is on the northern North Atlantic and the Nordic Seas. With the southern
boundary at 47 N, the study domain covers Newfoundland, but excludes various marginal and
inland seas with significant independent storm activity, such as the Mediterranean and Adriatic
Seas, as well as the Black and Caspian Seas. The northern boundary at 80 N takes the domain
up to Fram Strait, including Svalbard, but excluding
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
and review of some methods for regional flood frequency anal-
ysis. J. Hydrol., 186, 63–84.
GREHYS. (1996b). Inter-comparison of regional flood frequency procedures for Canadian rivers.
J. Hydrol., 186, 85–103.
Grover, P.L., Burn, D.H. & Cunderlik, J.M. (2002). A comparison of index flood estimation
procedures for ungauged catchments. Can. J. Civ. Eng., 29, 734–741.
Hosking, J.R.M. & Wallis, J.R. (1993
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
to be simple and therefore has important drawbacks.
Future improvements should be made in the light of applications within a larger toolbox of scenario
methods.
2008 Elsevier Ltd. All rights reserved.
* Tel.: +31 317 482422; fax: +31 317 419000.
E-mail address: kasper.kok@wur.nl.
Contents lists available at ScienceDirect
Global Environmental Change
journa l homepage: www.e lsev ier .com/ locate
/media/loftslag/Kok_JGEC658_2009.pdf
level, surveys commissioned by the European Com-
munity/the European Union provide an indication of trends in concern about cli-
mate change. Since 1992, such surveys have been undertaken among representative
samples of citizens in its Member States, and specifically on topics related to the
environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB
in 2002). These have included
/media/loftslag/Lorenzoni_Pidgeon_2006.pdf
for ice, ocean and land applications
Snævarr Guðmundsson, Hrafnhildur Hannesdóttir and Helgi Björnsson ....................... 15
Post-Little Ice Age (1891–2011 AD) volume loss of Kotárjökull glacier, southeastern Iceland,
as established from historical photograph and lidar
Sverrir Guðmundsson, Eyjólfur Magnússon, Helgi Björnsson, Finnur Pálsson, Tómas
Jóhannesson and Etienne Berthier
/media/vatnafar/joklar/Reykholt-abstracts.pdf
wide and
1000 m long shelf called Þófi, terminating at 80–100 m a.s.l., see Map 4. The inclination of
the shelf is 15 on average. The surface of Þófi is covered with unconsolidated glacial till and
landslide deposits and marked with five gullies. The brook called Þófalækur near the middle of
the shelf divides it into an inner and outer part. On the outermost part of the shelf, there is a small
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
by the manufacturers.
Enercon E44 Vestas V80
Rotor diameter [m] 44 80
Hub height [m] 55 67
Rated power [kW] 900 2000
Cut-in speed [m s 1] 3 4
Rated speed [m s 1] 15 16
Cut-out speed [m s 1] 28 25
For any given turbine, there are three important characteristic wind speeds. The cut-in speed is the
lowest wind speed at which a turbine can generate usable power. The rated speed is the lowest wind
speed at which
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
.................... 85
8
Figure 57 50% PM10 probability map for an eruption like 1362 at Öræfajökull ..................... 86
Figure 58 The probability of exceedance curve at key locations (Öræfajökull) ...................... 87
Figure 59 Tephra accumulation rate on the ground on 7 May 1982 (Öræfajökull) ................. 88
Figure 60 Tephra accumulation rate on the ground on 5 May 1981 (Öræfajökull
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf