York collaborated in installing a seismograph network throughout Iceland, including a network of five seismographs in the interior of the country. During the same period the number of stations in the IMO network increased markedly.
A new era of seismic monitoring began in Iceland in 1991, when a digital seismic system, the SIL system, was upgraded to fully automatic operation. It was designed
/earthquakes-and-volcanism/conferences/jsr-2009/100_years/
of Akureyri
Institute of Earth Sciences, University of Iceland
KAUST, King Abdullah University of Science and Technology
Húsavík Academic Center
Icelandic Meteorological Office
Earthquake Engineering Research Centre, University of Iceland
Civil Protection Department, National Commisioner of the Icelandic Police
Iceland Catastrophe Insurance
Husavik Academic centre
Ministry of the Interior/about-imo/news/nr/2701
-time and
detects signal characteristics similar to previously observed eruptions using a three-fold
detection procedure based on: 1) an amplitude threshold; 2) the signal-to-noise ratio; and 3) an
emergent ramp-like shape. Data from six Icelandic eruptions was used to assess and tune the
module, which can provide 10–15 minutes of warning for Hekla up to over two hours of
warning for some other
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
m
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/media/ces/2010_017.pdf
to increase in Finland by 13–26% by the 2080s (Ruosteenoja
and Jylhä, 2007) and extreme precipitations are expected to in-
crease (Beniston et al., 2007). On the other hand, temperature in-
creases of 2–6 C by the end of the century are estimated to
decrease the snow accumulation by 40–70% by the same period
(Vehviläinen and Huttunen, 1997; Beldring et al., 2006; Ruosteeno-
ja and Jylhä, 2007
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
Forms of Participatory Modelling and its Potential for
Widespread Adoption in the Water Sector
Matt Q1Hare
Durango 330, Depto 2, Roma Norte, Cuauhtemoc, Mexico D.F. 06700, Mexico
ABSTRACT
This article serves as a support for those interested in learning more about participatory
modelling and its potential for widespread adoption by resource managers. The rst part
introduces the reader to four
/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
-based and 10 based on IPCC GCM
simulations. The choice of the GCM models was based on their SAT
performance for the present-day climate near Iceland as mentioned above.
2. For GCM-based scenarios, temperature change in the highland interior of
Iceland, where the large ice caps are located, were increased by 25% based on
the results of RCM downscaling (Nawri & Björnsson, 2010).
3. Expected
/media/ces/2010_016.pdf
in other words, why should
participation be undertaken?
2. How can “good” or “effective” participation
be carried out and evaluated?
In addition, concepts and methods of stakeholder
analysis in natural resources management (Grimble
and Wellard 1997), as well as in public policy
analysis (Bryson et al. 2002), have been discussed
in detail to enable planners and policy makers to
better understand
/media/loftslag/vonKorff_etal-2010.pdf