; 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
to be simple and therefore has important drawbacks.
Future improvements should be made in the light of applications within a larger toolbox of scenario
methods.
2008 Elsevier Ltd. All rights reserved.
* Tel.: +31 317 482422; fax: +31 317 419000.
E-mail address: kasper.kok@wur.nl.
Contents lists available at ScienceDirect
Global Environmental Change
journa l homepage: www.e lsev ier .com/ locate
/media/loftslag/Kok_JGEC658_2009.pdf
finished,
and possibly tested before implementation starts
(Bots 2007).
Following Bots (2007), we note that the word
“design” can denote an activity as well as a product.
In this article, design as a product is synonymous
with the participation plan (point y). This plan is
based on design as an activity, represented here by
the space between points x and y. What needs to
happen in this phase (x/media/loftslag/vonKorff_etal-2010.pdf
Barthelmie, R.J., Takle, G.S. & Andersen, T. (2008). The impact of climate change on wind energy resources. Proceedings of the World Renewable Energy Congress-X, 6pp (Invited Plenary presentation). 6pp.
Pryor, S.C., Barthelmie, R.J. & E.S. Riley (2007). Historical evolution of wind climates in the USA, Conference on the science of making torque from wind, Danish Technical University, August 2007
/ces/publications/nr/1943
was represented on the native grids of each individual
model. Therefore, the monthly means of the modelled radiation were first interpolated
onto a common 2.5 x 2.5 degree grid, and 30 year running means were applied to smooth
the influence of random interannual variability. Thereafter, anomalies from the baseline
period mean were calculated.
2
Fig. 2. Percentage change of incident global solar
/media/ces/CES_D2.4_solar_CMIP3.pdf
15.9.04
Forum 2
3.11.04
Forum 3
12.04.05
Interviews
Jan/Feb 05
Group Model Building -
Identify Problems & Measures
8
Simulation Models
Testing Solutions
Forum 1
15.9.04
Forum 2
3.11.04
Forum 3
12.04.05
KG
Feb/March 05
Interviews
Jan/Feb 05
Forum 4
15.06.05
Forum 3
12.04.05
r 5
07.09.05
Forum 4
15.06.05
9
x
Measures Costs Ecological
Efficiency
Accep-
tance
Needed
control
Further
Effects
1....
2
/media/loftslag/Hare_2-participation.pdf
with the following equation,
h = c
t
2
where c is the speed of light (c = 2.99 x 108 m/s). In principle, CL51 is able to detect three cloud
layers simultaneously, but if the cloud base is obscured due to precipitation or ground-based
fog, vertical visibility is reported. Information about fog and precipitation can also be derived
from the return signal as they attenuate the return signal from a cloud. In its
/media/vedurstofan-utgafa-2019/VI_2019_009.pdf
Clausen, N.-E., Pryor, S. C., Guo Larsén, X., Hyvönen, R., Venäläinen, A., Suvilampi, E., Kjellström, E., Barthelmie, R. (2009). Are we facing increasing extreme winds in the future? EWEC 2009 Marseille session DT2A, 19 March 2009.
Engen-Skaugen,T & Førland, E.J. (2010). Future change in return values and extreme precipitation at selected catchments in Norway, met.no Report 20/2010 (draft).
Engen
/ces/publications/nr/1680
Pálsson F., Rögnvaldsson
Ó., Sigurðsson O., Snorrason Á., Sveinsson Ó. G. B., Thorsteinsson Th. 2007.
Effect of climate change on hydrology and hydro-resources in Iceland. Rep.
OS-2007/011, National Energy Authority, Reykjavík.
Liang, X.-Z., Li L. and Kunke K. E. 2004 Regional climate model simulation
of U.S. precipitation during 1982–2002. Part I: Annual cycle. J. Climate, 17,
3510–3529.
Pálsson, F
/media/ces/Paper-Olafur-Rognvaldsson_91.pdf