et al.
3
2005
Seismic hazard in the Hengill area based on the SIL earthquake catalogue - First results (PDF)
Kristján Ágústsson, Páll Halldórsson
42
0,8
2005
A model of the release of the two June 2000 earthquakes based on all available observations (PDF)
Sigurlaug Hjaltadóttir, Kristín S. Vogfjörð, Þóra Árnadóttir, Páll Einarsson, Peter Suhadolc
8
8,2
2005
/earthquakes-and-volcanism/reports-and-publications/
and Reykjavík.
The fault on which the earthquake occurred is the same fault that gave rise to a magnitude 7 earthquake in August 1784.
Yesterday's earthquake was not preceded by foreshocks and only a few aftershocks have been detected. This is the largest earthquake in this area since 2000, and the largest in the South Iceland lowland region (South Iceland seismic zone) since 2008.
It is possible
/about-imo/news/nr/2888
) and
other gases
A wide spectrum of measures needed in order to reach deep enough emission
reductions
503/02/2010
Global greenhouse gas emissions
by sectors in 2005
The emissions sum up to approximately 46,000 MtCO2eq.
Data source: CAIT, cait.wri.org. *) The estimated effect of land use change &
forestry, 8,000 MtCO2, is for the year 2000.
603/02/2010
Raupach et al 2007; Le Quere et al. 2009
/media/ces/Savolainen_Ilkka_CES_2010.pdf
over five-day period in Iceland. Several
landslides hit the town of Seyðisfjörður during these days, the
largest on 18 December. It ranks as the most damaging landslide to
have affected an urban area in Iceland.Table
2: Precipitation overview
2020 from several stations. (1) Total precipitation (mm). (2)
Percentage of the 1971 to 2000 average precipitation. (3) Percentage
of the 10-year
/about-imo/news/the-weather-in-iceland-in-2020
with precipitation was considerably higher than the
normal in both
Reykjavík and Akureyri.
Table
2: Precipitation
overview 2018 from several
stations. (1)
Total precipitation (mm). (2) Percentage of the 1971 to 2000 average
precipitation. (3) Percentage of the 10 year average precipitation
(2008-2017). (4) Maximum 24-hr precipitation. (5) Number of
precipitation days. (6) Number
/about-imo/news/the-weather-in-iceland-in-2018
using data from six recent
Icelandic eruptions: Hekla 2000, Eyjafjallajökull 2010, Fagradalsfjall 2021, and Grímsvötn
1998, 2004, and 2011. For tuning, data for these eruptions had to be converted from IMO’s old
in-house RSAM data format to the new Tremv csv format. In addition to developing the
ALERT module, this project involved several updates to the original Tremv program.
Figure 2/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
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1.3 The June 2000 earthquakes
The large ML 6.4 earthquake on 17 June occurred
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
.............................................................................................................................72. Real time estimation of earthquake magnitudes based on dominant frequency in
p waves (elarms) ..................................................................................................................29
3. Intensity vs. Peak ground acceleration (pga) and peak ground velocity (pgv) in
SW-Iceland
/media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf
in the seismicity pattern in connection with the observed crustal deformation
which accompanied the 1994 and 1999–2000 swarms. From the nine earthquakes detected
in the area in 1991, only three are located within the central part of the volcano, and five
beneath the western slopes of the volcano (Figure 4). In May 1992 detected seismicity
started to increase steadily (Figure 2) and one ~Mlw3
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf