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Results:

• 51. Lettenmaier_Dennis_CES_2010pdf

  Withdrawal Reliability Grand Coulee Recreation Reliability R e l i a b i l i t y ( % , m o n t h l y b a s e d ) Control Period 1 Period 2 Period 3 RCM 2040-2069 60 80 100 120 140 Firm Hydropower Annual Flow Deficit at McNary P e r c e n t o f C o n t r o l R u n C l i m a t e PCM Control Climate and Current Operations PCM Projected Climate and Current Operations PCM Projected /media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf

• 52. Eyjafjallajokull_status_2010-05-07_IES_IMO

  recorded at 5-13 km depth, but fewer than yesterday. GPS deformation: Measurements from around Eyjafjallajökull indicate no major net discplaceaments, suggesting a stabilization of the surface deformation since yesterday. Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64 km distance from the eruption site shows that about 5 % of the ash is smaller /media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf

• 53. James-Smith_Edward_CES_2010

  opportunity evaluation Case studies NOE Net SEAS-NVE Findings of case studies • Distribution companies generally well equipped for climate change – Cabling of all overhead lines well under way – Distribution boxes in areas with increased risk of flooding are elevated already – Salt spray further inland is becoming an increasing problem for substations and transformers Cabling in Denmark /media/ces/James-Smith_Edward_CES_2010.pdf

• 54. VI_2009_012

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 55. CES_D2.4_task1

  /media/ces/CES_D2.4_task1.pdf

• 56. Lorenzoni_Pidgeon_2006

  ). The implications of the present analysis are twofold. Firstly, a risk commu- nication strategy based on providing scientifically sound information alone, even if tailored to individuals’ perceptions of the issue and geared towards correcting 88 I. LORENZONI AND N. F. PIDGEON misinformed opinions (Kempton, 1997), whilst clearly outlining feasible actions individuals can undertake /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 57. IMO_AnnualReport2014

  ANNUAL REPOR T 2014 2 I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 ?Veðurstofa Íslands 2015 Bústaðavegur 7–9, 108 Reykjavík, Iceland The annual report was drafted by the IMO sta?. Editor: Sigurlaug Gunnlaugsdóttir Design and layout: Hvíta húsið Printing: Oddi ISSN 2251-5607 Cover photo: Gro Birkefeldt Møller Pedersen I N D E X 4 Bárðarbunga 7 Rockslide /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 58. AnneFleig_May2010_CES

  E l b e i n D r e s d e n , A p r i l 2 0 0 7 CES conference, Oslo, Norway, 31 May - 2 June 2010 Typical features • develop slowly, • become severe when they cover a large region and persist for an extended period. E l b e i n D r e s d e n , A p r i l 2 0 0 7 ( s p i e g e l . d e ) Anne K. Fleig et al. “Regional hydrological droughts and weather types in north /media/ces/AnneFleig_May2010_CES.pdf

• 59. Publications

  and cold. CE flyer 4. [Flyer] Hisdal, H., Kuusisto, E., Barthelmie, R., Lizuma, L., Lindström, G., Jónsson, P., Kriauciuniene, J., & Reihan, A. (2006). Climate and Energy 2003-2006, Statistical Analysis. CE flyer 5. [Flyer] Rummukainen, M., Christensen, J. H., Ólafsson, H., Jylhä, K., & Førland, E. (2006). Climate and Energy 2003-2006, Climate Scenarios. CE flyer 6. [Flyer] Fidje /climatology/research/ce/publications/

• 60. Crochet_Philippe_CES_2010

  ≤   ≤ >− 0 00 0 )( TTif TTifTTDDFsnow   ≤ >− 0 00 0 )( TTif TTifTTDDFice Mean annual temperature difference Difference relative to 1971-2000 Difference between 25% warmest and 25% coldest years barb2right +1°C (25% warmest) barb2right -0.7°C (25% coldest) barb2right +1.7°C Catchment elevation (m.a.s.l) Catchment elevation (m.a.s.l) s n o w m e l t ( m m / d ) g l a c i a l m e l t /media/ces/Crochet_Philippe_CES_2010.pdf