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
The Rhine River Basin
The Rhine basin (Fig. 3) covers an area of approximately 185,000 km2, distributed between
nine countries. Two third of the basin is located in Germany, whereas the alpine countries of
which Switzerland is the most important form 20% of the area (Buck et al. 1993). With its
1,320 km, of which 880 km is navigable, the Rhine is one of the longest rivers in Europe
(Frijters
/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
Av. Ed.
Belin, 31400 Toulouse, France
Received: 21 March 2011 – Published in The Cryosphere Discuss.: 6 April 2011
Revised: 5 October 2011 – Accepted: 20 October 2011 – Published: 2 November 2011
Abstract. The Little Ice Age maximum extent of glaciers in
Iceland was reached about 1890 AD and most glaciers in the
country have retreated during the 20th century. A model for
the surface mass balance
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
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/media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf
ISBN 978-9979-68-238-7. NHP Report No. 50, P. 638-645.
Kriauciuniene J. & Kovalenkovienė M. (2008). Dependence of Lithuanian river runoff extremes on atchment area. XII Biennal International Conference. Hydrological extremes in small basins, 18-20 September, 2008, Cracow, Poland. ISBN-978-83-88424-38-0. P.183-186.
Kriauciuniene, J., Kovalenkovienë, M., and Meilutytë-Barauskienë D. (2007). Changes
/ces/publications/nr/1943
im-
proved by a double-difference location meth-
od [Slunga et al., 1995], and supported by P -
wave particle-motion analysis at GRF, reveal a
northerly trending event distribution, centered
at the southern caldera rim, ~1 km east of the
main eruption site (Figure 1b). Focal depths
mostly concentrate above 4 km and decrease
by ~2 km near the eruption onset.
The detection threshold
/media/jar/myndsafn/2005EO260001.pdf
aversion should influence the first mover’s decision. The
98 Public Choice (2012) 151:91–119
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Public Choice (2012) 151:91–119 99
Table 1 The predicted effect of
intrinsic preferences on first and
second movers’ contributions
1st mover 2nd mover
Disadvantageous Negative None
inequity aversion
Advantageous None Positive
inequity
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
kg/s. Plume compo-
sition measurements were made by FTIR, MultiGAS and DOAS dur-
ing multiple campaigns early in the eruption.
IMO is collecting precipitation samples at ~20 meteorological
observation sites. IMO performs the estimation of pH and amount
of sulphates and other pollutants (HF, HCl) to identify potential are-
as a?ected by acid rain. These samples are then analysed in cooper
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf