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-SAR's office leads the project with the help of many SAR team members as well as others with thorough experience in travelling in Iceland in different conditions. Safetravel is supported by a number of sponsoring companies.
112 Iceland app
An option is 112 Iceland, an app which is easy to use. It can be used in emergency, if an accident occurs or if someone is lost. Tourist can also leave
/about-imo/news/nr/2878
night and day, all year round.
112 Iceland app
Safetravel provides 112 Iceland, an app which is easy to use. It can be used in emergency, if an accident occurs or if someone is lost. Tourist can also leave their "trail" in case of search. From Safetravel's web-site, the app can be downloaded for either Android phones, Windows phones or iPhone:
First of all you can call for help by pressing
/about-imo/news/nr/3220
-corrected SPOT 5
high-resolution geometric (HRG) images with 2.5 m
2.5 m spatial resolution, acquired in the autumn 2003
and (4) airborne polarimetric synthetic aperture radar
images observed simultaneously to the 1998 EMISAR
images and the EMISAR DEM viewed as a shaded
relief image (Magnu´sson et al. 2005b).
We estimate the average specific net mass balance (in
m yr1 w. eq.) as
bn r
DV
A1 N
/media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
); new long-term investment strategy prioritizing low- or zero-net carbon forms of
mobility
2040 Modal shift in logistics chains, especially within heavy industry.
3.3 Backcasting scenario narrative
Low-Impact Mobility Project Evaluation (LIMPE)
Climate change is occurring. Is it natural or anthropogenic? It doesn’t matter. Even
though the future is inherently uncertain, one certainty
/media/loftslag/Group4.pdf
). NeWater is based on the
hypothesis that IWRM cannot be realised unless current
management regimes undergo a transition towards more
0301-4797/$ - see front matter r 2007 Elsevier Ltd. All rights reserved.
doi:10.1016/j.jenvman.2007.05.009
Corresponding author. Tel.: +45 38 14 27 71; fax: +45 38 14 20 50.
E-mail address: hjh@geus.dk (H.J. Henriksen).
(Downing et al., 2005). Vulnerability
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
August 2014 07:10 - from geoscientist on duty
Seismic activity has decreased as a result of the pressure release, however a significant amount of earthquakes is still detected in the magma dike, between the eruption site and south to about 5 km into Dyngjujökull.
Strongest events were 3.8 in the caldera of Bárðarbunga at 04:37, as well as 2.9 at 05:39 and 3.5 at 06:38 in the dike. These earthquake
/earthquakes-and-volcanism/articles/nr/3000
the eruption site and south
to about 5 km into Dyngjujökull.
Strongest events were 3.8 in the caldera of Bárðarbunga at 04:37, as well as 2.9 at 05:39 and
3.5 at 06:38 in the dike. These earthquake are very closely monitored, but no significant
change volcanic activity following these has been observed so far.
Web camera from Míla shows the area. Míla's background photo has nothing to do
/media/jar/Bardarbunga-2014_August-events.pdf
August 2014 07:10 - from geoscientist on duty
Seismic activity has decreased as a result of the pressure release, however a significant amount of earthquakes is still detected in the magma dike, between the eruption site and south to about 5 km into Dyngjujökull.
Strongest events were 3.8 in the caldera of Bárðarbunga at 04:37, as well as 2.9 at 05:39 and 3.5 at 06:38 in the dike. These earthquake
/earthquakes-and-volcanism/articles/nr/3000/