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Results:

• 1. Statistical Analysis

  (2010). Trends in streamflow in the hydropower producing Nordic countries and implications for water resource management, IAHS Publ. 340, 279-285. National Hellström, S-S., and Lindström, G. (2008). Regional analys av klimat, vattentillgång och höga flöden (Regional analysis of climate, runoff and flooding). SMHI Report Nr 110, 23 p. Hisdal, H., Holmqvist E., Jónsdóttir, J. F., Jónsson, P /ces/publications/nr/1943

• 2. Publications

  M., & Hellström, S.-S. (2006). Climate change effects on dam safety - a sensitivity analysis of the Swedish hydrological dam safety guidelines. Presented at the European Conference on Impacts of Climate Change on Renewable Energy Sources, Reykjavik, Iceland, June 5-9. [Extended abstract] Andréasson, J., Gardelin, M., Bergström, S., & Hellström, S.-S. (In press). Känslighetsanalys av /climatology/research/ce/publications/

• 3. Hydropower, Hydrology

  ) på University of Gloucestershire i Cheltenham 29/9 2009. Roald, L.A. Klimaendringer, flom og skred. Forelesning på kurset: 09/50 Klimatilpasning i samfunnsplanleggingen arrangert av NUSB i Trondheim 10/11-2009. Vehviläinen, B. Climate change and Finlands water resources. Symposium of Large Lakes. March 8, 2010, Lahti, Finland. Veijalainen, N. Climate and Energy Systems (CES): Hydrology /ces/publications/nr/1938

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

  Av. Ed. Belin, 31400 Toulouse, France Received: 21 March 2011 – Published in The Cryosphere Discuss.: 6 April 2011 Revised: 5 October 2011 – Accepted: 20 October 2011 – Published: 2 November 2011 Abstract. The Little Ice Age maximum extent of glaciers in Iceland was reached about 1890 AD and most glaciers in the country have retreated during the 20th century. A model for the surface mass balance /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 5. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 6. ces-glacier-scaling-memo2009-01

  Meteorological Office, Memo ÚR- TóJ-2009-01. AV AILABILITY The gls software can be obtained from Tómas Jóhannesson Veðurstofa Íslands — Icelandic Meteorological Office Bústaðavegi 9 IS-150 Reykjavík Iceland Phone: +354-1-5226000, Fax: +354-1-5226001, E-mail: tj@vedur.is 3 /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 7. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  la tio ns hi ps be tw ee n di ffe re nt dis cipline s = > bro ad inte grate d outp ut (bu tn o tq ua nt ita tiv e) Pr ogres s towa rd sIWR M measu re s Ind icator s o fe ffec to f measu res , invo lvin g m o n ito rin g M ul tip le fra m es (so cia l sy st em ):w at er u se s su ch as n av ig at io n , hy dr o ele ct ric po w er ge n er at io n , flo o d pr o te ct io n m u st be ha rm o n ize d w /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 8. Keskitalo_et_al-MLG_and_adaptation_FINAL

  /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 9. IPPC-2007-ar4_syr

  /media/loftslag/IPPC-2007-ar4_syr.pdf

• 10. VI_2015_005

  in this study, 16 Figure 7. Seasonal per grid point occurrence of low-pressure centres (LPC) for daily av- erages, as well as for 5-day and 31-day running means of daily grid-point time-series. The dotted lines indicate the domain boundaries. The dash-dotted lines indicate bound- aries between different sectors, as described in the text. Note the difference in scale of the colour shading between /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf