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/
/ 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
.................................................. 36
?Veðurstofa Íslands 2020
Bústaðavegi 7–9, 105 Reykjavík
ISSN 2251-5607
Efni ársskýrslunnar var unnið af starfsmönnum
Veðurstofu Íslands
Ritstjórn: Haukur Hauksson og Sigurlaug
Gunnlaugsdóttir
Hönnun og umbrot: Ennemm
Prentun: Svansprent
Forsíða: Úr árlegri ferð Jöklarannsóknafélagsins og
vísindamanna á Vatnajökul. Hér á Bárðarbungu í júní
2019.
Ljósmynd
/media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf
As a second stage of our method, to find a more
robust core for a potentially new design guide we
deconstructed, compared, and reorganized the
various steps and principles of the five guides. We
proceeded as follows:
For each author, we created “author tables”
(Appendix 1: Tables A1-1–A1-5) based on
substeps. In these tables we listed the step as
originally named by the author, deconstructed
/media/loftslag/vonKorff_etal-2010.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
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
................ 91
Figure B.5. Rake distribution for mapped faults/clusters in boxes E and F,
Brennisteinsfjöll-Bláfjöll. ................................................................................. 92
Figure B.6. Rake distribution for mapped faults/clusters in box G, Ölfus. ......................... 93
Figure B.7. Rake distribution for mapped faults/clusters in box H, Hengill, active
between January
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf