on the quantity at hand (strengths and weaknesses in
Box 1. The error propagation equation
The error propagation equations for the most common
operators are (s is the standard deviation):
Addition and Subtraction: z ¼ x þ yþ/ or z ¼
x y/
sz ¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
s2x
þ
s2y
þ/
r
Multiplication by an exact number: z
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.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
Systems is explained here on the Icelandic
Met Office web site.
The next meeting will be held on Tuesday 3rd of March 2015.
The National Commissioner of the Icelandic Police, Department of Civil Protection and Emergency Management
Almannavarnir www.avd.is/en Twitter: @almannavarnir
/media/jar/Factsheet_Bardarbunga_20150228.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
mix, 4) mobility patterns,
technological development, 5) equitable distribution of social goods, ethical dynamics
Background information and knowledge gaps: 1) time scale-what is the consensus view
of when are the CC impacts projected to begin to be felt, 2) spatial scale-where are the
impacts expected to occur, 3) vulnerability assessments of differential capacity to adapt
to CC impacts
/media/loftslag/Group4.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