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Dashed lines encompass the V-shaped zone of tephra deposition. (c)
Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall
from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November.
The top portion shows its projection on an EW-vertical plane. The minimum detection height for
Grímsvötn is seen at 6 km, and the plume extends
/media/jar/myndsafn/2005EO260001.pdf
inty in decision making linking pluriform uncertainty combining certified and tacit knowledge
Tommy Chan Mich el Laiho Patrick Driscoll Kare Lundgren Hector Guin a Barrientos
Eivind Junker Jussi Ylhäisi Athanasios Votsis
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/media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
with 20% and 2% for the HIRHAM experiments
using HadAM3H and with 30% and 7% for the ECHAM-
driven experiments for Middle Europe and Scandinavia,
respectively.
[18] RCM output is not available for the entire period
1961–2100 because transient RCM simulations are com-
putationally very demanding. Instead two 30-year time
slices are available; one representative for the climate in
the period 1961–1990
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
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Catchment
/media/ces/Lawrence_Deborah_CES_2010.pdf
example
can be given by the low cost still flood risk adaptation by implementing early warning system. But
there is one more suggestion dfor stakeholders to restrict infrastructure in the cities of Horsens.
Fiva PhD Courses : Adaptive management in relation to climate change (august 22 2011 - august 26 2011)
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/media/loftslag/Group-1_Scenarios-for-AWM.pdf
; fax: +358 20 490 2590.
E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen).
Journal of Hydrology 391 (2010) 333–350
Contents lists available at ScienceDirect
Journal of Hydrology
journal homepage: www.elsevier .com/ locate / jhydrol
Author's personal copy
narios from GCMs or RCMs, and with different emission scenarios
(e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
performance of the
model.
REFERENCES
Førland, E. J., Allerup P., Dahlström B., Elomaa E., Jónsson T., Madsen H.,
Perälä J., Rissanen P., Vedin H. and Vejen F. 1996. Manual for operational cor-
rection of Nordic precipitation data. DNMI Report No. 24/96 Klima, 66 pp.
Benoit, R., Pellerin P., Kouwen N., Ritchie H., Donaldson N., Joe P. and Soulis
E. D. 2000. Toward the use of coupled atmospheric
/media/ces/Paper-Olafur-Rognvaldsson_92.pdf
/$ - see front matter 2007 Elsevier Ltd. All rights reserved.
doi:10.1016/j.envsoft.2007.02.004
odelling process e A framework
e
an der Sluijs b, Anker Lajer Højberg a,
eghem c,dd (GEUS), Copenhagen, Denmark
, Department of Science Technology and Society,
, The Netherlands
e 22 (2007) 1543e1556
www.elsevier.com/locate/envsoft
the pursuit of the objectives of preserving, protecting and im-
proving
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf