54 results were found for 부산진슈얼『텔레그램@uy454』텔레그램@uy454 슈얼광고팀 슈얼광고홍보☎슈얼광고회사㋤슈얼구글 ラ籒 describe.

Results:

• 11. Group2-report

    Temperature  Extreme events  Droughts   Storms  Climate 1  +++  ++/‐‐  +  ++  +  +++  Climate 2  ++  +  +  +    +  Climate 3  ‐  +/‐  +++  ‐  ++  ++    The socio economic conditions in 2050 describe three different worlds, which are represented by the  pictures in Figure 1.      Figure 1: Qualitative description of the three different socio economic set of conditions (Society 1 to 3).   Society 1 /media/loftslag/Group2-report.pdf

• 12. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  ) Use this model to identify policies that are likely to succeed or that probe key uncertainties; (2) being to (1) Work with stakeholders to develop a shared under- standing of the system to be managed and the desirable outcomes, by developing a system model that can be used for policy screening; Wal as a d e social and political values in water resource ment. ters and Holling (1990) describe /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

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

  be adapted to changing climate. Nonstationary hydrologic variables can be modeled stochasti- cally to describe the tem- poral evolution of their pdfs, with estimates of uncertainty. Methods for estimating model parameters can be developed to combine historical and paleo- hydrologic measurements with projections of multiple climate models, driven by multi- ple climate-forcing scenarios. Rapid flow /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 14. Hare-2011-ParticipatoryModelling

  of events, • participatory methods used, • participation mode, • skills needed to organize and implement the participatory modelling. The following subsections describe the criteria and their criterion (in italics) used to classify the participatory modelling nine process examples in Tables T22 and T33. Participatory Modelling Purpose This refers to the purposes that the participatory modelling /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 15. Kok_2-scenarios-lecture-2

  Vliet, M., Kok, K., Veldkamp, T. 2010. Linking stakeholders and modellers in scenario studies; the use of Fuzzy Cognitive Maps as a communication and learning tool. Futures 42(1): 000-000. In press. Souza Soler de, L., Kok, K., Câmara, G., Veldkamp, T. In prep. Using Fuzzy Cognitive Maps to describe current system dynamics and develop land cover scenarios: a case study in the Brazilian Amazon /media/loftslag/Kok_2-scenarios-lecture-2.pdf

• 16. Refsgaard_etal-2007-Uncertainty-EMS

  out? Who will do the modelling work? Who should do the technical reviews? Which stake- holders/public should be involved and to what degree? What are the resources available for the project? The water manager needs to describe the problem and its context as well as the available data. A very important (but often over- looked) task is then to analyse and determine what are the various requirements /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 17. 2011_005

  stations in Figure 2. Figure 2. Stations for national network – suggested and existing. 4.3 Preferred locations of stations for volcano monitoring A simple but very useful model to describe crustal deformation, associated with magma movement and volcanic eruptions, is the Mogi model, which describes deformation at the surface of an elastic half-space. It is specified using four parameters /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

• 18. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  uncertainty in various contexts of importance for IWRM. Refsgaard et al. (2007) describe guidance and tools related to the modelling process and its interaction with the water management process. Van Asselt and Rotmans (2002) describe uncertainty in integrated assessment modelling, i.e. in a broader context with focus on the decision process and the external societal factors. Dewulf et al. (2005 /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 19. VI_2019_009

  measurements in meters, with a maximum visibility of 20 km, then an hour table is based on 10 minute average values. Both manual and automatic records are rounded to the next kilometer and combined in a table with concurrent time. Present weather The manual observations are done every three hours where SYNOP codes are used to describe present weather, while the automatic stations record instantaneous /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 20. 2010_017

  (Hjartarson, 1994b) and a geological map by Jóhannesson and Sæmundsson (1998). During the implementation of the groundwater module two internal errors in WaSiM were encountered. Both errors caused artificial creation of water as certain cells started to act as an inexhaustible source of water. One of the error emerged when it was initially tried to describe the hydrological properties of a watershed /media/ces/2010_017.pdf