ANN−10
−5
0
5
10
15
20
delta w (%
)
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17C
h
a
n
g
e
i
n
g
e
o
s
t
r
o
p
h
i
c
w
i
n
d
s
p
e
e
d
(
%
)
Change in wind over the Baltic Sea in 70 years time at the time of CO2-doubling
Chen and Aschberger, 2006
17
CM
IP
G
CM
s
A need for regional ensemble simulations
head2right Changes are uncertain
head2right Size and sometimes even sign
/media/ces/Kjellstrom_Erik_CES_2010.pdf
of
Eyjafjallajökull, at approximately 5-7 km depth. The high velocity zones are elongated in the east-west direction, in
line with geological surface features and are separated by a zone of relatively lower velocity (3.0 km/s), where
earthquakes prior to and during the 2010 summit eruption were located. The high velocity zones most likely
correspond to intrusive bodies similar to those previously imaged
/media/norsem/norsem_asdis.pdf
reduction scenarios for limiting the emission by 50% and by 85%
corresponding the overlimit emissions and underlimit emission for
a temperature rise level of 2 C.
903/02/2010
WEO 2009
1003/02/2010
IPCC Special Report on Renewable Energy Sources
and Climate Change Mitigation (SRREN)
1) Introduction (Renewable energy and climate change) (5% share of the
whole report)
2) Bioenergy (15 %)
3) Direct
/media/ces/Savolainen_Ilkka_CES_2010.pdf
as the volume of the lava field at Holuhraun. The red
dotted line is an exponential curve used to estimate the diminishing flow of lava from the Holuhraun eruption and estimate when the lava flow
will go below 5 m3/s. If the diminishing activity follows this trend then the eruption might come to an end anywhere between June 2015 and
April 2016.
NATIONAL COMMISSIONER OF THE ICELANDIC POLICE
/media/jar/Factsheet_Bardarbunga_20150130.pdf
Peninsula, between Fagradalsfjall and
Kleifarvatn - the largest of which was a magnitude
5.6 earthquake in the vicinity of Núpshíðarháls, which occurred at 13:43 on
20th October. The maps displayed here show ground deformation associated with
movement on faults during the period 16th-22nd October.The large signal shown
in the vicinity of Skolahraun represents movement of up to 5 cm
/about-imo/news/satellite-images-show-significant-ground-deformation-associated-with-earthquake
shows the direction of the wind, which blows toward the point of the barb. Wind-speed is symbolized by diagonal lines at the end of the barb; for instance, a short line represents 2.5 m/s, a long line5 m/s and a triangle represents 25 m/s.
Mean sea level pressure is shown in solid lines, the contour interval is 2 hPa.
The sliding bar below the map is used to change the validity time
/weather/articles/nr/1211
forcings. Decadal averages of observations are shown for the period 1906-2005 (black line) plotted against the
centre of the decade and relative to the corresponding average for the 1901-1950. Lines are dashed where spatial coverage is less than 50%. Blue shaded
bands show the 5 to 95% range for 19 simulations from five climate models using only the natural forcings due to solar activity
/media/loftslag/IPPC-2007-ar4_syr.pdf
is N197°E. The J21 fault, on the other hand, is more
linear but with varying dip. South of the epicentre the fault is vertical but north of it, dip
changes to 77°. It is 15.5 km long, strikes N179°E and deepens to the south from 6 km to 9
km. Many other smaller faults in Southwest Iceland that were illuminated by the 2000
activity have also been mapped, including the fault planes of three M~5/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
East and Up components
over the period 27 July – 2 September 2021. The station, which is located close
to the center of the inflating area, shows that the uplift started between the
end of July and beginning of August (mainly visible in the Up component) and it
is still ongoing (2. Sept 2021). The dashed red line indicates the rise speed
that is assessed to be ~5 cm /month
/about-imo/news/uplift-signal-detected-in-askja-volcano
– 1987, bottom). The vertical red lines indicate
the start date of the melt season as retrieved by the first filtering method.
13
Figure 5 – Evolution of the snowpack (black line), cumulative melting (dashed blue
line), and daily runoff (grey bars) for Hágöngulón (year 1986 – 1987, top; year 1984 –
1985, bottom). The vertical red lines indicate the start date of the melt season
/media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf