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/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
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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
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
Twin-Otter as survey aircraft.
Lidar measurements of the cryosphere
Reykholt, Iceland, June 20–21, 2013
Guðmundsson and others 15
Post-Little Ice Age (1891–2011 AD) volume loss of Kotárjökull
glacier, southeastern Iceland, as established from historical
photography and lidar
Snævarr Guðmundsson*, Hrafnhildur Hannesdóttir and Helgi Björnsson
Institute of Earth Sciences, University
/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
the Fljótsdalsheiði region . . . . . . . 47
18 Seasonal mean wind power density within the Fljótsdalsheiði region . . . . . . . . 48
19 Directional mean wind power density within the Gufuskálar region . . . . . . . . . 49
20 Seasonal mean wind power density within the Gufuskálar region . . . . . . . . . . 50
21 Directional mean wind power density within the Hellisheiði region . . . . . . . . . 51
22 Seasonal mean
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
) ................. 89
Figure 61 Tephra accumulation rate on the ground on 8 October 1982 (Öræfajökull) ............ 90
Figure 62 Tephra accumulation rate on the ground in Skaftafell (Öræfajökull) ...................... 91
Figure 63 Preliminary intersectional map ................................................................................ 93
Figure 65 Initial user-interface of the public web-site
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf