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Results:

• 11. Journal_of_Hydrology_Veijalainen_etal

  annual temperature varied from 5 C to 2 C and precipitation from 450 mm to 700 mm (Drebs et al., 2002). Finland is a long country and the temperature gradient is strong especially in winter (Fig. 1a), which affects the accumula- tion and melting of snow. In south-western Finland the thermal winter lasts on average for 100 days whereas in northern Finland this season is about 100 days longer /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 12. GA_2009_91A_4_Andreassen

  and asimplified mass balance model suggests that airtemperature and albedo is satisfactorily parameter-ised, at least for the AWS altitude. However, thecompared period covers only 5 of the 58 modelledyears in this study. Furthermore, the specific win-ter, summer and net balances measured at Stor-breen in 2001–2006 deviate markedly from the mean for the whole observation period. A combi-nation /media/ces/GA_2009_91A_4_Andreassen.pdf

• 13. Group4

  summers, leading to melting permafrost in the northern part of Finland, resulting in more frequent buckling of roadways, 5) increases in spring flooding and riparian flooding and 6) coastal sea level rise and erosion (Jaroszweski, Chapman, & Petts, 2010). Key uncertainties: 1) epistemic uncertainties- regionally down-scaled projected impacts, road usage patterns, road safety data, cost data /media/loftslag/Group4.pdf

• 14. IPPC-2007-ar4_syr

  and their interactions with sustainable develop- Figure I.1. Schematic framework representing anthropogenic drivers, impacts of and responses to climate change, and their linkages. Schematic framework of anthropogenic climate change drivers, impacts and responses ment. Topic 5 assesses the relationship between adaptation and mitigation on a more conceptual basis and takes a longer-term per- spective. Topic 6 /media/loftslag/IPPC-2007-ar4_syr.pdf

• 15. 2010_005_

  Temperature . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 17 4.2 Total Precipitation . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 19 5 Seasonal Differences in Climate Trends 20 6 Conclusions 21 5 List of Figures 1 Mean annual surface air temperature during the 1961–90 control period, differ- ences in degrees between the control period and the 2021–50 reference /media/ces/2010_005_.pdf

• 16. ces-glacier-scaling-memo2009-01

  2008) together with a regression line through this data set and a regression line derived for a data set of more than a hundred valley glaciers (Bahr and others, 1997). The regression lines are of the form v = csg ; (5) where v and s are glacier volume and area, respectively. The coefficient and exponent for the Icelandic ice caps are c = 0:048, g = 1:23, when the area and volume are expressed /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 17. ces-oslo2010_proceedings

  5 6 Welcome to the conference “ Future Climate and Renewable Energy: Impacts, Risks and Adaptation” We welcome you to the international conference Future Climate and Renewable Energy: Impacts, Risks and Adaptation. The conference is convened by the Nordic-Baltic project Climate and Energy Systems which is funded by Nordic Energy Research, the Nordic Energy sector /media/ces/ces-oslo2010_proceedings.pdf

• 18. VI_2015_009

  .............................................................. 19 5 Conclusion .................................................................................................. 23 6 Acknowledgements....................................................................................... 23 7 References .................................................................................................. 24 Appendix I - Identification /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 19. Horsens_case

  level coursed by tides is small with a range of less than 0.5 m. Figur 1. Horsens Fjord catchment. WFD main catchment area is 794 km2 NONAM Summerschool Copenhagen 22-26 August 2011 2 Physical features and ecosystem The fjord landscape is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations /media/loftslag/Horsens_case.pdf

• 20. James-Smith_Edward_CES_2010

  opportunity evaluation Case studies NOE Net SEAS-NVE Findings of case studies • Distribution companies generally well equipped for climate change – Cabling of all overhead lines well under way – Distribution boxes in areas with increased risk of flooding are elevated already – Salt spray further inland is becoming an increasing problem for substations and transformers Cabling in Denmark /media/ces/James-Smith_Edward_CES_2010.pdf