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Results:

• 41. aerodrome_summaries_20140603

  M (171FT ) FRE Q UENCIE S (PE R CENT ) O F OCCU R RENC E O F CONCURREN T WIN D DIRECTIO N (I N 30 0 SEC T ORS ) AN D SPEE D (I N KN O TS ) WITHI N SPECIFIE D RANGE S ANN U A L WIN D WIN D SPEE D (KT) ) DIRECTIO N CAL M 1– 5 6–1 0 11–1 5 16–2 0 21–2 5 26–3 0 31–3 5 36–4 0 41–4 5 46–5 0 >5 0 T O T A L V ARIABL E 0 0 0 0 0 0 0 0 0 0 0 0 0 35-36-0 1 3 2 3 3 2 1 1 0 0 0 0 0 14 02-03-0 4 0 2 4 4 3 1 0 0 /media/vedur/aerodrome_summaries_20140603.pdf

• 42. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  aversion should influence the first mover’s decision. The 98 Public Choice (2012) 151:91–119 Fi g. 1 O pt im al co n tr ib u tio n de pe nd in g o n α , r an d p Public Choice (2012) 151:91–119 99 Table 1 The predicted effect of intrinsic preferences on first and second movers’ contributions 1st mover 2nd mover Disadvantageous Negative None inequity aversion Advantageous None Positive inequity /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 43. GA_2009_91A_4_Andreassen

  the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf

• 44. Weather stations

  TíðaskarðFaxaflsjObs.ForecastMeteogramInfo.Obs. data Tjörnes - GerðibrekkaNorth EsjObs.ForecastMeteogramInfo.Obs. data TorfurNorth EsjObs.Info.Obs. data Return to the top of the page U UpptyppingarCentralsjObs.Info.Obs. data Return to the top of the page V VaðlaheiðiNorth EsjObs.Info.Obs. data Vaðlaheiði IINorth EsjObs.Info.Obs. data VatnaleiðFaxaflsjObs.ForecastMeteogramInfo.Obs. data /weather/stations/

• 45. Crochet_Philippe_CES_2010

  in snow cover duration between 25% warmest and 25% coldest years +1.7°C Catchment elevation (m.a.s.l) Catchment elevation (m.a.s.l) D u r a t i o n i n m o n t h barb2right -40 % Magnitude difference 100(Warmest - Coldest)/Coldest barb2right -37 days Mean yearly maximum snowmelt rate Timing difference between 25% warmest and 25% coldest years +1.7°CCatchment elevation (m.a.s.l) Catchment /media/ces/Crochet_Philippe_CES_2010.pdf

• 46. Kurpniece_Liga_CES_2010

  • MetNo-HIRLAM-HadCM3, • SMHI-RCA3-BMC with the SRES A1B. The climate model results were downscaled using statistical downscaling method: Sennikovs, J. and Bethers, U. 2009. Statistical downscaling method of regional climate model results for hydrological modeling. 18th World IMACS / MODSIM Congress, Cairns, Australia 13-17 July 2009 http://mssanz.org.au/modsim09 Observed, modeled /media/ces/Kurpniece_Liga_CES_2010.pdf

• 47. Lawrence_Deborah_CES_2010

  100 15 17 19 21 23 25 Mean annual peak runoff (mm/day) P e r c e n t a g e b e l o w g i v e n v a l u e g39g72g79g87g68g3g70g75g68g81g74g72g3 g40g80g83g76g85g76g70g68g79g3g68g71g77g88g86g87g80g72g81g87 Percentage change in 200-year flood Uncertainty – Relative magnitude of sampled s urces N = 115 GCM/RCM = 50 EA/DC = 38 HBV = 27 • Differences in GCM/RCM tend to be more significant in inland /media/ces/Lawrence_Deborah_CES_2010.pdf

• 48. VI_2014_006

  the com- plexity of the hydrological processes through modelling, but its application is usually limited to the short-range. Although the results demonstrated a great potential for this method, its success- ful application in real-time will strongly depend on the quality and availability of streamflow observations, which can be poor or simply missing during periods of variable durations, e.g /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 49. ces-oslo2010_proceedings

  ............................................................................... 20 Räisänen, J. Probability distributions of monthly-to-annual mean temperature and precipitation in a changing climate ......... 22 Nikulin, G., Kjellström, E., Hansson, U., Strandberg G. and Ullerstig A. Nordic weather extremes as simulated by the Rossby Centre Regional Climate Model: Model evaluation and future projections /media/ces/ces-oslo2010_proceedings.pdf

• 50. Perrels-CBA

  of market organisation alternatives 26.8.2011Adriaan Perrels/IL 10 Cost-benefit analysis – the basics 3 Simple example: despite positive IRR still cash flow challenge years 1 - 8 CBA example - initial investment 100; interest and discount 5%; operational cost +5%/y; benefits +10%/y; IRR = 7.4% -20 -10 0 10 20 30 40 50 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 years m o n e y u n it s writing off finance /media/loftslag/Perrels-CBA.pdf