probably a few meters.
An interactive 3D model of the earthquakes during the magma
intrusion. The di?rent colours represent the activity in time from
16 August to 12 September.
During the magma intrusion, intense earthquake activity related to
subsidence of the Bárðarbunga caldera was located at the caldera
rim. Over 70 earthquakes above magnitude 5 occurred in the first
four months after the onset
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
about 28% and losses from the polar ice sheets
contributing the remainder. From 1993 to 2003 the sum of these
climate contributions is consistent within uncertainties with the total
sea level rise that is directly observed. {WGI 4.6, 4.8, 5.5, SPM, Table
SPM.1}
Observed decreases in snow and ice extent are also consistent
with warming (Figure 1.1). Satellite data since 1978 show that an-
nual average
/media/loftslag/IPPC-2007-ar4_syr.pdf
1). Over the same period, the average total number of
people reported affected2 per decade rose by 1200%, from
approximately 38 thousand to 480 thousand. Meanwhile,
the total cost of reported damage3 doubled, from US$ 1.2
billion to US$ 2.4 billion (2006 prices), although this could
partially be explained by a higher density or vulnerability
of infrastructure and areas being used by humans. More
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
Dashed lines encompass the V-shaped zone of tephra deposition. (c)
Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall
from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November.
The top portion shows its projection on an EW-vertical plane. The minimum detection height for
Grímsvötn is seen at 6 km, and the plume extends
/media/jar/myndsafn/2005EO260001.pdf
in a collaboration between the Austrian engineering company Ingenieurbüro
Illmer Daniel e.U. (DI), Efla consulting engineers and the Icelandic Meteorological Office (IMO).
Daniel Illmer carried out the analysis of landslide protection measures, Jón Kristinn Helgason,
Tómas Jóhannesson and Eiríkur Gíslason wrote sections about the geographical setting, the land-
slide history and the assessment
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
Baugur is rather mellow with only three fountains. Their maximum height was about 120 m. A geodetic specialist arrived today to measure the height of the craters. Baugur proved to be about 60 m high and its fountains 60 m above that, or around 120 m in total. Baugur's babies are still active and were boiling and murmuring throughout the day.
In general, eruptive activity has diminished and all
/about-imo/news/nr/2985
Baugur is rather mellow with only three fountains. Their maximum height was about 120 m. A geodetic specialist arrived today to measure the height of the craters. Baugur proved to be about 60 m high and its fountains 60 m above that, or around 120 m in total. Baugur's babies are still active and were boiling and murmuring throughout the day.
In general, eruptive activity has diminished and all
/about-imo/news/nr/2985/
• Methodology
• Key findings
• Conclusions
2
Forestry in Finland
1. Land area distribution 2. Species distribution
Total Forestry land 26.3 mill. ha
3. Growing stocks, increment and drain 4. Site type distribution
Source: Finnish Forest Research Institute, 2008
3
Forest management
Final felling
Timber
Energy biomass
Thinning
Timber
Pre-commercial or
energy biomass thinning
Regeneration Regeneration
4
/media/ces/Alam_Ashraful_CES_2010.pdf
and western sides of the crater
lake is a wall of ice. On the northern side a tephra wall rises 20 meters
above the water. The ice walls at the southwestern corner of the crater
are melting, i.e. at the site of the vent that was active 4 – 6 June. The
rate of melting is assumed to be about one cuber meter per second.
Seismic tremor: Low tremor level. Pulses are observed off and on.
Earthquakes
/media/jar/Eyjafjallajokull_status_2010-06-15_IES_IMO.pdf
örugt að fara fyrir Horn í um 10 sml frá landi en það yrði
að hafa góðan útvörð.
Kl.1341, kalla TFB og spyr um ETA í RVK, ETA um kl 1440.
Kl 1305, AIS umferð fyrir N- Horn. Vegna bilunnar í WS 1 var megináhersla lögð á ískönnun í
þessu flugi.
Flugskýrsla TF-SIF
12. desember 2010
Flug nr. 117410.025
Ískönnun.
Meginröndin lá um eftirtalda staði.
1. 67°47.0N 023
/media/hafis/skyrslur_lhg/Isskyrsla_20101212.pdf