were carried out to obtain the flow and
sliding parameters for Hoffellsjökull that resulted in a good
simulation of the observed 20th century evolution of the
glacier geometry. The obtained values for the rate factor
and the sliding parameter are A= 4.6× 10−15 s−1 kPa−3 and
C = 10× 10−15 m a−1 Pa−3, respectively.
The ice divide is kept at a fixed location in the model com-
putations presented here
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
- Instantaneous Index flood models for Region 2.......................... 44
Appendix IX - Comparison between reference and estimated instantaneous index
floods for Region 1........................................................................................ 45
Appendix X - Comparison between reference and estimated instantaneous index
floods for Region 2
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf
is based on Moho reflections from the location marked by the X (Vogfjörd et
al., 2002).
11
Figure 2. Upper: Cumulative number of earthquakes in and near to Eyjafjallajökull.
Lower: Magnitude distribution (local moment magnitude scale, Mlw).
1.2 Seismic activity and deformation of the volcano
The number of detected earthquakes in Eyjafjallajökull has risen substantially since
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf
of Geophysical Research, 108(D3), 4124, doi:10.1029/2002JD002287.
IPCC (2001), Climate change 2001: the scientific basis. Contribution of working group I to the
third assessment report of the intergovernmental panel on climate change. (eds. Houghton,
J. T. , Y. Ding, D. J. Griggs, M. Noguer, P. J. van der Linden, X. Dai, K. Maskell and C.
A. Johnson), Cambridge University Press, Cambridge, UK
/media/ces/ces_geus_paakitsoq_full_report.pdf
flood-threatened areas (from watercourses,
lakes and sea) and flood-proof areas
- If possible, make a map showing risks Risk = damage extent x probability
- Using the above-named maps, a vision plan should be prepared at a regional and municipal
level In connection with this, consider how interested parties can be involved in a debate about
visions
- Prepare a climate change adaptation plan
/media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf
areas (from watercourses,
lakes and sea) and flood-proof areas
- If possible, make a map showing risks Risk = damage extent x probability
- Using the above-named maps, a vision plan should be prepared at a regional and municipal
level In connection with this, consider how interested parties can be involved in a debate about
visions
- Prepare a climate change adaptation plan with maps that show
/media/loftslag/Case_A___Horsens_Fjord.pdf
for reviewing:
- Make if possible a factual theme map that shows flood-threatened areas (from watercourses,
lakes and sea) and flood-proof areas
- If possible, make a map showing risks Risk = damage extent x probability
- Using the above-named maps, a vision plan should be prepared at a regional and municipal
level In connection with this, consider how interested parties can be involved
/media/loftslag/Horsens_case.pdf
at the operational/local level.
A calibrated approach (standardized questionnaires and
interviews, expert judgment, and reinterpretation of out-
comes by means of relevant literature) was used to com-
pare the state of affairs in water management in the
selected case-studies.
Adaptive and integrated water management
Given the expected increase of climate-related extreme
events, water governance capabilities
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf