experiments for evaluating the effectiveness of avalanche defence structures in Iceland. Main results and future programme (pdf 0,8 Mb) (Í: Proceedings of the International Seminar on Snow and Avalanches Test Sites, Grenoble, France, 22−23 November 2002, F. Naaim-Bouvet, ed., s. 99−109, Grenoble, Cemagref, 2003, author T. Jóhannesson) [abstract] (html)
Stálgrindur eða snjóflóðanet? Val á tegund
/avalanches/imo/protective/
aversion should influence the first mover’s decision. The
98 Public Choice (2012) 151:91–119
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Public Choice (2012) 151:91–119 99
Table 1 The predicted effect of
intrinsic preferences on first and
second movers’ contributions
1st mover 2nd mover
Disadvantageous Negative None
inequity aversion
Advantageous None Positive
inequity
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
behavior as the models we would like to compare it with – Campbell,
Joyner and Boore, and Fukushima and Tanaka–despite the generally lower predictions.
Campbell's model is only valid for distances less than 50 km since his data set, of magnitude 5
to 7.7 events, consisted only of observations close to the epicenter (more than 86% were closer
than 30 km).
The theoretical relation for attenuation
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
/ design,
availability, materials, ICT,
modal split)
26.8.2011Adriaan Perrels/IL 5
Categorising stages of adaptation
Passive Adaptation
- automatic in nature
and economy
- only ex post measures
(no anticipation)
Active Adaptation
- automatic in nature
and economy
- ex ante and ex post
policies
Emission scenario dependent
baseline (A1-T, B1, A2, etc.)
Reference costs and benefits
/media/loftslag/Perrels-CBA.pdf
(). The circulation of Icelandic waters-a
modelling study. Ocean Science , –.
Nygaard, B. E. K., Hálfdán Ágústsson & K.
Somfalvi-Toth (). Modeling wet snow ac-
cretion on power lines: improvements to previ-
ous methods using years of observations.
Journal of Applied Meteorology and Climatology
(), –.
Philippe Crochet (). Sensitivity of Icelandic
river basins to recent
/media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
and CNES, n.d.;
National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional
altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein
et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea
level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
borð eru nokkrir sjómenn, talið frá vinstri: Sveinn Sveinsson, Aðalsteinn
Sveinsson, ónafngreindur, Benóný Sveinsson, Jón Guðjónsson formaður,
Sveinn Benónýsson og Eyjólfur Sveinsson. Fyrir daga Veðurstofunnar þurftu
íslenskir sjómenn að treysta á athyglisgáfu og eigið hyggjuvit ef þeir vildu
ráða í veður morgundagsins. Margir sjómenn öðluðust mikla reynslu í þeim
efnum en oft á tíðum máttu
/media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf
the
step when this appeared necessary for comparability,
and explained the substep according to the
descriptions by the authors of the guide. In the fourth
column of the author tables, we noted which
substeps in the other guides corresponded to the
substep under examination, which brings us to
reconstruction.
In three “reconstruction tables” (Appendix 2: Tables
A2-1–A2-3), we recombined the results
/media/loftslag/vonKorff_etal-2010.pdf
on the European level [e.g.
Water Framework Directive (Directive 2000/60/EC),
Common Agricultural Policy, etcetera], except for the
Ukrainian part of the Tisza. However, the Ukraine shows
strong incentives to enter the EU community and thus the
EU acquis communautaire is used as key reference for the
development of its water management principles. It was
nevertheless decided to select two case-studies
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
A (A1, A2, A3). ........................................................................................... 89
Figure B.2. Rake distribution for mapped faults/clusters in box B, Fagradalsfjall-W. ...... 90
Figure B.3. Rake distribution for mapped faults/clusters in box C, Fagdaralsfjall-E. ....... 90
Figure B.4. Rake distribution for mapped faults/clusters in box D, Kleifarvatn
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf