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Results:

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

  Public Choice (2012) 151:91–119 DOI 10.1007/s11127-010-9735-1 Inequity and risk aversion in sequential public good games Sabrina Teyssier Received: 5 January 2010 / Accepted: 12 October 2010 / Published online: 3 November 2010 ³ Springer Science+Business Media, LLC 2010 Abstract Behavioral hypotheses have recently been introduced into public-choice theory (Ostrom in American Political Science /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 2. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  1 PhD Workshop preceding Adaptation Research Conference – 27 & 28 August, Helsinki Climate change adaptation - Analysis, Planning and Implementation Programme Venue: Rantapuisto, Ramsinniementie 14, FIN-00980 HELSINKI directions for travel can be found at the conference web site http://www.nordicadaptation2012.net/ Informal start at 26 August On Sunday evening 8pm an informal get /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 3. Hare_1_PartINONAM

  monitoring Public involvement campaigns • moderated activity with a limited number of participants in which participants work together to carry out a common task » Nominal Group Technique, Participatory modelling (e.g. group model building), Role playing games, Scenario building, Forum theatre, Participatory budgeting.... Workshops / Collaboration Taken from Hare & Krywkow, (2004) Matching classes /media/loftslag/Hare_1_PartINONAM.pdf

• 4. Moellenkampetal_etal-2010

  [online] URL: http://www.ecologyandsociety.org/vol15/iss4/art11/ Synthesis, part of a Special Feature on Implementing Participatory Water Management: Recent Advances in Theory, Practice and Evaluation Co-engineering Participatory Water Management Processes: Theory and Insights from Australian and Bulgarian Interventions Katherine A. Daniell 1, Ian White 2, Nils Ferrand 3, Irina S. Ribarova 4, Peter /media/loftslag/Moellenkampetal_etal-2010.pdf

• 5. Daniell_etal-2010

  Copyright © 2010 by the author(s). Published here under license by the Resilience Alliance. Moellenkamp, S., M. Lamers, C. Huesmann, S. Rotter, C. Pahl-Wostl, K. Speil, and W. Pohl. 2010. Informal participatory platforms for adaptive management. insights into niche-finding, collaborative design and outcomes from a participatory process in the rhine basin. Ecology and Society 15(4): 41. [online /media/loftslag/Daniell_etal-2010.pdf

• 6. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  Public Choice (2010) 143: 293–301 DOI 10.1007/s11127-010-9626-5 Foundations of the Ostrom workshop: institutional analysis, polycentricity, and self-governance of the commons Michael D. McGinnis · James M. Walker Received: 25 January 2010 / Accepted: 22 February 2010 / Published online: 8 April 2010 ³ Springer Science+Business Media, LLC 2010 Abstract This paper highlights important lessons /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 7. 47th Nordic Seismology Seminar

  Registration 47th Nordic Seismology Seminar Registration The registration is now open. Please follow this link /norsem/norsem2016/registration/

• 8. Factsheet_Bardarbunga_20141015

  greater than M3.0 were recorded over the last 48 hours in or around the caldera. The largest one were M4.8 at 18:51 yesterday.  Little seismic activity is now detected in the northern part of the dyke and around the eruption site.  GPS measurements show minor movements. No great changes were detected.  No change was detected in water monitoring that cannot be explained by changing weather /media/jar/Factsheet_Bardarbunga_20141015.pdf

• 9. Bardarbunga_kafli20140825

  have extensive ice cover. The 2009 m high Bárðarbunga central volcano lies at the NW edge of the ice cap, with only its NW slopes ice free. It is dominated by a 80 km2 and up to 700 m deep ice-filled caldera. Bedrock rises to 1850 m in the northwest caldera rim and is lowest in a narrow gap the east rim where minimum elevation is 1350 m. The ice free fissure swarm north of Vatnajökull strikes /media/jar/Bardarbunga_kafli20140825.pdf

• 10. TF-FMS_20141204_skyrsla

  on the northern site of the lava flow, minor outbreaks were observed in the southwest close to the vents and into a lava-free part in the middle of the flow, see photo on the next page. Eruption site seen from NNW, rather calm bubbling activity. Photo: Martin Hensch EBE-035-1 Eftirlitsflug /media/jar/TF-FMS_20141204_skyrsla.pdf