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Results:

• 21. 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

• 22. 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

• 23. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 24. 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

• 25. 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

• 26. 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

• 27. 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

• 28. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  improving management policies and practices by learning from the outcomes of implemented management strategies. Partici- patory integrated assessment is here a form of problem structuring for identification of gaps, ambiguity and multiple frames, confrontation, and integration of the most divergent views with respect to a given problem situation. Additional methods and tools that AM require com /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 29. GA_2009_91A_4_Andreassen

  the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf

• 30. 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