), Norway
Finnur Pálsson, Institute of Earth Sciences, University of Iceland
Gro Birkefeldt Møller Pedersen, Nordic Volcanological Center, Department of Earth Sciences, University of Iceland
Peter Rieger, RIEGL Laser Measurement Systems GmbH, Austria
Robert Ricker, Alfred Wegener Institute for Polar and Marine Research, Germany
Ciaran Robb, Scott Polar Research Institute (SPRI
/lidar/lidar-2013/participants/
distribution will in practice not alter the obtained total ice volume much in comparison to the
overall uncertainty of the procedure.
Delayed response of the ice-covered area
The coloured curves in Figure 1, showing simulated volume and area for three retreating Ice-
landic ice caps with a shallow ice approximation ice flow model, demonstrate that the response
of the ice-covered area to ice volume
/media/ces/ces-glacier-scaling-memo2009-01.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
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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
Number
Faxaflói1Breiðafjörður0West fjords0North West0North East0Eastern coastal area0East fjords0South East 0South0Central highlands0
Total:1
Last 24 hours
Region
Number
/avalanches/notifications/
The project will be organized as a matrix structure with work groups, WG, on the renewable energy resources. Cross-cutting issues are also delegated to WG. These WG will be supported and served by a Steering group with one representative from each of the partners. An Information management group will be responsible for information dissemination, active stakeholder involvement and the public outreach
/ces/project/
methodology is widely utilized by many automatic earthquake detectors, but instead of having
window lengths on the order of minutes, like the ALERT module, they have window durations
on the order of seconds. A longer STA window duration will make the module less sensitive to
small signals (Trnkoczy, 1999). Additionally, the total duration of the STA and LTA windows
may not exceed 24 hours
/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
• 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