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Results:

• 21. Perrels-CBA

  operational cost, etc.) and the annual revenues • consider an appropriate discount rate and assess NPV (net present value), IRR (internal rate of return), and net cash flows • rank alternatives by score level • SCBA: social CBA – total benefits -/- total costs for society, in this case benefits and costs often don’t accrue (entirely) to the same organisation due to the public nature of a project /media/loftslag/Perrels-CBA.pdf

• 22. Journal_of_Hydrology_Veijalainen_etal

  ) in Europe yield contradictory results on the changes in floods in many parts of Europe, including Finland. Dankers and Feyen (2008) reported a considerable reduction of 10–40% in 100-year discharges in Finland, much of northern Sweden and north-western Russia by the end of the century due to decrease in snow accumulation; however Lehner et al. (2006) evaluated that the 100-year floods in the same areas /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 23. GA_2009_91A_4_Andreassen

  to highly negative summer balances, but also lower bw than the average for 1949–2006. Calculated change in specific mass balance for a ±1°C change in air tem- perature was ±0.55 m w.e., whereas a ±10 % in- crease in precipitation represented a change of ± 0.20 m w.e. Model results further indicated that for a 2°C warming, the ablation season will be extend- ed by c. 30 days and that the period /media/ces/GA_2009_91A_4_Andreassen.pdf

• 24. IPPC-2007-ar4_syr

  data, models or analyses, then the following scale of confidence levels is used to express the assessed chance of a finding being correct: very high confidence at least 9 out of 10; high confidence about 8 out of 10; medium confidence about 5 out of 10; low confidence about 2 out of 10; and very low confidence less than 1 out of 10. Where uncertainty in specific outcomes is assessed using expert /media/loftslag/IPPC-2007-ar4_syr.pdf

• 25. 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

• 26. Group4

  Focus 10. Rising carbon prices, putting price pressure on carbon-intensive inputs in the road sector, including concrete, asphalt and bitumen. 11. Shorter logistics chains driven by shifts toward service consumption rather than goods consumption, reducing Heavy Goods Vehicle traffic 12. Shift to biological primary resource inputs, reducing the need for mining, metallurgy and other primary /media/loftslag/Group4.pdf

• 27. 2010_005_

  day during the 1961–90 control period, differences in percent of the control period between the control period and the 2021–50 reference period, and linear trends in percent of the control period per decade within the 2004–50 period, for the IPCC GCM ensemble mean, the SMHI-RCAO, the MetNo-HIRHAM, and the DMI-HIRHAM5. . . . . . . . . . . 31 10 Mean annual air pressure at mean sea level /media/ces/2010_005_.pdf

• 28. ces-oslo2010_proceedings

  ............................................................................................................... 8 PAST AND PRESENT CHANGES IN CLIMATE AND HYDROLOGY Dyrrdal, A.V., Vikhamar-Schuler, D., Stranden, H.B. and Skaugen, T. Analysis of past snow conditions in Norway – Time periods 1931-60, 1961-90 and 1979-08 ............................. 10 Crochet, P. Impacts of historic climate variations on streamflow characteristics in Icelandic rivers /media/ces/ces-oslo2010_proceedings.pdf

• 29. Reykholt-abstracts

  ................................................................................................................... 8 Liss M. Andreassen, Hallgeir Elvehøy, Sindre Engh and Bjarne Kjøllmoen ..................... 9 Lidar measurements of Norwegian glaciers – an overview Neil Arnold* and Gareth Rees .............................................................................................. 10 Calculation of glacier velocity from repeat /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 30. ces-glacier-scaling-memo2009-01

  and ice caps may be derived from data about the area distribution of ice bodies in the drainage basin. Since the exponents g in the volume–area scalings v = csg for both ice caps and glaciers TóJ 3 5.12.2009 Memo Area (km2) Volume (km 3 ) 50 100 50 100 150 200 250 50 100 150 200 250 a71 a71a71 a71 a71 10 50 500 500020 1000 1 5 10 0 100 0 2 2 0 20 0 200 0 100 10000 Icelandic ice /media/ces/ces-glacier-scaling-memo2009-01.pdf