51 results were found for 【K528.COM】ChatGPT账号GPT-5.2Plus/Pro会员出售 hml7k.

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• 21. 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

• 22. VI_2009_006_tt

  to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 23. 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

• 24. 2013_001_Nawri_et_al

  However, these regions above 1000 mASL are glaciers, and are not relevant for wind energy pro- duction. The highest wintertime wind speeds at 50 mAGL over near-coastal terrain in the western part of the island are reduced from 11 – 12 m s 1 to around 10 m s 1, whereas over intermedi- ate terrain in the interior, wind speed is increased from around 7 m s 1 to around 10 m s 1 (not shown). 24 Figure 6 /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 25. CES_D2.4_solar_CMIP3

  %, for several months less than 2%. The good accordance encourages utilization of the models to construct future pro- jections. Admittedly, there is quite a large scatter among the various models, and conse- quently one is more justified to base the projections on the entire ensemble of the models rather than on any individual model. 2 ESTABLISHMENT OF THE PROJECTIONS The output of the model simulations /media/ces/CES_D2.4_solar_CMIP3.pdf

• 26. Milly_etal-2008-Stationarity-dead-Science

  hedged against small climate changes. Additionally, climate projec- tions were not considered credible (12, 14). Recent developments have led us to the opinion that the time has come to move beyond the wait-and-see approach. Pro- jections of runoff changes are bolstered by the recently demonstrated retrodictive skill of cli- mate models. The global pattern of observed annual streamflow trends /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 27. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  296 Public Choice (2010) 143: 293–301 2 The commons The literature on the commons, or what is more technically defined as common-pool re- sources (CPRs), should be viewed initially from its place in the larger literature on dilem- mas of collective action. Since the foundational work of H. Scott Gordon (1954) on the com- mons, and Mancur Olson (1965) on collective action more broadly, the behavioral /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 28. Climate Report

  fields.The glacial retreat has led to significant changes in hydrological conditions as the course of glacial rivers has been altered, new pro-glacial lakes have been formed, while existing ones have become more extensive or, in some cases, dried up. In 2009, the river Skeiðará altered its course and joined with the river Gígjukvísl, leaving an 880 m long bridge running over mostly dry riverbed /climatology/iceland/climate-report

• 29. Climate Report

  fields.The glacial retreat has led to significant changes in hydrological conditions as the course of glacial rivers has been altered, new pro-glacial lakes have been formed, while existing ones have become more extensive or, in some cases, dried up. In 2009, the river Skeiðará altered its course and joined with the river Gígjukvísl, leaving an 880 m long bridge running over mostly dry riverbed /climatology/iceland/climate-report/

• 30. Paper-Olafur-Rognvaldsson_91

  of such an approach is that it is relatively inexpensive in terms of computer resources used for simulations of the atmospheric flow at relatively high spatial and temporal resolutions. As resolution is increased, pro- cesses governed by the interaction of the large scale flow and topography be- come better resolved by the models. One drawback of this approach which is not present in global /media/ces/Paper-Olafur-Rognvaldsson_91.pdf