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Results:

• 71. Daniell_etal-2010

  and interests into policy-making and decision-making processes. Also, by providing space for informal multi- stakeholder platforms, management experiments can be established more easily in rigid regulatory settings, allowing for social learning to take place. Stakeholder participation is currently stipulated by several legal provisions, such as the Water Framework Directive, which plays an increasingly /media/loftslag/Daniell_etal-2010.pdf

• 72. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  and civil society groups; (3) management instruments in terms of water resources and demand assessments, economic instruments and water resources information and monitoring; (4) national plans, e.g. relevant Sector Reform Plans, Infrastructure Plans and National Environmental Action Plans; (5) endorsed international agreements and processes; (6) for a for cross-sectoral and multi-stakeholder /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 73. A minor eruption underway

  is considered small at this stage and the volcanic activity has somewhat decreased since yesterday evening. The eruptive fissure is appr. 500 - 700 m long. The lava area is less than 1 km2 covering an area that is appr. 500 m wide. Lava fountains are small and lava flows are currently a very local hazard. The seismic activity is minor and spread around the Fagradalsfjall area. There is no indication /about-imo/news/earthquake-swarm-in-reykjanes-peninsula

• 74. VI_2009_013

  for the 1994 event, but located the source roughly 3 km farther northeast. A more recent interpretation based on a combined multi-temporal InSAR algorithm (Hooper, 2008; Hooper, personal communication 2008) places the two sill intrusions at 5.6 ± 0.1 km in 1994 and at 5.7 ± 0.5 km in 1999–2000. No observed crustal deformation accompanied the seismic swarm in 1996, which produced /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 75. VED_AnnualReport-2013_screen

  to issue warnings and forecasts. These data provide a benchmark for assessing ongo- ing changes in the Arctic, valuable information on natural resources in Iceland such as water and wind resources, as well as being fundamental in risk as- sessment studies carried out at IMO. In order to broaden the research already carried out at IMO the institute is involved in many multi- participant /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 76. Climate and Modeling Scenarios

  climate change simulations for Europe. Rossby Centre Newsletter, May 2009. Räisänen, J. & L. Ruokolainen (2008). Probabilistic climate fore­casts based on multi-model ensemble simulations. 26.02.2008: Modellers' review, Helsinki. Räisänen, J. & Ruokolainen L. (2009). Probabilistic forecasts of temperature and precipitation change by combining results from global and regional climate models (CES /ces/publications/nr/1680

• 77. ces-oslo2010_proceedings

  it reaches between 3 and 4°C (not shown). In summer the climate change signal in temperature is smaller with between 1 and 3°C in all Nordic land areas in the models and between 1 and 2°C in the multi-model mean (Fig. 1). Also the spread between the simulations is smaller with the inter-model standard deviation being less than 1°C in all of the area (not shown). Summertime changes /media/ces/ces-oslo2010_proceedings.pdf

• 78. CES_D2.4_task1

  distribution of probability distribution”), however, we focus in this report on multi-model mean (i.e., “best-estimate”) climate projections, as represented by the red lines in the mentioned two figures. Table 2.1. Definitions used in classifying monthly-to-annual values of temperature and precipitation. Very cold Temperature below the 10th percentile in 1961-1990 Cold Temperature below /media/ces/CES_D2.4_task1.pdf

• 79. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  but they may also cancel each other. Thus, even large uncertainties may have small consequences for decision making, because multiple sources of information provide sufficient knowledge to justify action in climate change adaptation. Keywords Climate change . Adaptation . Uncertainty . Risk . Water sectors . Multi-disciplinary 1 Introduction Climate change affects many aspects of human societies /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 80. Kok_JGEC658_2009

  the calibration consisted of stabilising the state vector by varying the strength of the additional feedback. 3. Fuzzy Cognitive Maps to understand complex systems—the Brazilian Amazon example To further illustrate the potential of Fuzzy Cognitive Maps, an example of the application to the issue of deforestation in the Brazilian Amazon is given. This example is illustrative because of its multi-scale /media/loftslag/Kok_JGEC658_2009.pdf