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
M A M J J A l
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/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
ea
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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
input is often ad hoc
and does not do justice to either the richness of the stories or the
quantitative complexity of the models. The weak link between the
qualitative and quantitative scenarios might well be the most
problematic aspect of the Story-and-Simulation methodology.
The main objective of this paper is to introduce, explain, and
illustrate the potential of a possible improvement
/media/loftslag/Kok_JGEC658_2009.pdf
very/somewhat worried about the greenhouse
effect (of these, 43% were very worried); in 19924 the percentage had increased to
89% (of these, 62% were very worried) (INRA (Europe), 1992). In 19955 public
concern was similar: 84% declared to be very/quite worried about climate change
as a global environmental threat (INRA (Europe)-ECO, 1995). By 2002 another
survey (EORG, 2002) suggested
/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