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/
at the plate boundary, leading to volcanic activity and earthquakes. The
geological units are shown on the map in Figure 1. The Western Volcanic Zone (WVZ)
encompasses the part of the rift which enters land at the western tip of Reykjanes Peninsula
(RP), runs east along the peninsula to the Hengill region, where it turns northward. East off the
Hengill region the rifting shifts approximately 90/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 are
Global Navigation Satellite System (GNSS) data providers (SONEL, n.d.).
The North Sea is home to one of the most dense tide gauge networks in the world, with over 15 tide
gauge series that span at least 100 years along its coastline (Quante and Colijn, 2016). In Denmark,
17
the national tide gauge network consists of 90 automatic stations run in cooperation of the Danish
Meteorological
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
19
61
til
19
90
(%
)
0
200
250
150
100
50
300
350
jan feb mar apr maí jún júl ágú sep okt nóv des
Úrkoma 2019
Reykjavík úrkomuhlutafall 2019 % Akureyri úrkomuhlutafall 2019 %
Vi
k h
ita
fr
á m
eð
all
ag
i 1
96
1–
19
90
(°
C)
-1
3
2
1
0
4
5
jan feb mar apr maí jún júl ágú sep okt nóv des
Meðalhiti 2019
Reykjavík hitavik 2019 Akureyri hitavik 2019
Á Slysaöldu á Mælifellssandi í nóvember 2019
/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
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