and on the road into the area making observation of the eruption more difficult for
the scientists in the field.
Seismic activity in Bardarbunga continues to be strong. Since Monday, the 3. of November, 200 earthquakes have
been detected in the caldera. The largest measured earthquake was on Tuesday, November 4. at 20:45 of M4,8. A
total of 15 earthquakes were of sizes between M 4 and 5; 15 of sizes
/media/jar/Factsheet_Bardarbunga_20141105.pdf
monitoring so that warnings may be issued if necessary.
Vatnajökull National Park will issue locations of viewing areas. Information on evacuation
routes will be issued by officers on site.
The
restricted area extends 20 m outside the edges of the new lava field, to the edge of
Dyngjujökull glacier on the south side, the river Jökulsá á Fjöllum to the east and to the
westernmost branches
/media/jar/Bardarbunga-2015_MarchAprMay-events.pdf
Lidar measurements of the cryosphere
Reykholt, Iceland, June 20–21, 2013
Lidar measurements
of the cryosphere
Reykholt, Iceland, June 20–21, 2013
Abstract volume
Lidar map of the ice-covered stratovolcano Öræfajökull in S-Vatnajökull, S-Iceland,
surveyed by TopScan GmbH in August 2011
Lidar measurements of the cryosphere
/media/vatnafar/joklar/Reykholt-abstracts.pdf
no
tcaus
e
mor
e
problem
si
n
th
e
(far
)futur
e
(20
year
s
o
r
more
)
Vos
s
et
al
.(
200
6),
Dub
e
an
d
Swatu
k
(200
2),
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te
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al
.(
199
7)
Alread
y
no
w
preparation
s
ar
e
take
n
fo
rth
e
(far
)futur
e
(20
year
s
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more
)
Raadgeve
re
t
al
.(
200
8),
Pahl-Wos
te
t
al
.(
2007
c),
Vos
s
et
al
.(
200
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13
.Flexibl
e
measures
,
keepin
g
option
s
ope
n
Measure
s
take
n
no
w
o
r
propose
d
fo
rth
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
deviation across the ensemble) and sign agreement (a percentage of models in the ensemble that
project the same sign of changes as the entire ensemble does).
Analysis
In Fig.1a shown are simulated changes in the annual extreme temperature range calculated
as difference between 20 yr mean absolute annual maxima and minima temperatures in baseline
and future scenario periods. The range
/media/ces/CES_D2.4_VMGO.pdf
of land origin ▲•
Undetermined or unknown x
Table 3.3
Form of ice (Fa Fb Fc Fp Fs)
Element Floe size Symbo
l
Pancake ice - 0
Small ice cake; brash ice < 2 m 1
Ice cake 2-20 m 2
Small floe 20-100 m 3
Medium floe 100-500 m 4
Big floe 500 m-2 km 5
Vast floe 2-10 km 6
Giant floe > 10 km 7
Fast ice - 8
Icebergs, growlers or
floebergs
- 9
Undetermined or
unknown
- x
- 5 -
Annex I
Sample ice charts
from
/media/hafis/frodleikur/ice-chart_colour-code-standard.pdf
the Fljótsdalsheiði region . . . . . . . 47
18 Seasonal mean wind power density within the Fljótsdalsheiði region . . . . . . . . 48
19 Directional mean wind power density within the Gufuskálar region . . . . . . . . . 49
20 Seasonal mean wind power density within the Gufuskálar region . . . . . . . . . . 50
21 Directional mean wind power density within the Hellisheiði region . . . . . . . . . 51
22 Seasonal mean
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
10:25 – 10:40
Icelandic Perspective and Hemispheric Overview (Chair: Edward Hanna)
Iceland: on the northern flank of the jet stream – T Jónsson
Circumpolar Vortex: Calculations and Correlations – P Jones
Response of the wintertime atmospheric circulation to current and projected Arctic sea ice
decline – G Magnusdottir
Group Discussion
10:40 – 11:00 Coffee Break
11:00 – 12:45
11:00 – 11:20/media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf
adaptation issues and
uncertainties with a focus on issues requiring a planning horizon of more than 20 years,
when a climate change signal could begin to dominate the natural climate variability, and
where a relatively long economic lifetime of adaptation projects makes it important to give
careful consideration to uncertainty. In Tables 2, 3, 4 and 5, climate change impacts are
characterised
/media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf