9 results were found for ������������������katalk:po03���200%������ ��������� ������ ���������������������op.

Results:

• 1. field_report_03032015

  /media/jar/field_report_03032015.pdf

• 2. Keranen_Jaana_CES_2010

  /media/ces/Keranen_Jaana_CES_2010.pdf

• 3. IPPC-2007-ar4_syr

  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

• 4. GA_2009_91A_4_Andreassen

  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

• 5. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  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

• 6. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  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

• 7. Adalgeirsdottir-etal-tc-5-961-2011

  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

• 8. Refsgaard_etal-2007-Uncertainty-EMS

  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

• 9. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  no tcaus e mor e problem si n th e (far )futur e (20 year s o r more ) Vos s et al .( 200 6), Dub e an d Swatu k (200 2), Kicker te t al .( 199 7) Alread y no w preparation s ar e take n fo rth e (far )futur e (20 year s o r more ) Raadgeve re t al .( 200 8), Pahl-Wos te t al .( 2007 c), Vos s et al .( 200 6) 13 .Flexibl e measures , keepin g option s ope n Measure s take n no w o r propose d fo rth /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf