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Journal of Environmental Management 88
Heid
, Øste
d
e
A broad range of tools are available for integrated water resource management (IWRM). In the EU research project NeWater, a
Human dependence on water leaves us vulnerable to
climate change, flood and drought hazards, and poverty
dynamic element of vulnerable groups and their relation-
ship to water resources, and to represent the decisions
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
and direction, as well as air temperature, from the IMO operational surface station net-
work. Most anemometers are installed at 10 m above ground level (mAGL). However, at some
stations, surface winds are measured at different heights, h, varying between 4.0 and 18.3 m.
3This is done using a GRIB-API command on Parameter 141 (snow depth) in the earliest boundary
data file: grib_set -f -d 0.0 -w
/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
....................................................................................... 10
3 September 2012 .................................................................................. 12
3 Radiation fluxes at the surface ....................................................................... 16
4 Heat fluxes at the surface .............................................................................. 21
5 Net energy
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
Grin’s work on this article was part of the programme of the
Dutch Knowledge network on System Innovations (KSI).
P. Huntjens (&) C. Pahl-Wostl
Institute for Environmental Systems Research,
University of Osnabruck, Barbarastraße 12, Geb. 66,
49069 Osnabruck, Germany
e-mail: patrickhuntjens@yahoo.com
J. Grin
Amsterdam School for Social Science Research,
University of Amsterdam, Amsterdam
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
up to ~13 km height.
BY K. S. VOGFJÖRD, S. S. JAKOBSDÓTTIR,
G. B. GUDMUNDSSON, M. J. ROBERTS, K. ÁGÚSTSSON,
T. ARASON, H. GEIRSSON, S. KARLSDÓTTIR,
S. HJALTADÓTTIR, U. ÓLAFSDÓTTIR,
B. THORBJARNARDÓTTIR, T. SKAFTADÓTTIR,
E. STURKELL, E. B. JÓNASDÓTTIR, G. HAFSTEINSSON,
H. SVEINBJÖRNSSON, R. STEFÁNSSON, AND T. V. JÓNSSON
Research, 2005), which are complemented by
three continuous GPS stations
/media/jar/myndsafn/2005EO260001.pdf
Refsgaard a,*, Jeroen P. v
Peter A. Vanroll
a Geological Survey of Denmark and Greenlan
b Copernicus Institute for Sustainable Development and Innovation
Utrecht University, Utrecht
c
Environmental Modelling & Softwar
equitable manner without compromising the sustainability of
* Corresponding author. Tel.: þ45 38 142 776; fax: þ45 38 142 050.
E-mail address: jcr@geus.dk (J.C. Refsgaard).
1364-8152
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
a systematic com-
parison of results to observed precipitation has been carried out. Un-
dercatchment of solid precipitation is dealt with by looking only at
days when precipitation is presumably liquid or by considering the
occurrence and non-occurrence of precipitation. Away from non-
resolved orography, the long term means (months, years) of observed
and simulated precipitation are often
/media/ces/Paper-Olafur-Rognvaldsson_92.pdf