in
our analyses, as will be further outlined in the
discussion.
Among these principles, we found no direct
contradictions between the guides; our corresponding
analysis can be traced with the help of the author
principle tables, A3-1–A3-4 in Appendix 3, and the
summary table in Appendix 4, Table A4.
Nevertheless, we realized that there were tensions
between several of the principles, e.g., between P2
/media/loftslag/vonKorff_etal-2010.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
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
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