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the com-
plexity of the hydrological processes through modelling, but its application is usually limited to
the short-range. Although the results demonstrated a great potential for this method, its success-
ful application in real-time will strongly depend on the quality and availability of streamflow
observations, which can be poor or simply missing during periods of variable durations, e.g
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf
of the data and the state
of the instruments that are still running is in many cases not known. The Reykjavík series from the
old harbour is the only one known to be of good quality (not only for some periods) (ibid.), even
though more frequent calibrations would have been needed there too and it is unclear how it is best to
calibrate the instrument since 1994 (Tryggvason, 2017). Proposals of a new sea
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
from this run are shown in Fig. 12.
that best simulated the measured glacier geometry. The
rate factor (A) calibrated in this manner is on the order of
6× 10−15 s−1 kPa−3; a value that has been recommended for
temperate ice (Paterson, 1994), but characterizes softer ice
than the average of a series of model calibrations that is now
recommended (Cuffey and Paterson, 2010). Here, two ap-
proaches
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
with 20% and 2% for the HIRHAM experiments
using HadAM3H and with 30% and 7% for the ECHAM-
driven experiments for Middle Europe and Scandinavia,
respectively.
[18] RCM output is not available for the entire period
1961–2100 because transient RCM simulations are com-
putationally very demanding. Instead two 30-year time
slices are available; one representative for the climate in
the period 1961–1990
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
research.
The town of Ísafjörður stands on a narrow spit in the fjord Skutulsfjörður, which meets the waters of the larger fjord Ísafjardardjúp. The town is surrounded by mountains, best seen from sea, and when the group enjoyed a sailing tour, a humpback whale honoured the guests with its presence although it escaped the camera. The small island of Vigur was visited. The photos below were taken
/about-imo/news/nr/2736
At this rate, the lava flow will soon be larger than any seen for more than two centuries in the volcanically active island nation. And there's no telling when it will stop—months, maybe, or years.“
„Despite its remoteness, the Holuhraun eruption is one of the best monitored in history, thanks to new instruments deployed by the European Commission-funded FUTUREVOLC project and other international teams
/about-imo/news/nr/3003
is intended to monitor the long term development in deformation around Bárðarbunga. After the eruption in Holuhraun began, GPS stations around Bárðarbunga have been showing continuous displacements towards its caldera (a subsidence signal). Since then, the rate of subsidence has been slowly decreasing. These changes in displacement velocities are very slow and can best seen by looking at a longer time
/about-imo/news/nr/3074
of travellers in Iceland. Alongside weather information, details are also available about earthquake activity in Iceland.
Recently, the Icelandic version of our site received an award from the Society for Icelandic Web Industry, SVEF, for the best web-site in public service during 2007.
Our web-site has achieved accessibility certification based on WAI (Web Accessibility Initiative) from Sja ltd
/about-imo/news/nr/1238
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/about-imo/news/nr/1302
of travellers in Iceland. Alongside weather information, details are also available about earthquake activity in Iceland.
Recently, the Icelandic version of our site received an award from the Society for Icelandic Web Industry, SVEF, for the best web-site in public service during 2007.
Our web-site has achieved accessibility certification based on WAI (Web Accessibility Initiative) from Sja ltd
/about-imo/news/nr/1238/