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/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
Interpreting the dynamic output
3.2.1. The current situation
After about 20 iterations, the value of all concepts has stabilised
in the graph that represents the current situation (top left of Fig. 4).
The new equilibrium reflects the current situation of deforestation
in the Amazon, with a high value for agricultural expansion
(C6 = 1.4). Land titling issues (C1 = 0.8); infrastructure expansion
(C2/media/loftslag/Kok_JGEC658_2009.pdf
Lidar measurements of the cryosphere
Reykholt, Iceland, June 20–21, 2013
Lidar measurements
of the cryosphere
Reykholt, Iceland, June 20–21, 2013
Abstract volume
Lidar map of the ice-covered stratovolcano Öræfajökull in S-Vatnajökull, S-Iceland,
surveyed by TopScan GmbH in August 2011
Lidar measurements of the cryosphere
/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
approximately centred around Iceland: the outer domain with
43 42 grid points spaced at 27 km (1134 1107 km), the intermediate domain with 9590 grid
points spaced at 9 km, and the inner domain with 196 148 grid points spaced at 3 km. The
northwest corner of the outer domain covers a part of the southeast coastal region of Greenland.
Otherwise, the only landmass included in the model domain
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
& Höskuldsson, 2008; Thordarson & Larsen,
2007). Highly active volcanic systems as Hekla, Katla, Bárðarbunga and Grímsvötn, have
explosive eruptions rates of 82%, 97%, 90% and 95%, respectively (Gudmundsson & Larsen,
2016; Larsen & Gudmundsson, 2016b, 2016a; Larsen & Thordarson, 2016). Volcanic eruptions
are quite common in Iceland and occur on average every two to five years (Larsen & Eiríksson
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf