmál eru mjög á
döfinni enda stærsta
/media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf
the flood-hazard observer or the person on duty for avalanche and landslide dangers.
The Snow Avalanche Centre of the Icelandic Meteorological Office is located at Suðurgata 12, 400 Ísafjörður, tel. +(354) 450 3000.
The Akureyri branch is located at Borgir v/Norðurslóð, 600 Akureyri, tel. +(354) 4600524.
At Keflavík international airport, the Icelandic Meteorological Office runs
/about-imo/office-hours-and-location/