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• 31. ces-oslo2010_proceedings

  Resources and Energy Directorate Edited by: Heidi H. Pikkarainen Print: Norwegian Water Resources and Energy Directorate Number printed: 130 Cover design: Rune Stubrud Prepared for: The CES project Norwegian Water Resources and Energy Directorate Middelthunsgate 29 P.O. Box 5091 Majorstua N-0301 OSLO NORWAY Telephone: +47 22 95 95 95 Fax: +47 22 95 90 00 /media/ces/ces-oslo2010_proceedings.pdf

• 32. Horsens_breakout_12August

  The group should imagine itself as a policy agency responsible for designing a long term (20 years) planning process that should enable the society to cope with the climate change effects and its uncertainties and develop a climate change adaptation strategy. We will form two groups with slightly different topics as described in the terms of references below. Each group should have 3-4 /media/loftslag/Horsens_breakout_12August.pdf

• 33. VI_2020_008

  .............................................................................................................. 20 3.1 Block Maxima ....................................................................................................................... 21 3.2 Peak-over-Threshold ............................................................................................................. 22 3.3 Estimation /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 34. Water_resources_man_Veijalainen_etal

  Based on a report by Verta et al. (2007) 92. 5 93. 0 93. 5 94. 0 94. 5 95. 0 M A MJ F J J A S O N D Mean 19702000 Min and max 1970–2000, natural rating curve Target water level zone 1 Target water level zone 2 Q=+20% Q=+10% Q= 0% Q=15% Q=30% 92.90 m snow target 1 92.70 m snow target 2 Water level (m ) Month the regulation limits Lake Syväri has target water level zones, which are not legally /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 35. 2011_005

  ....................................................................................................19 5.1.2 Shared servers ...............................................................................................19 5.2 Automated download of receiver files .....................................................................20 5.3 Processes ..................................................................................................................20 5.3.1 Data retrieval /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

• 36. Keranen_Jaana_CES_2010

  /media/ces/Keranen_Jaana_CES_2010.pdf

• 37. Paper-Olafur-Rognvaldsson_91

  The role of orography was found to be crucial in determining the precipitation dis- tribution and amount. Atmospheric flow over Iceland was simulated for the period January 1961 through June 2006 using version 3–7–3 of the PSU/NCAR MM5 mesoscale model (Grell et al., 1995). The domain used is 123× 95 points, centered at 64◦ N and 19.5◦ W, with a horizontal resolution of 8 km. There are 23 vertical /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

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

  no tcaus e mor e problem si n th e (far )futur e (20 year s o r more ) Vos s et al .( 200 6), Dub e an d Swatu k (200 2), Kicker te t al .( 199 7) Alread y no w preparation s ar e take n fo rth e (far )futur e (20 year s o r more ) Raadgeve re t al .( 200 8), Pahl-Wos te t al .( 2007 c), Vos s et al .( 200 6) 13 .Flexibl e measures , keepin g option s ope n Measure s take n no w o r propose d fo rth /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 39. ice-chart_colour-code-standard

  of land origin ▲• Undetermined or unknown x Table 3.3 Form of ice (Fa Fb Fc Fp Fs) Element Floe size Symbo l Pancake ice - 0 Small ice cake; brash ice < 2 m 1 Ice cake 2-20 m 2 Small floe 20-100 m 3 Medium floe 100-500 m 4 Big floe 500 m-2 km 5 Vast floe 2-10 km 6 Giant floe > 10 km 7 Fast ice - 8 Icebergs, growlers or floebergs - 9 Undetermined or unknown - x - 5 - Annex I Sample ice charts from /media/hafis/frodleikur/ice-chart_colour-code-standard.pdf

• 40. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  adaptation issues and uncertainties with a focus on issues requiring a planning horizon of more than 20 years, when a climate change signal could begin to dominate the natural climate variability, and where a relatively long economic lifetime of adaptation projects makes it important to give careful consideration to uncertainty. In Tables 2, 3, 4 and 5, climate change impacts are characterised /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf