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Results:

• 51. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 52. Hare-2011-ParticipatoryModelling

  - work. The second half of the article discusses the potential for participatory modelling to progress from being a mainly research-driven activity in the water sector to one being adopted for widespread use by water managers. By widespread adoption I mean that participatory modelling becomes mainstream in the sector and that managers set up their own organizing teams, independent of researchers /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 53. Awards and press

  wanted to drop you guys a line and say thank you. I was in Iceland for 16 days in September surfing, and your web site was so crucial to the trip on knowing when to move and where to go. Keep up the great work. Thanks again.Preparing a visit to Iceland Elizabeth wrote in August 2015: "I just wanted to thank you so much for your wonderful website, which is truly one of the most comprehensive /about-imo/the-web/awards_and_press/

• 54. VI_2014_006

  .................................................................................................. 56 Appendix I Observed versus deterministic temperature forecasts over the period 01/09/2001– 31/08/2006. .................................................................................................. 59 Appendix II Observed versus deterministic precipitation forecasts over the period 01/09/2001– 31/08/2006 /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 55. Machguth_Horst_CES_2010

  experiments with different RCM’s • explore RCM biases • apply a different mass balance model data 2 RCM’s • HIRHAM4, Scenario A1B, 25 km, 1950-2100, Greenland • RCAO, Scenario A1B, 50 km, 1960-2100, Pan-Arctic 4 Weather Stations (Ta, Sin) • GC-Net Swiss Camp: 1150 m a.s.l. (1995 – 2006) • GC-Net Crawford: 2020 m a.s.l. (1995 – 2006) • Asiaq Station 437: 300 m a.s.l. (1983 – 2006) • DMI Illulisat /media/ces/Machguth_Horst_CES_2010.pdf

• 56. VI_2019_009

  .............................. 41 39 From left to right, the horizontal axis has the following SYNOP codes (in groups): 21 - 60,61 - 62,63 - 64,65 - 68 - 80 - 81 - 82. ................................................ 42 40 From left to right, the horizontal axis has the following SYNOP codes (in groups): 22 - 26 - 27,87 - 70,71 - 74....................................................................... 43 /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 57. TietavainenHanna_CES_2010

  the observed data sets are smaller in SW than in NE • MMM overestimates precipitation, but is closer to observations in SW than NE barb2right Better observational coverage in SW SW NE p r e c i p i t a t i o n s u m ( m m ) CES Conference, Oslo 31.5.-2.6.2010 SWNE • Precipitation trends (mm / 10 yr) in 1961-2000 according to observations and model simulations (MMM) • Including the range /media/ces/TietavainenHanna_CES_2010.pdf

• 58. Alam_Ashraful_CES_2010

  FOREST BIOMASS FOR ENERGY PRODUCTION – POTENTIALS, MANAGEMENT AND RISKS UNDER CLIMATE CHANGE Ashraful Alam, Antti Kilpeläinen, Seppo Kellomäki School of Forest Sciences, University of Eastern Finland, Joensuu F t Cli t d R bl E I t Ri k d Ad t tiu ure Cl ma e an enewa e nergy – mpac s, s s an ap a on Oslo, Norway 2 June, 2010 Contents • Forestry in Finland • Challenges • Objectives /media/ces/Alam_Ashraful_CES_2010.pdf

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

  at the operational/local level. A calibrated approach (standardized questionnaires and interviews, expert judgment, and reinterpretation of out- comes by means of relevant literature) was used to com- pare the state of affairs in water management in the selected case-studies. Adaptive and integrated water management Given the expected increase of climate-related extreme events, water governance capabilities /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 60. VI_2015_005

  of Greenland, which is consistent with earlier findings (e.g., Dacre & Gray, 2009; Hanson et al., 2004; Hodges, Lee, & Bengtsson, 2011; Jahnke-Bornemann & Brümmer, 2009; Raible et al., 2008; Schneidereit et al., 2007; Serreze et al., 1993; I. F. Trigo, 2006; Wang, Swail, & Zwiers, 2006; Wernli & Schwierz, 2006). Therefore, whether defined as a local minimum of the seasonal mean MSLP field /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf