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/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
for Iceland were made. The CE
project used an ensemble of six GCMs and RCMs from the PRUDENCE project for four different
emissions scenarios (B1, B2, A2, and A1FI) developed by the Intergovernmental Panel on Climate
Change (IPCC). The GCMs used by the CE project showed more warming during winter than
summer. During winter, the median projected warming from 1961–90 to 2070–99 ranged from
3–6 K, and from 2
/media/ces/2010_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
................................................................................................................................... 88
Melvold, K. and Laumann, T.
A coupled mass-balance and ice-flow model for Midtdalsbreen; projection of glacier length based on climate
scenarios (CES) ..................................................................................................................................................... 90
Thorsteinsson, Th., Sigurðsson, O. and Einarsson, B.
Monitoring changes
/media/ces/ces-oslo2010_proceedings.pdf
Discrete
numerical
Categorical Narrative
Constant in space and time A1 A2 A3
4Varies in time, not in space B1 B2 B3
Varies in space, not in time C1 C2 C3
It is noticed that the matrix is in reality three-dimensional
(source, type, nature). Thus, the categories type and nature
are not mutually exclusive, and it may be argued that the ma-
trix should be modified in such a way that the two uncer
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.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
–8% likelihood that a vent will open on Heimaey. In other words, there is a 92–97% likelihood
that the next eruption within the volcanic system will not be on Heimaey. The most densely
populated parts of Heimaey in the north and around the harbor are the most vulnerable to
Moderate and Large lava flows originating on the island. Almost all infrastructure on the island
is vulnerable to lava
/media/vedurstofan-utgafa-2020/VI_2020_011_en.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