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...................................................................................... 30
7 References .................................................................................................. 31
Appendix I - Identification of homogeneous groups of catchments obtained with
the ROI technique and associated growth curves .............................................. 33
Appendix II - WaSiM daily flow simulations: Best run verification for the cali-
bration
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf
Grain size distribution from heimaey 1973 eruption ..................................................... …64
D. Age of vents relative to best fit line ............................................................................... …65
E. Weight-bearing capacity of homes in heimaey .............................................................. …67
F. How to contextualize the probabilities given
/media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
Research Infrastructures themselvesdrive best practice at Volcano Observatories,link scientists and stakeholdersopen pathways for enterprise to better exploit georesources such as geothermal energy in volcanic areas.The project will exploit and build-upon existing and emerging national and pan-European research infrastructures, such as the ongoing European Plate Observing System (EPOS) and the recently
/about-imo/news/eurovolc-a-networking-project-kick-off-meeting
from Grímsvötn 2004 and
2011 indicate that the wind at the 500 hPa level, backtraced for 500 s gives the best results.
For Eyjafjallajökull 2010 this time constant was closer to 200 s.
The system has been described in posters and presentations at conferences in 2013 (Arason
et al., 2013a, b; Petersen et al., 2013).
10
Review of lightning data during previous eruptions
Prior
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf
needed.
square4 Different renewable energy sources are in different state of technological
maturity (Best deployment potential have hydro, biomass and wind,
breakthrough of solar is coming. Geothermal and ocean energy are in
developmental state.)
square4 Integration of renewable energy in existing and future energy systems is a
central challenge.
square4 In the assessment of changes, several
/media/ces/Savolainen_Ilkka_CES_2010.pdf
)
Annual
Winter
Summer
• Accounts for natural
variability and differences
between climate models
Width of the distribution primarily determined by
natural temperature variability: larger in winter than in summer.
Winter Summer Annual
Best estimate (ºC) 1.3 0.7 1.0
5-95% uncertainty range (ºC) -0.5…+3.1 -0.2…+1.6 0.0…+1.8
Probability of warming (%) 90% 90% 96%
Ref: Räisänen and Ruokolainen (2007
/media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf
)
Best case (1.5 C increase; 2%
increase in prec)
BAU A B
Change +30 % C D
Scenario
combination
Impact
Adaptation measures
North South North South
A *
CC: Possible increase in the
amount of snow more
snow clearing increase in
operational costs
S-E: increase in traffic
volume increased wear of
roads increase in
maintenance cost.
**
CC: Possibly less snow,
more rain
/media/loftslag/Group3-The-future-of-the-Finnish-national-road-network.pdf
Such landslides fall from a comparatively high
elevation, cause extensive disruption and upheaval of loose materials and soils in their
way, and can travel considerable distances uphill against opposing slopes.
Secondly, there are medium-sized or large, rapid debris flows that are released from com-
paratively high elevations and are confined to gullies as they travel down the mountain-
side, similar
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf