9 results were found for ������������ ������������KA���:Vb20���24������ ������������ ������������������������,������������������,������������,������������,������op.
Assessment Re-
port (AR4).
Topic 1 summarises observed changes in climate and their ef-
fects on natural and human systems, regardless of their causes, while
Topic 2 assesses the causes of the observed changes. Topic 3 pre-
sents projections of future climate change and related impacts un-
der different scenarios.
Topic 4 discusses adaptation and mitigation options over the
next few decades
/media/loftslag/IPPC-2007-ar4_syr.pdf
were gradually reduced in the 1960s(Østrem and Liestøl 1964). For a period in the1970s and 1980s measurements were sparse and re-duced to a minimum, for some years snow accu-mulation was only measured at 10–20 points. Fromthe mid-1990s the mass balance programme was
MODELLING LONG-TERM SUMMER AND WINTER BALANCES
? The authors 2009
Journal compilation ? 2009 Swedish Society for Anthropology
/media/ces/GA_2009_91A_4_Andreassen.pdf
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
extensively used in experimental economics over the
past 20 years. One robust result is that a considerable percentage of individuals voluntar-
ily cooperate, even though the Nash equilibrium is to contribute nothing to the public good
(see Anderson 2001 and Ledyard 1995, for reviews).3 Once we drop the homo-œconomicus
hypothesis, by assuming that either all agents have social preferences or agents
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.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
BIOMATH, Ghent University, Gent, Belgium
d Water Quality Modelling modelEAU, University Laval, Quebec, Canada
Received 20 December 2005; received in revised form 5 February 2007; accepted 7 February 2007
Available online 27 April 2007
Abstract
A terminology and typology of uncertainty is presented together with a framework for the modelling process, its interaction with the broader
water
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
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/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf