32 results were found for WA 0821 1305 0400 Pusat Pembuatan Pagar Semi Tempa Caringin Kab Bogor.

Results:

• 21. Hare-2011-ParticipatoryModelling

  ea th , th e m et ho d u se d at th is st ag e fo r th es e st ak eh o ld er typ es is sp ec i
  ed .Sh oul d ther e be tw o o r mor e model sbein g develope d in th e process ,the n th e typ e o fmode lt o whic h th e metho d wa s applie d is show n in parentheses .O T re fe rs to th e co m po si tio n o ft he o rg an iz in g te am . Fo r o rg an iz in g te am in vo lve m en t in di ffe re n t pa rt /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 22. 2010_003rs

  /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 23. Keskitalo_et_al-MLG_and_adaptation_FINAL

  on national to local levels Characteri stics States Adaptation policy development Political system Sub-national case study areas (specific nested local authorities or municipalities in brackets) Semi- structured interviews UK (England) Often seen as leader with multi-level perspective, Centralised administration (with regard SouthEast England region (Hampshire and Surrey /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 24. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  basin water management into more adaptive regimes that are better able to deal with changing conditions? late In inter othesis and produced an interview guide for a 12 h tative semi-structured interview. After listening to the view and selecting sequences addressing our research ions, we transcribed these to written text which we r condensed and analysed using three different theore- hyp managers 4.1 /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 25. VI_2014_001

  WaSiM-ETH (Schulla and Jasper, 2007; Atladóttir et al., 2011; Þórarinsdóttir, 2012) was calibrated on 4 gauged catchments (vhm19, vhm38, vhm51 and vhm52). A semi-automatic multi-objective optimization based on the analysis of discharge information was used to assist in the selection of best model parameters for each catchment (Crochet, 2012d). The model was then used to simulate daily streamflow /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 26. VI_2015_005

  wintertime winds over Greenland, it can be assumed that positive changes in the zonal wind component are mostly due to a weakening of the large-scale circulation. Through the geostrophic wind relationship, this implies a weakening of the northward pressure gradient, and therefore a weakening of the Icelandic Low, relative to the semi-permanent high-pressure region over Greenland. The positive /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 27. Daniell_etal-2010

  are listed in a separate list in the Appendix, and most of them are available online. In order to thoroughly plan, establish, and evaluate the workshops and elicit answers to our research questions, we conducted in-depth interviews. These were semi-structured, guided face-to-face interviews, as well as telephone interviews, with the collaboration partners and workshop participants /media/loftslag/Daniell_etal-2010.pdf

• 28. Kok_et_al._TFSC_published_2011

  /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 29. Refsgaard_etal-2007-Uncertainty-EMS

  of the local optimisation routines based on non-linear regression, is that the prediction of interest is treated as an obser- vation, and the regression algorithm is then used to quantify the effect of the parameter uncertainty on this ‘‘observation’’. Some methods rely on a semi-analytical solution in which the regres- sion algorithm is used to compute either a predictive uncertainty interval /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 30. Reykholt-abstracts

  fields); automated feature tracking (using the VISICORR software (Dowdeswell and Benham, 2003)); and a semi-automated Fourier-transform based cross- correlation technique. In this paper, we extend this analysis to investigate the impact of various pre-processing steps (such as slope shading of the surface derived from the point cloud); the impact of the window size used to calculate the Fourier /media/vatnafar/joklar/Reykholt-abstracts.pdf