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61. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

taken to cope with floods and droughts. The characteristics (see next paragraphs) of AIWM are to be regarded as working hypotheses, since the change toward more adaptive management regimes is yet slow and empirical data and practical experience thus limited—in particular regarding the interdependence of elements of the management regime. The strong interdependence of the factors stabilizing /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
62. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

i.e. differences in people’s norms and values, human behaviour, i.e. behavioural variability and ‘non-rational’ behaviour; social, economic, cultural and political dynamics (societal variability), i.e. the non-linear, chaotic and unpredictable nature of societal processes (e.g. Funtowicz and Ravetz 1990). Epistemic uncertainty in a natural context includes limitations in data, models and limited /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
63. VI_2015_005

in their development. Also, MSLP is a poor indicator of cy- clonic activity in tropical regions, where the geostrophic wind relationship breaks down (e.g., Anderson, Hodges, & Hoskins, 2003; Hodges, 1994; Hodges, Hoskins, Boyle, & Thorncroft, 2003, 2004; Hoskins & Hodges, 2002; Murray & Simmonds, 1991). With limited spatial res- olution of gridded pressure data, there is the possibility that small or weak cyclones /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
64. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

situations of strategic interaction. 4Contributions may depend on beliefs about others’ contributions in an environment with strategic uncer- tainty; however, this effect does not pertain in an environment without strategic uncertainty. 5This limited choice was imposed in order to make the game as simple as possible and to yield clear theoret- ical predictions depending on intrinsic preferences. 94 /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
65. Hare-2011-ParticipatoryModelling

within the management system. Form III: Front-End Participatory Modelling This form includes very limited participation, focused exclusively on the early stages of the modelling process. Example 8: Moorlands (Hare, 1999). This modelling activity sought to develop competing models of red grouse population dynamics and management, within a simulation laboratory, for scientic purposes, i.e. assessing /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
66. Kok_et_al._TFSC_published_2011

or society pays); ‘population’ (high or low migration); ‘global integration’ (threat or opportunity); ‘public involvement’ (passive or active); and ‘technology’ (limited or widespread technology adoption). More details can be found in [39]. 840 K. Kok et al. / Technological Forecasting & Social Change 78 (2011) 835–851 Author's personal copy 3.3. Exploratory scenarios (WS1 and WS2) Four stories were /media/loftslag/Kok_et_al._TFSC_published_2011.pdf
67. Bárðarbunga 2014 - October events

in subsidence was observed for the M5.3 earthquake this morning. Earthquake rates in the dyke intrusion are rather low, around 20 events have been detected in the last 24 hours, the strongest one was magnitude 1.4 yesterday at 23:31. All events in the dyke were located between the northern part of Dyngjujökull and the eruption site in Holuhraun. The eruption continues, visibility on webcams was limited /earthquakes-and-volcanism/articles/nr/3011
68. Bardarbunga-2014_October-events

located between the northern part of Dyngjujökull and the eruption site in Holuhraun. The eruption continues, visibility on webcams was limited this morning due to weather. 20 October 2014 14:00 - from the Scientific Advisory Board Notes from the meeting of the Scientific Advisory Board (pdf 0.4 Mb) 20 October 2014 10:00 - from geoscientist on duty Seismic activity at Bárðarbunga is still high /media/jar/Bardarbunga-2014_October-events.pdf
69. VI_2014_005

and shape of the underlying terrain. There is the possibility that model simulations are accurate with respect to the model terrain, but still compare poorly to surface measurements, due to subgrid-scale variability of terrain elevation. Therefore, to be able to identify as much as possible model errors that are not related to a limited description of orography, the influence of local terrain /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
70. Bárðarbunga 2014 - October events

in subsidence was observed for the M5.3 earthquake this morning. Earthquake rates in the dyke intrusion are rather low, around 20 events have been detected in the last 24 hours, the strongest one was magnitude 1.4 yesterday at 23:31. All events in the dyke were located between the northern part of Dyngjujökull and the eruption site in Holuhraun. The eruption continues, visibility on webcams was limited /earthquakes-and-volcanism/articles/nr/3011/