78 results were found for WA 0821 1305 0400 Tempat Pasang Pintu Spandrel Aluminium Ukuran Standard Cibarusah Kab Bekasi.

Results:

• 41. Kriauciuniene_Jurate_CES_2010

  feeding Average annual runoff, l/s·km2 10 regional series from Baltic States Long-term regional series of temperature, precipitation and runoff were normalized with reference to the period of 1961- 1990. Precipitation and runoff were normalized by division with mean values. Temperature was normalized by subtraction with the mean and division of the standard deviation. The regional series /media/ces/Kriauciuniene_Jurate_CES_2010.pdf

• 42. Paper-Olafur-Rognvaldsson_91

  ice cap. Red, green and blue crosses represent mean winter balance val- ues at stakes along profiles HN, HSA and HSV respectively within the altitude interval 1440– 1680 metres (cf. Fig. 2). Error bars indicate the standard deviation of the observations. Ob- served values from individual snow stakes are from Sigurðsson et al. (2004), Sigurðsson and Sigurðsson (1998) and Sigurðsson /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 43. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  game allows us to see whether reducing strategic uncertainty, i.e., communicat- ing about others’ contributions to a public good, is Pareto-improving. In standard economic theory, this type of information should be worthless. However, if individual preferences are not those of risk-neutral homo-œconomicus, the experimental results will reveal whether information that reduces strategic uncertainty /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 44. CES_D2.4_VMGO

  and cold wave durations in summer and winter, duration of dry periods and fraction of very heavy precipitation (exceeding 90th quantile) and its duration in summer. The definition of the indices is explained in more detail below. To assess the robustness of simulated changes in the extremes the following metrics are employed: signal-to-noise (a ratio between ensemble mean change and its standard /media/ces/CES_D2.4_VMGO.pdf

• 45. VI_2014_005

  to provide overall better results within the Icelandic forecast domain than other mesoscale models. However, based on the standard model setup and parameterisations, there are systematic biases in 2-m air temperature and 10-m wind speed over the land area of Iceland (de Rosnay et al. (2013), Pálmason et al. (2013); see also the various experiments at http://brunnur.vedur.is/pub/bolli/harmonie/verif /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 46. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  of the three ice caps under consideration, the horizontal displacement of the HRS and DMA DEMs (40 m40 m spatial resolution) relative to the EMISAR DEM (5 m5 m spatial resolution) was eliminated by both maximizing the correlation and minimizing the standard deviation of the elevation differences of ice-free areas in the vicinity of the glaciers (gently sloping areas within ca. 80
  800 m away /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 47. CES_D2.4_task1

  /media/ces/CES_D2.4_task1.pdf

• 48. Refsgaard_etal-2007-Uncertainty-EMS

  be categorised into:  Epistemic uncertainty, i.e. the uncertainty due to imperfect knowledge. can be estimated: e.g. by use of standard flood frequency anal ysis on the basis of existing flow data. The (epistemic) uncer tainty may be reduced by improving the data analysis, making additional monitoring (longer time series) or by deep ening our understanding of how the modelled system works However /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 49. NOMEK09_Report

  course for your work now or in the future? 4,5 Course topics 4,2 Course format (disposition, lectures, exercise/volume) 3,9 Standard of teachers 4,0 Documentation and hands-outs 4,3 Organisation 4,7 How large was the new value for you? 3,8 To what extent did the course fulfil your expectations? 4,3 NOMEK 2009 11-15 May, Reykjavík, Iceland Next course and outlook for the future At the planning /media/vedurstofan/utgafa/skyrslur/2009/NOMEK09_Report.pdf

• 50. CES_D2.4_solar_CMIP3

  incident solar radiation with observations. Red squares: the baseline period (1971-2000) mean of the global radiation observed at Jokioinen in southwestern Fin- land (60.8◦N, 23.5◦E) for each calendar month. The thick black curve: the corresponding quantity as an average of the simulations performed with 18 global climate models. Grey shaded area: mean ± standard deviation of the simulations /media/ces/CES_D2.4_solar_CMIP3.pdf