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• 31. ces_risk_flyer

  Climate and Energy Systems, 2007‐2010 Risk Assessment working group http://en.vedur.is/ces The Climate and Energy Systems; Risks, Potential and Adaptation is in many ways a follow up on the Climate and Energy (CE) Nordic‐Baltic research project (2003‐2006), both funded by Nordic Energy Research (www.nordicenergy.net) and the Nordic energy sector. The main objective of the CE project was to make /media/ces/ces_risk_flyer.pdf

• 32. Keskitalo_et_al-MLG_and_adaptation_FINAL

  policy has emerged or is emerging within a multi- level governance framework, it is necessary to assess the ways in which adaptation policies and other actions have been developed at each level. Such an assessment was conducted by applying a set of three broad questions to the empirical data: 1) What policies or initiatives have been developed on each level? 2) How have such policies been /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 33. Joining forces in weather forecasting and climate research

  of how climate change will impact our countries” says Árni.A sustainable solution Powered entirely by Icelandic hydropower and geothermal energy sources and taking advantage of the local tempered climate for keeping the supercomputer components cool, the running costs and CO2 footprint will be kept to a minimum, saving tonnes of CO2 in line with the four nations' efforts towards reaching Net /about-imo/news/joining-forces-in-weather-forecasting-and-climate-research

• 34. Milly_etal-2008-Stationarity-dead-Science

  www.sciencemag.org SCIENCE VOL 319 1 FEBRUARY 2008 573 POLICYFORUM Systems for management of waterthroughout the developed world havebeen designed and operated under the assumption of stationarity. Stationarity—the idea that natural systems fluctuate within an unchanging envelope of variability—is a foundational concept that permeates training and practice in water-resource engineering /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 35. Keranen_Jaana_CES_2010

  / opportunity identification 4. Risk / opportunity estimation (consequences, probabilities) 1. Scope definition Targets 5. Risk / opportunity evaluation Adaptation, mitigation Risk management Risk analysis Action plan Risk assessment 2. Data collection 2 .2 - … very likely2 .1 – L isääntyvä sadan ta vuositasolla 0-8 % 2. Lisääntyvä sadanta 1 .2 - … 3very likely T urbii nien kapasioteett ia vo idaan /media/ces/Keranen_Jaana_CES_2010.pdf

• 36. Adalgeirsdottir-etal-tc-5-961-2011

  (DGPS) equipment in 2001. Continuous profiles, approximately 1 km apart, were measured in the accumulation zone and a dense net- work of point measurements were carried out in the abla- tion zone. Digital Elevation Models (DEMs) of the surface and bedrock were created from these data (Fig. 2; Björns- son and Pálsson, 2004). The estimated errors are at most 1–5 m (bias less than 1 m) for the surface /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 37. Reykholt-abstracts

  Reykholt, Iceland, June 20–21, 2013 1 Content Sessions ...................................................................................................................................... 4 Programme ............................................................................................................................... 4 List of participants /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 38. Energy System Analysis

  Energy Systems Energy System Analysis Climate change affects the electricity market in many ways. Increasing /ces/project/energy/

• 39. Refsgaard_etal-2007-Uncertainty-EMS

  for granted. 4.13. Stakeholder involvement Stakeholder involvement in not only the decision making process, but also in the modelling process, can help to assess and manage complex (environmental) problems in a better way. This potential can be tapped in three ways (Kloprogge and van der Sluijs, 2006): (1) by enabling them to articulate Table 3 Example of use of the uncertainty matrix for an initial /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 40. Eyjafjallajokull_status_2010-05-07_IES_IMO

  recorded at 5-13 km depth, but fewer than yesterday. GPS deformation: Measurements from around Eyjafjallajökull indicate no major net discplaceaments, suggesting a stabilization of the surface deformation since yesterday. Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64 km distance from the eruption site shows that about 5 % of the ash is smaller /media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf