4
Contents
1 Introduction ................................................................................................ 7
2 Study area and data ..................................................................................... 7
2.1 River basins .......................................................................................... 7
2.2 Streamflow data
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
2007a, b). BNs were tested in a recent EU
research project MERIT (Bromley, 2005; www.merit-
eu.net) 2001–2004, and this tool is currently considered in
Uncer
wate
NeWa
an
tainty is a central theme in integrated and adaptive
r management, where different disciplines need to be
Monitor and evaluate outcomes; apply learning to
develop a better understanding of the system.
(4)
Implement policies;(3
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
, Veðurstofu Íslands
Contents
1 Introduction ................................................................................................ 7
2 Model setup and data ................................................................................... 7
3 Model terrain and surface type ...................................................................... 9
4 Impact of initial conditions in blending
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.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
the elevation
drops by 300 m over a 4 km distance. Below the ice fall,
the glacier spreads out forming two branches, west and east
of a prominent ridge. Currently the eastern branch termi-
nates in a lagoon at ∼40 m a.s.l. and the western branch in
a lagoon at ∼20 m a.s.l. (local names are Hoffellsjökull and
Svínafellsjökull for the eastern and western branch, respec-
tively).
The first glaciological
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
regimes of
Number of flood and drought disasters in the past
decades per case study
0
2
4
6
8
10
12
1977-1986 1987-1996 1997-2006
Time period
Total number of flood and
drought disaster
s
Rivierenland
Alentejo
Upper Tisza - Hungary
Upper Tisza - Ukraine
Fig. 1 Number of reported flood and drought disasters in the past
decades in Rivierenland, Alentejo, Hungarian part of Upper Tisza,
and Ukrainian
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