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

  to identify and disentangle the individual preferences which effec- tively play a role in individuals’ decisions in social dilemmas. One key feature of such social dilemmas is the presence of strategic uncertainty: individuals decide whether to cooperate without knowing what others have decided. This paper empirically specifies the individual preferences which matter in a particular social dilemma /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 12. Horsens_breakout_12August

  uncertainties on climate change effects? o Which ambiguities are in play regarding various themes and challenges? o Prepare a survey of the main uncertainties and ambiguities, their characteristics and describe how to deal with the different sources of uncertainties o How are you representing and explaining uncertain knowledge to stakeholders? 3. Prepare a stakeholder involvement plan o How do you /media/loftslag/Horsens_breakout_12August.pdf

• 13. VI_2020_005

  ). The rising mean sea levels are significant drivers of increased flood risk but other factors play a big role as well (Church, Clark, et al., 2013). Vertical isostatic movement is fast in Iceland and therefore, its pattern will be an important factor in determining spread and severity of future floods in the country (Björnsson et al., 2018). Other factors that are more difficult to predict /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 14. Henriksen-AM

  as a whole. The ability to negotiate about and agree on rules and roles seems to play an essential role. Despite the collaborative nature of social learning strong leadership and facilitation have proven to be important • Learning may have different degrees of intensity and scope from learning within groups, to actor networks and to structural change (addressed in the concept of tripple loop learning /media/loftslag/Henriksen-AM.pdf

• 15. VI_2014_006

  that if two meteorological situations are similar regarding large scale atmospheric circulation, they should also be similar with respect to local meteorological conditions. Local meteorological conditions depend on the synoptic situation but local features such as orography and surface properties play also an important role. Considering a given meteorological situation characterised by some synoptic /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 16. Group4

  strategic investment plan and coordinated with strategic guidance from the EU concerning transport policies and plans. The policy objectives set within relevant EU directives will play an integral part within Finnish long range planning processes, as EU directives allow member states flexibility to implement various measures according to national conditions. An essential requirement has been the buy /media/loftslag/Group4.pdf

• 17. Keskitalo_et_al-MLG_and_adaptation_FINAL

  on adaptation. However, adaptation action in Woking has largely occurred as a result of the state performance assessment framework, again indicating the role that central state measures play at the local level. Following its development of adaptation actions in 2008, Woking was appointed one of the national “Climate Change Beacons” to serve as an inspiration to other local authorities. 4.2 /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 18. Markarfljót outwash plain and Öræfajökull

  around Öræfajökull Volcano that would be liable to flooding during a subglacial eruption are identified. Jökulhlaups are simulated as instant release waves over the ice surface using the SAMOS 2D avalanche model, using estimates of the magnitude of historical jökulhlaups in the region. Simulations are made for jökulhlaups caused by a caldera eruption, flank eruptions, and pyroclastic density /hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/

• 19. CES_D2.4_VMGO

  cold wave duration ranges from 1-3 to more than 10 days throughout the region (Fig. 2d). In contrast with changes in heat waves, the most pronounced changes (decrease) in cold wave durations can be distinguished in northern areas of the region notably over northern EU and north-western ER (by 6-8 days), and Russian Far North (by 8-10 days). The spatial picture of changes in heat and cold wave /media/ces/CES_D2.4_VMGO.pdf

• 20. VI_2017_009

  and this difference to be most prominent in the NW part of the Iceland domain (see Figure 5a). The reason for this is most likely an overestimate of the sea ice cover in Arctic-44. As the sea ice seems to play an important role in this difference it is important to consider the quality of the sea ice simulations. We look at this in more details later in this study. The results for Arctic-44 show slightly /media/vedurstofan-utgafa-2017/VI_2017_009.pdf