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/media/loftslag/Group5-Stakeholders_involvement.pdf
Change 19 (2009) 122–133
A R T I C L E I N F O
Article history:
Received 14 November 2007
Received in revised form 21 August 2008
Accepted 25 August 2008
Keywords:
Fuzzy Cognitive Maps
Scenario
Participation
Resilience
Brazil
A B S T R A C T
The main drawback of the Story-and-Simulation approach is the weak link between qualitative and
quantitative scenarios. A semi-quantitative tool, Fuzzy
/media/loftslag/Kok_JGEC658_2009.pdf
at the operational/local level.
A calibrated approach (standardized questionnaires and
interviews, expert judgment, and reinterpretation of out-
comes by means of relevant literature) was used to com-
pare the state of affairs in water management in the
selected case-studies.
Adaptive and integrated water management
Given the expected increase of climate-related extreme
events, water governance capabilities
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
which are significantly lower com-
pared with similar beginning and end years. Consequently, for the 2004–50 period, the average
RCM warming rates of 0.29 K per decade over the ocean, and 0.35 K per decade over the land are
somewhat larger than for the reduced IPCC ensemble mean.
Additionally, the tabulated values of SAT differences between the 1961–90 control period and
either the 2021–50
/media/ces/2010_005_.pdf
level, surveys commissioned by the European Com-
munity/the European Union provide an indication of trends in concern about cli-
mate change. Since 1992, such surveys have been undertaken among representative
samples of citizens in its Member States, and specifically on topics related to the
environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB
in 2002). These have included
/media/loftslag/Lorenzoni_Pidgeon_2006.pdf
and Implementation of Seismic Early Warning Processes in South-West Iceland
Kristín S. Vogfjörd, Einar Kjartansson, Ragnar Slunga, Páll Halldórsson, Sigurlaug Hjaltadóttir, Gunnar B. Gudmundsson o.fl.
83 bls.
3,2 Mb
2010-003
Use of relatively located microearthquakes to map fault patterns and estimate the thickness of the brittle crust in Southwest Iceland
Sigurlaug Hjaltadóttir
104
/earthquakes-and-volcanism/reports-and-publications/
frequency distributions for Re-
gion 1 derived with index flood model no. 6: bµ(D) = a(AP=Z)b ............................ 39
5
Appendix VI - Empirical and modeled daily flood frequency distributions for
Region 2 derived with index flood model no. 3: bµ(D) = a(APm)b ......................... 41
Appendix VII - Instantaneous Index flood models for Region 1. .......................... 43
Appendix VIII
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf
to theoretical framework. I do also want to thank him for an
enjoyable time during this work, both in the office and in the field.
This work was carried out as a part of the Skaftá cauldrons research project which
was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja-
sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com-
pany), the National Energy
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
= {0, . . . ,20}. The second option, option b, is
such that the dictator keeps 18 points for herself and gives two points to the receiver: the
distribution (18,2). In decision 1, the dictator thus chooses between the distribution (0,0)
(zero for herself and zero for the receiver) and the distribution (18,2) (18 for herself and
two for the receiver); in decision 2, the choice is between (1,1
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf