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Results:

• 21. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  to determine a global figure for economic impact (From: EM-DAT 2008). 4 Based on baseline assessments of the case-studies in the NeWater- project (http://www.newater.info). 264 P. Huntjens et al. 123 these case-studies, more specifically in their level of AIWM.5 Therefore, this paper intends to identify differ- ences and similarities in AIWM, to detect general patterns, and to compare measures being /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 22. Paper-Olafur-Rognvaldsson_92

  is defined as a 24 hour period where the simulations are dry (rmm5 ≤ 0.1) but the observations are wet (robs > 0.1). Figure 5 shows the percentage of missing events during the summer months (JJA) at each of the observation stations. There is higher probability of missing events during sum- mer than in winter (map not shown). In Fig. 6 the precipitation during missing Figure 3: Ratio [%] of "false alarms /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

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

  The Cryosphere, 5, 961–975, 2011 www.the-cryosphere.net/5/961/2011/ doi:10.5194/tc-5-961-2011 © Author(s) 2011. CC Attribution 3.0 License. The Cryosphere Modelling the 20th and 21st century evolution of Hoffellsjökull glacier, SE-Vatnajökull, Iceland G. Aðalgeirsdóttir1,2, S. Guðmundsson1, H. Björnsson1, F. Pálsson1, T. Jóhannesson3, H. Hannesdóttir1, S. Þ. Sigurðsson4, and E. Berthier5 /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 24. Wind Energy

  the contiguous USA. 30th Annual Applied Geography Conference, Indianapolis, October 2007. 10 pp. Clausen, N.-E., Lundsager, P., Barthelmie, R., Holttinen, H., Laakso, T. & Pryor, S.C. (2007). Wind Power. In: J. Fenger (Ed.) Impacts of Climate Change on Renewable Energy Sources: Their role in the Nordic energy system, Nord 2007:003, 105-128. Clausen N.E., Pryor S.C., Larsén X.G., Hyvönen R /ces/publications/nr/1944

• 25. raisanen_ruosteenoja_CES_D2.2

  ............................................................................................................ 4 3. Best estimates of temperature and precipitation change................................................ 7 4. How certainly will temperature and precipitation increase? ....................................... 10 5. Uncertainty ranges and quantiles of temperature and precipitation change .............. 12 6. Hindcast verification of the resampling ensemble /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 26. Energy Systems

  Sveinsson, S. M. Garðarsson and S. Gunnlaugsdóttir (Eds.), Northern hydrology and its global role: XXV Nordic hydrological conference, Nordic Association for Hydrology, Reykjavík, Iceland August 11-13, 2008, pp 615-622. Reykjavík: Icelandic Hydrological Committee. Sveinsson, O.G.B., Linnet, Ú. & Elíasson, E.B. (2010). ” Hydropower in Iceland ? Impacts and adaption in future climate”, ”, Conference /ces/publications/nr/1937

• 27. Markarfljót outwash plain and Öræfajökull

  on the slopes the volcano, the jökulhlaups are quick to hit the lowlands once floodwater has reached the glacier's surface — in as little as ~5 minutes at peak discharge. Chapter V. Öræfi district and Markarfljót outwash plain: Rating of flood hazards (pdf 2.35 Mb) Pages 101–122 Emmanuel Pagneux og Matthew J. Roberts Short summary A semi-quantitative, damage-oriented method /hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/

• 28. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  dialogue Analyse Gaps (3) ? WR management functions ? Gaps to meet WR goals ? Management potentials and constraints Prepare Strategy and Action Plan (4) ? Enabling environment ? Tools and guidelines ? Monitoring system ? River basin action plan Build Commitment to Action (5) ? Political adoption ? Stakeholder acceptance ? Commit financing Implement IWRM Framework /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 29. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  climate changes between the CMIP3 and ENSEMBLES simulations 15 4. Impact of RCM data on forecasts of climate change 18 5. Probabilistic projections of temperature and precipitation change 24 5.1 Best estimates and uncertainty ranges of temperature and precipitation change 24 5.2 How probably will temperature increase (precipitation change) by at least X°C (Y%)? 28 6. Conclusions 34 References /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 30. Climate and Modeling Scenarios

  4-5 Nov 2008, Helsinki, Finland. Kjellström, E. (2010). Deliverable 4.3. Report on user dialogue and analysis of regional climate scenarios for northern Europe. Swedish Meteorological and Hydrological Institute, Technical report, final version delivered 15 April 2010. Kjellström, E., Drews, M., Christensen, J. H., Haugen, J. E., Haakenstad, H. & Shkolnik, I. (2010). An ensemble of regional /ces/publications/nr/1680