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Results:

• 71. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  296 Public Choice (2010) 143: 293–301 2 The commons The literature on the commons, or what is more technically defined as common-pool re- sources (CPRs), should be viewed initially from its place in the larger literature on dilem- mas of collective action. Since the foundational work of H. Scott Gordon (1954) on the com- mons, and Mancur Olson (1965) on collective action more broadly, the behavioral /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 72. 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

• 73. 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

• 74. 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/

• 75. 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

• 76. 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

• 77. 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

• 78. PhD_course-Programme_26Aug2011-final

  for widespread adoption in the water sector. Environmental Policy and Governance. DOI: 10.1002/eet.590 Kaner S (2007) Facilitator’s Guide to Participatory Decision-Making. Jossey-Bass: San Francisco. Cooke B, Kothari U (2007) Participation: the new tyranny? (4th edition) Zed Books: New York. Daniell KA, White I, Ferrand N, Ribarova IS, Coad P, Rougier J-E, Hare MP, Jones NA, Popova A, Rollin D /media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf

• 79. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 80. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf