out, adding to the results and making them more precise. Below are photographs, maps and graphs that show the main results of measurements and analyses that are available, now two weeks after the event.
Width of fracture line: 800 m
Vertical drop: 350 m
Runout length beyond the lake shore: ~1000 m
Volume: ~30–50 million m³
Estimated duration of the slide: 20 seconds according to seismographs
/avalanches/articles/nr/2929
Fjölbrautaskólanum við Ármúla
Kristín S. Vogfjörð, Veðurstofu Íslands
VÍ 2009-012
ISSN 1670-8261
Skýrsla
+354 522 60 00
+354 522 60 06
vedur@vedur.is
Veðurstofa Íslands
Bústaðavegur 9
150 Reykjavík
5
Project no. 036935
Project acronym: SAFER
Project title: Seismic eArly warning For EuRope
Instrument : Specific Targeted Research Project
Thematic Priority: Sustainable development
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
line shows the seismic moment released in the dyke intrusion south of the Holuhraun eruption site, the blue line represents the moment released in or around the caldera. The lower plot shows the magnitudes of the earthquakes as a function of time, blue for the caldera and orange for the dyke
/about-imo/news/on-the-bardarbunga-earthquakes
is shown in three frequency bands (0,5-1 Hz; 1-2 Hz; 2-4 Hz).
A low frequency tremor pulse is clearly seen just before noon 23rd August. This tremor (red line) was interpreted as signs of magma having arrived at the surface under the glacier and prompted IMO to raise the aviation colour code from orange to red. The tremor lasted a few hours and then gradually decreased during the afternoon
/earthquakes-and-volcanism/articles/nr/2970
-resources. The mission of EPOS-Norway is therefore in line with the European vision of EPOS.
EPOS-Norway project has started in January 2016 and will during the next five years focus on the
implementation of the three main components. These are: (i) Developing a Norwegian e-Infrastructure
to integrate the Norwegian Solid Earth data from the seismological and geodetic networks, as well as
the data
/media/norsem/norsem_atakan_norway.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
from 5
years of continuous GPS measurements in
Iceland, submitted to Journal of Geophysical
VOLUME 86 NUMBER 26
28 JUNE 2005
PAGES 245–252
Eos, Vol. 86, No. 26, 28 June 2005
EOS, TRANSACTIONS, AMERICAN GEOPHYSICAL UNION
PAGES 245, 248
Forecasting and Monitoring a
Subglacial Eruption in Iceland
Fig. 1. (a) Map of Iceland illustrating the location of monitoring networks discussed in the text
/media/jar/myndsafn/2005EO260001.pdf
mode ................................................... 14
5 Errors associated with SURFEX .................................................................... 15
6 Statistical correction of model results .............................................................. 19
7 Original and corrected 2-m air temperature .................................................... 22
8 Original and corrected 10-m
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
improving
management policies and practices by learning from the
outcomes of implemented management strategies. Partici-
patory integrated assessment is here a form of problem
structuring for identification of gaps, ambiguity and
multiple frames, confrontation, and integration of the
most divergent views with respect to a given problem
situation.
Additional methods and tools that AM require com/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf