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Results:

• 51. Daniell_etal-2010

  limited. Therefore, experimentation as a research methodology and as an approach to management is key to adaptive management (e.g., Walters 1997, Lee 1999, Richter et al. 2003, Pahl-Wostl 2006). Such management should allow managerial practices to be changed based on new insights (Pahl- Wostl et al. 2008), as well as allow the evaluation of “management experiments”. According to Lee (1999 /media/loftslag/Daniell_etal-2010.pdf

• 52. Kok_JGEC658_2009

  thinking Not limited by data availability Data-driven Focus on social changes Focus on biophysical data K. Kok / Global Environmental Change 19 (2009) 122–133 123 Author's personal copy dynamics, such as Causal Loop Diagrams (Sterman, 2000); the Syndromes approach (Eisenack et al., 2007); and Bayesian networks (Pearl, 2000). 2.2. Definition and background A Fuzzy Cognitive Map is a representation /media/loftslag/Kok_JGEC658_2009.pdf

• 53. VI_2014_001

  the index flood and catchment attributes (see for instance Grover et al., 2002, for a review of potential methods). The index flood method has recently been evaluated for ten catchments in northern Iceland (Crochet, 2012a, 2012b), considering both daily and instantaneous flood quantiles. Results are promising, but the limited number of gauged sites available in these regions prevents the devel /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 54. IPPC-2007-ar4_syr

  responses to anthro- pogenic warming. The available analyses are limited in the number of systems, length of records and locations considered. Natural tem- perature variability is larger at the regional than the global scale, thus affecting identification of changes to external forcing. At the re- gional scale, other non-climate factors (such as land-use change, pol- lution and invasive species /media/loftslag/IPPC-2007-ar4_syr.pdf

• 55. Information and help

  at a regional scale in specific areas. The bulletin is general due to limited information and it applies to a large area of land. Thus, it does not replace local assessment at any given time. However, it is one of the tools that individuals can use to estimate avalanche danger at a local scale. Avalanches are one of the main sources of risk for backcountry travelers in mountains during winter /avalanches/forecast/help

• 56. Paper-Olafur-Rognvaldsson_92

  measurements. This can be done by comparing long term means (months, years) of simulated and observed precip- itation. Such a comparison would be of use to a hydrologist but of somewhat limited value for a forecaster. We therefore set out to making comparisons that would assess strong and weak points of the simulations to aid forecasters. We want to know how the errors in the simulated precipitation /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 57. Water_resources_man_Veijalainen_etal

  the possibilities to decrease the highest water levels are limited, because increasing the outflow from Lake Saimaa could cause flood damage on the Russian side in the outflow river, the Vuoksi. The current contract with Russia does not allow the discharges to increase above the natural rating curve without mutual agreement. To account for this, a maximum discharge of 1,100 m3/s was used in the simulations /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 58. Kok_2-scenarios-lecture-2

  research VIII. Resources: extensive vs limited IX. Institutional conditions: open vs constrained C Scenario content - complex vs simple: X. Temporal nature: chain vs snapshot XI. Variables: heterogeneous vs homogenous XII. Dynamics: peripheral vs trend XIII. Level of deviation: alternative vs conventional XIV. Level of integration: high vs low Scenarios - types EXAMPLE 1 – EXPLORATORY SCENARIOS /media/loftslag/Kok_2-scenarios-lecture-2.pdf

• 59. Perrels-CBA

  -economic criteria (∆%GDP; ∆% employment; etc. in case of very large or very effective projects) • NB! Different metrics may produce different rankings for the same set of projects • Above listed indicators are only straightforward in case of priced effects and assuming limited and tractable uncertainty • Above list of indicators provides no clue of redistribution effects, nor of implications /media/loftslag/Perrels-CBA.pdf

• 60. Reykholt-abstracts

  as a method to calculate glacier and ice sheet velocity. The two most common techniques revolve around radar interferometry, and feature tracking using radar or visible imagery. Velocity calculations from spaceborne plat- forms, particularly for slower and/or smaller ice masses, are limited by the spatial resolution and repeat interval of such imagery, however. In this paper, we evaluate the potential /media/vatnafar/joklar/Reykholt-abstracts.pdf