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  • 41. 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
  • 42. VI_2015_005

    This is also the case with cyclones in all three sectors. Cyclones in the eastern or western sector are also strongly affected by the presence of central cyclones. In both sectors, cyclones tend to move east, unless there are cyclones in the neighbouring sector, in which case pressure tendencies are reversed. 21 Figure 10. Composite mean temporal MSLP tendencies, for different MSLP modes. Com- posite mean /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
  • 43. 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
  • 44. 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
  • 45. VI_arsskyrsla2020

    climatological work. In 1991 the first Nordic project studying the impact of climate change on hydrol- ogy and hydropower was initiated. It was to be repeated more than a decade later with comprehensive Nordic pro- jects on climate impact on renewable energy resources and energy systems. This led to significant changes in the decision framework of the Nordic energy sector, in many cases reaping /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf
  • 46. Daniell_etal-2010

  • 47. Kok_et_al._TFSC_published_2011

    of individual countries to be excluded from the EU. By 2050, resources are strictly managed and prots are spread over the EU. The gap between the rich and poor countries widens, yet the EU survives. A crucial sector in this scenario is agriculture, both because of the high degree of self-sufciency that is needed and the important role of ‘water for food’. As water resources are limiting, agriculture /media/loftslag/Kok_et_al._TFSC_published_2011.pdf
  • 48. vonKorff_etal-2010

  • 49. VI_2019_009

    To distinguish between rain and snow, the volume is com- pared to the water equivalent but the volume of snow is ten times larger. Figure 1. How PWD22 determines the type of precipitation. Using the information about the changes of the backscatter signal, water equivalent and temper- ature the Vaisala Present Weather Detector can give information about the type of precipitation. It is also used /media/vedurstofan-utgafa-2019/VI_2019_009.pdf
  • 50. VI_2015_007

    moments (PWM) proposed by Hosking et al. (1985b) was adopted to fit the individual GEV distributions at each site and the parameters of the regional growth curve (qR(D;T )) were estimated with the GEV/PWM regionalization algorithm pro- posed by Hosking et al. (1985a), as in Crochet (2012a,b) and Crochet & Þórarinsdóttir (2014). 3.4 Evaluation statistics In order to assess the capacity of the IFM /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

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