University
of Technology, Istituto Nazionale di Geofisica e Vulcanologia, Düsseldorf University of
Applied Sciences, University of Palermo, University of Cambridge, and British Geological
Survey.
18 September 2014 11:30 - from the Scientific Advisory Board
Attending: Scientists from Icelandic Met Office and the Institute of Earth Sciences University
of Iceland along with representatives from
/media/jar/Bardarbunga-2014_September-events.pdf
change. These values are not to be used for further research as they are preliminary and all rights to the data belong to the scientists who are acquiring and interpreting the data.
The participating institutions include: Icelandic Meteorological Office, Chalmers University of Technology, Istituto Nazionale di Geofisica e Vulcanologia, Düsseldorf University of Applied Sciences, University of Palermo
/earthquakes-and-volcanism/articles/nr/3001/
(ECT)
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/media/ces/Alam_Ashraful_CES_2010.pdf
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/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
; University of Iceland
5.8.2014
_____________________________________________________
In the evening of 21 July 2014, a large rockslide occurred in Askja, which descended into the
caldera lake (Lake Öskjuvatn). The slide was released from the southeastern caldera wall in
an area called “Suðurbotnar”. It is one of the largest known rockslides since the settlement of
Iceland. The slide covered
/media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf
In the evening of 21 July 2014, a large rockslide occurred in Askja, which descended into the caldera lake (Lake Öskjuvatn). The slide was released from the southeastern caldera wall in an area called “Suðurbotnar”. It is one of the largest known rockslides since the settlement of Iceland. The slide covered most
/avalanches/articles/nr/2929
; from which
extensive data streams enter IMO and are utilized
for forecasts and research purposes.
Dissemination
The main dissemination of IMO is in the form of
forecasts and warnings; through radio, T V, direct di-
alog with stakeholders and through IMO‘s web-site
(vedur.is). Additionally, the web provides compre-
hensive real-time data on the weather, earthquakes
and deformation, as well
/media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
) and Jónsdóttir (2008).
Therefore, comparison of measured and simulated water balance cannot be di-
rectly used for validation of the model-generated precipitation. According to the
non-scaled MM5 output for the period 1961–1990, mean precipitation for the
whole of Iceland was 1790 mm y−1. After scaling the precipitation, this value
was reduced to 1750mm y−1, i.e. by approximately 2%. This difference
/media/ces/Paper-Olafur-Rognvaldsson_92.pdf
of the lake before the eruption (according to Digital Terrain Model, DTM, from ISOR).
Ice tunnel in Gígjökull
Gígjökull 11 June 2010: an ice tunnel can be seen above the main canyon in the palagonite. Another canyon has formed to the west. Photo: Emmanuel Pierre Pagneux.
Assessment - 17 June 2010 10:00
There is a wall of ice at the eastern, southern and western sides of the crater lake
/earthquakes-and-volcanism/articles/nr/1884