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Results:

• 21. Risk Assessments

  riskianalyysit - ilmaston muutoksen synnyttämät riskit ja mahdollisuudet. 12.03.2009, Research Report VTT-R-01942-09, Tampere. 13 p. + app. 24 p. Linnerud, Kristin (2009) Test and evaluation of a climate risk assessment procedure. Case study: The Norwegian hydro power company SFE. CICERO, University of Oslo. Report 2009:3. Feb.2009. 44 p. ISSN:0804-4562. Linnerud, Kristin (2009) Climate change /ces/publications/nr/1941

• 22. Refsgaard_etal-2007-Uncertainty-EMS

  be broader than stated? (7) Further elicit and specify the distribution (shape and percentiles or characterising parameters). (8) Verify with the expert that the distribution that you constructed from the expert’s re- sponses correctly represents the expert’s beliefs. (9) Decide whether or not to aggregate the distributions elicited from dif- ferent experts (this only makes sense if the experts /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

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

  regimes of Number of flood and drought disasters in the past decades per case study 0 2 4 6 8 10 12 1977-1986 1987-1996 1997-2006 Time period Total number of flood and drought disaster s Rivierenland Alentejo Upper Tisza - Hungary Upper Tisza - Ukraine Fig. 1 Number of reported flood and drought disasters in the past decades in Rivierenland, Alentejo, Hungarian part of Upper Tisza, and Ukrainian /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 24. 2010_005_

  decade within the 2004–50 period, for the UKMO HadCM3, and the MPI ECHAM5-r3. . . . . . . . . . . . . 28 7 Mean annual surface air temperature and total precipitation during the 1961–90 control period, and linear trends within the 1958–2001 period, for the ERA-40 reanalyses. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 29 8 Differences between the RCM and underlying /media/ces/2010_005_.pdf

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

  of the glaciers. An up to 8 m thick winter snow layer was measured in the accumulation area (∼4 m w.e.). Ice melt of up 10 m w.e. was measured in the lowest part of the ab- lation zone in summer, and 2 m w.e. was melted during win- ter. Taking into account ∼2 m of annual rainfall, the runoff from this part of the glacier was estimated as ∼14 m w.e. per year; a surprisingly high value (Ahlmann, 1939 /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 26. Forecasts - Gufuskálar

  GMT 4° ENE 10 Cloud cover: 100% 20 GMT 3° ENE 10 Cloud cover: 100% 21 GMT 2° ENE 9 Cloud cover: 0% 22 GMT 2° ENE 8 Cloud cover: 0% 23 GMT 1° ENE 8 Cloud cover: 0% Tue 2.05 00 GMT 1° ENE 7 Cloud cover: 0% 01 GMT 1° ENE 8 Cloud cover: 0% 02 GMT 1° ENE 8 Cloud cover: 0% 03 GMT 1° ENE 8 Cloud cover: 0% 04 GMT 0° ENE 8 /m/forecasts/areas

• 27. Journal_of_Hydrology_Veijalainen_etal

  ; fax: +358 20 490 2590. E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen). Journal of Hydrology 391 (2010) 333–350 Contents lists available at ScienceDirect Journal of Hydrology journal homepage: www.elsevier .com/ locate / jhydrol Author's personal copy narios from GCMs or RCMs, and with different emission scenarios (e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 28. BIHN_windrose_2005-2014

  Wind rose BIHN 2005 − 2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 1 2 3 4 5 6 Frequency of wind direction (%) Aerodrome Total observations: 28301 Calm: 5.3% Variable winds: 1.6% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 2 4 6 8 10 0 45 90 135 180 225 270 315 360 N E S /media/vedur/BIHN_windrose_2005-2014.pdf

• 29. Hare-2011-ParticipatoryModelling

  Dispatch: 02.08.11 CE: E E T 5 9 0 No. of Pages: 19 ME: 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Another possible driving force behind its popularity is changing legislation requiring environmental managers and policy-makers to increase stakeholder participation in their work [e.g /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 30. GA_2009_91A_4_Andreassen

  the variations in the seasonal componentsof the mass balance; – use the model to reconstruct the mass balanceprior to 1949; – study the sensitivity of the model to differentmodel set ups and choices of parameters; – and study the climate sensitivity of the glacierand implications of climate change on the massbalance. SettingStorbreen (61°36' N, 8°8' E) is located in the Jotun-heimen mountain massif /media/ces/GA_2009_91A_4_Andreassen.pdf