in West-Iceland. The temperatures will become cooler.
4.12.2015 at 10:50
Forecaster on duty
Teitur Arason
Haraldur Eiríksson
Þorsteinn V. Jónsson
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/about-imo/news/nr/3245
the south and south-east of the country, where heavy sleet or rainfall will occur until early on Wednesday. According to the latest forecast, the oncoming violent storm will be far more severe than the storms in recent days.
Sunday 6.12.2015 13:30 UTC
Forecasters on duty:
Elín Björk Jónasdóttir
Teitur Arason
Haraldur Eiríksson
Þorsteinn V. Jónsson
/about-imo/news/nr/3247
Kögri. Ísinn var þunnur en svo virtist sem stöku jakar væru 10-15 sml. innan við
megin röndina.
SLAR mynd af legu íssins.
Flugskýrsla TF-SIF
11. Janúar 2012
Flug nr. 00212.025
Næst landi liggur ísinn um eftirtalda staði:
Kl.1550, ískönnun lokið.
Veður: V- 10-35 HN, létt skýjað austast en 4-6/8 ský á vestur og norðurmiðum
/media/2012/isskyrsla_2012-01-11.pdf
segir hann að þetta er dreifar og þéttur ís hjá honum, lofthiti -5°c. Staður á
LLDM er N67.12,10, W020.04,44. LLDM er á leið til Ísafjarðar til að landa rækju þar.
Eftir lendingu í Reykjavík upplýsti TFB að LLDM hefði haft samband vegna hafíss. Hafði
kl.0030 siglt framá 30-30 metra háan borgarís á stað: 67°10,45´n-020°14,7´v. Sást allvel í
ratsjá. Þéttleiki hafíss í næsta nágrenni um 3/10
/media/hafis/skyrslur_lhg/isskyrsla_14122010.pdf
and Finland. The event was located approximately 59 km SE of Piteå and 80 km NE of
Skellefteå in Sweden, while the distance to the nearest Finnish city, Raahe, was 100 km. The
earthquake was widely felt in northern Sweden and Finland, the furthest reports come from some 250
km away, with intensities up to V. The main event was followed by 6 aftershocks within the first 8
hours, and two
/media/norsem/norsem_lund.pdf
and our intention is to run these models dur-
ing times of hazardous events and even on a daily
basis to further improve monitoring.
Avalanche monitoring has progressed. The em-
phasis is now on improving our services, especially
to the Icelandic Road and Coastal Administration
with regard to transport. The reason is that com-
munity structure has changed considerably in recent
years and the need
/media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
2008)
together with a regression line through this data set and a regression line derived for a data set
of more than a hundred valley glaciers (Bahr and others, 1997). The regression lines are of the
form
v = csg ; (5)
where v and s are glacier volume and area, respectively. The coefficient and exponent for the
Icelandic ice caps are c = 0:048, g = 1:23, when the area and volume are expressed
/media/ces/ces-glacier-scaling-memo2009-01.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
-scale Category
P
e
r
c
e
n
t
a
g
e
o
f
C
a
t
e
g
o
r
y
F
a
t
a
l
i
t
i
e
s
Permanent Homes
Casualties and Timing
Casualties and Time of Day
150
200
250
I
n
d
e
x
V
a
l
u
e
Fatalities
0
50
100
Overnight Morning Early Afternoon Late Afternoon Late Evening
I
n
d
e
x
V
a
l
u
e
Injuries
Nocturnal Tornadoes
7
8
9
10
R
a
t
i
o
N
i
g
h
t
t
o
O
t
h
e
r
T
i
m
e
s
0
1
2
3
4
5
6
F0 F1 F2 F3 F4
F
/media/loftslag/Tornado_Impacts_-_FMI_Presentation.pdf