mean surface air temperature anomalies ....................................... 28
14 Surface air temperature anomalies over Scandinavia ...................................... 29
15 Composite mean precipitation anomalies..................................................... 30
6
1 Introduction
Extratropical low-pressure systems, persisting for at least a few days, have long been recognised
as one
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
of homogeneous groups of catchments obtained with
the ROI technique and associated growth curves .............................................. 26
Appendix II - Index flood estimation at gauged sites treated as ungauged. ............ 29
5
6
1 Introduction
Flood frequency analysis is a prerequisite in flood risk assessment studies and for the design
of various hydraulic structures. Often, flood quantile
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
it will be one of the main aspects
of this paper.
2.3. Properties
The elements of a Fuzzy Cognitive Map are as follows:
Concepts: C1, C2, . . ., Cn. These represent the drivers and
constraints that are considered of importance to the issue under
consideration.
State vector: A = (a1, a2, . . ., an), where ai denotes the state of the
node Ci. The state vector represents the value of the concepts
/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
................................................................. 25
6 Analog hazard situations in the Alps and implemented or planned mitigation
measures..................................................................................................... 29
6.1 Kerschbaumsettlement/Navis.................................................................... 29
6.2 Gschliefgraben
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
visibility are not included, containing 1467 records.
34
0%
20%
40%
60%
80%
0 5 10 15 20
Visibility [km]
Propo
rtion of record
s
0%
1%
2%
3%
0 5 10 15
Visibility [km]
Propo
rtion of record
s
Figure 29. Records from the automatic station. The figure to the right is the visibility
without the most frequent value.
0%
10%
20%
30%
−20 −15 −10 −5 0 5 10 15 20
Mismunur [km]
Propo
rtion of record
s
Figure 30
/media/vedurstofan-utgafa-2019/VI_2019_009.pdf
. . . . . . . . . . . 56
27 Directional mean wind power density within the Langanes region . . . . . . . . . . 57
28 Seasonal mean wind power density within the Langanes region . . . . . . . . . . . 58
29 Directional mean wind power density within the Meðallandssveit region . . . . . . 59
30 Seasonal mean wind power density within the Meðallandssveit region . . . . . . . 60
31 Directional mean
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf