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Results:

• 71. VI_2017_009

  /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 72. Kok_et_al._TFSC_published_2011

  the backcasting workshop, in plenary this desired end-point that needed to be reached was discussed in detail. In groups, the end-point was modied further to better t with the logic of the exploratory scenario that was used as context. Note that the use of the word ‘end-point’ followed e.g. [29], specically also to distinguish between the very short description of the desired state in 2050 and the rather /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 73. 2010_005_

  which are significantly lower com- pared with similar beginning and end years. Consequently, for the 2004–50 period, the average RCM warming rates of 0.29 K per decade over the ocean, and 0.35 K per decade over the land are somewhat larger than for the reduced IPCC ensemble mean. Additionally, the tabulated values of SAT differences between the 1961–90 control period and either the 2021–50 /media/ces/2010_005_.pdf

• 74. 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

• 75. 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

• 76. 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

• 77. Reykholt-abstracts

  /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 78. Moellenkampetal_etal-2010

  work effectively together? Have there been changes since the co-initiation process? If so, changes on what and why? A more complete description of the evaluation-protocol development and procedures is beyond our scope, but is available in Daniell (2008). For our purposes, we will describe a number of methods of data collection used within the protocols that are relevant to our focus of how project /media/loftslag/Moellenkampetal_etal-2010.pdf

• 79. ces-oslo2010_proceedings

  type rivers is precipitation. The snow melt water rate is almost equal to the groundwater for continental type rivers. Regional patterns of precipitation, temperature and river runoff were done in all Nordic countries (Lindström et al, 2006). Regionalization of territory of the Baltic countries is needful for description of precipitation, temperature and river runoff patterns. Long-term /media/ces/ces-oslo2010_proceedings.pdf

• 80. VI_2020_008

  and 65 vertical levels (Bengtsson et al., 2017). The fine-scale gridding gives 66,181 terrestrial points over Iceland – 40 times greater than those in the current 1M5 calculations. The description of the terrain is therefore much improved. However, it should be noted that even at this resolution the narrowest fjords and dales are not properly resolved. For the most part, the model simulates /media/vedurstofan-utgafa-2020/VI_2020_008.pdf