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Results:

• 51. Refsgaard_etal-2007-Uncertainty-EMS

  and possibly the stake- holders at different phases of the modelling project. Many QA guidelines exist such as Middlemis (2000) and Van Waveren et al. (1999). The HarmoniQuA project (Schol- ten et al., 2007; Refsgaard et al., 2005a) has developed a com- prehensive set of QA guidelines for multiple modelling domains combined with a supporting software tool, MoST (downloadable via http /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 52. 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

• 53. VI_2019_009

  - 26,83,84 - 27,87 - 70,71 - 72,73 - 74. ............................ 28 21 From left to right, the horizontal axis has the following SYNOP codes (manual station): The first is 10, the second is 11 & 41, the third is 40 and to the right is 46. 29 22 Number of records as a function of height of the 1st cloud layer from the manual and automatic stations /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 54. VI_2015_005

  mean surface air temperature anomalies ....................................... 28 14 Surface air temperature anomalies over Scandinavia ...................................... 29 15 Composite mean precipitation anomalies..................................................... 30 6 1 Introduction Extratropical low-pressure systems, persisting for at least a few days, have long been recognised as one /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 55. Kok_JGEC658_2009

  to be simple and therefore has important drawbacks. Future improvements should be made in the light of applications within a larger toolbox of scenario methods.  2008 Elsevier Ltd. All rights reserved. * Tel.: +31 317 482422; fax: +31 317 419000. E-mail address: kasper.kok@wur.nl. Contents lists available at ScienceDirect Global Environmental Change journa l homepage: www.e lsev ier .com/ locate /media/loftslag/Kok_JGEC658_2009.pdf

• 56. Lorenzoni_Pidgeon_2006

  level, surveys commissioned by the European Com- munity/the European Union provide an indication of trends in concern about cli- mate change. Since 1992, such surveys have been undertaken among representative samples of citizens in its Member States, and specifically on topics related to the environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB in 2002). These have included /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 57. VI_2015_009

  by rescaling a dimensionless regional flood frequency distribution or growth curve, qR(D;T ), com- mon to all sites of the homogeneous region, with the so-called index flood, µi(D), of the target site: bQi(D;T ) = µi(D)qR(D;T ); (1) where bQi(D;T ) is the estimated flood quantile, i.e. the T -year flood peak discharge averaged over duration D, at site i. The regional growth curve, qR(D;T /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 58. 2013_001_Nawri_et_al

  . . . . . . . . . . . . . . . . . 28 9 Weibull shape parameter at 50 and 100 mAGL for all wind directions . . . . . . . 30 10 Average wind power density based on corrected WRF model data . . . . . . . . . 33 11 Average wind power density based on NORA10 data . . . . . . . . . . . . . . . . 34 12 Differences in wind power density between northerly and southerly winds . . . . . 35 13 Directional /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 59. VI_2016_006_rs

  Such landslides fall from a comparatively high elevation, cause extensive disruption and upheaval of loose materials and soils in their way, and can travel considerable distances uphill against opposing slopes. Secondly, there are medium-sized or large, rapid debris flows that are released from com- paratively high elevations and are confined to gullies as they travel down the mountain- side, similar /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 60. VI_2020_004

  ..................................................................................................................... 28 3.5 Power lines ................................................................................................................ 29 3.6 Impact at selected locations ...................................................................................... 30 4 Methodology /media/vedurstofan-utgafa-2020/VI_2020_004.pdf