38 results were found for 【77AGG.COM】citratoto slot marontoto slot login rpr pro apk slot empire88 slot p4x.

Results:

• 31. Hare-2011-ParticipatoryModelling

  to create their own participatory modelling pro- cesses. The article presents the arguments in favour of such a move and then considers the potential barriers, based on two basic conditions that need to be ful
  lled if adoption is to take place:
  rst, that suf
  cient resources are available for water managers to undertake the organization of participatory modelling processes, and secondly /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 32. 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

• 33. vonKorff_etal-2010

  /media/loftslag/vonKorff_etal-2010.pdf

• 34. VI_2013_008

  1987). The dynamical system under study here is the hydrologic response of a watershed to atmo- spheric forcing and physiography, which is governed by complex processes taking place at different spatial and temporal scales. Rather than to attempt to explicitly describe these pro- cesses through hydrological modeling, the analogue method proposed here simply attempts to predict future streamflow /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 35. 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

• 36. Journal_of_Hydrology_Veijalainen_etal

  ) Finland the spring flood peaks are currently by far the largest floods and as they mostly decreased with climate change the magnitude of the annual 2 and 100-year floods decreased. In the north (Fig. 8a) some scenarios still pro- duced large spring floods in 2070–2099. In southern Finland (in the coastal rivers Fig. 8e and in the lake area Fig. 8d) large floods occurred not only in spring but also /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 37. VI_2009_006_tt

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 38. VI_2014_006

  /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf