-2B. Mon. Wea. Rev., 132, 2184–
2203.
Dickinson, R. E., Errico R. M., Giorgi F. and Bates G. T. 1989. A regional cli-
mate model for the western United States. Clim. Change, 15, 383–422.
Giorgi, F. 1990. On the simulation of regional climate using a limited area
model nested in a general circulation model. J. Climate, 3, 941–963.
Giorgi, F., and Mearns L. O. 1999. Introduction to special section
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improving
management policies and practices by learning from the
outcomes of implemented management strategies. Partici-
patory integrated assessment is here a form of problem
structuring for identification of gaps, ambiguity and
multiple frames, confrontation, and integration of the
most divergent views with respect to a given problem
situation.
Additional methods and tools that AM require com/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
and possibly the stake-
holders at different phases of the modelling project.
Many QA guidelines exist such as Middlemis (2000) and
Van Waveren et al. (1999). The HarmoniQuA project (Schol-
ten et al., 2007; Refsgaard et al., 2005a) has developed a com-
prehensive set of QA guidelines for multiple modelling
domains combined with a supporting software tool, MoST
(downloadable via http
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
the com-
plexity of the hydrological processes through modelling, but its application is usually limited to
the short-range. Although the results demonstrated a great potential for this method, its success-
ful application in real-time will strongly depend on the quality and availability of streamflow
observations, which can be poor or simply missing during periods of variable durations, e.g
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf
with maps that show:
o Dry areas
o Flood-threatened areas with shared protection (dykes, etc.)
o Flood-threatened areas with individual flood-proof buildings
o Areas exempted from future construction
o Areas where water can be stored
o Areas laid out as future storage basins
o Areas where local filtration of rainwater can take place
- Consider whether contingency plans should be prepared
/media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf
:
o Dry areas
o Flood-threatened areas with shared protection (dykes, etc.)
o Flood-threatened areas with individual flood-proof buildings
o Areas exempted from future construction
o Areas where water can be stored
o Areas laid out as future storage basins
o Areas where local filtration of rainwater can take place
- Consider whether contingency plans should be prepared for specially
/media/loftslag/Case_A___Horsens_Fjord.pdf
in a debate about
visions
- Prepare a climate change adaptation plan with maps that show:
o Dry areas
o Flood-threatened areas with shared protection (dykes, etc.)
o Flood-threatened areas with individual flood-proof buildings
o Areas exempted from future construction
o Areas where water can be stored
o Areas laid out as future storage basins
o Areas where local filtration of rainwater can
/media/loftslag/Horsens_case.pdf
that most of this volume increase occurred in
Febuary.
Geothermal activity:
o Ice cauldrons at the SE rim of Bárðarbunga are now 5-10 m deeper than they
were in late January.
o The southern ice cauldron on the western rim is similar in depth as was two
months ago, but it has grown wider. The northern cauldron on the western rim
is unchanged since January.
o An ice cauldron, which
/media/jar/Bardarbunga-2015_MarchAprMay-events.pdf
nostaa,
m utta
oh ijuoksutu
ksia tulee
Sähkönvas tus kasvaa
-> energ iahäv iö ita
Muuntajien
elinikä lyhenee
Jääkannen
m uodostaminen
h idastuu
Very likely,
the
probab ility
that the next
decade is
warmer is
90% .
Ilm iö
1 .1 – korkeammat
läm pötilat etenkin talvella
Skenario
1. Lä mpimäpi i lmasto
O ma luokitteluOma luokit te lu
Nykyiset t ai
tuleva t
varautumiskahdo
llisuudet
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