46 results were found for WA 0852 2611 9277 RAB Pembuatan Kamar Set Ukiran Mewah Apartemen Podomoro Golf View Bogor.

Results:

• 11. Kok_et_al._TFSC_published_2011

  development is well-suited to the challenges posed by the WFD to develop a long-term view by involving stakeholders. In this paper we analyse the process and results of a series of stakeholder workshops to develop scenarios at pan-European level. Specifically, we aim at analysing the method and results of combining a backcasting methodology and exploratory scenario development process. Four /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 12. 2010_017

  measurements instead of river discharge data. The National Energy Authority has supported this work with contracts on 8 hydrological modelling and groundwater research. The model was then used to make a future projection of runoff for two watersheds in Iceland for the period of 2021–2050 (Einarsson & Jónsson, 2010). The WaSiM model (Jasper et al., 2002; Jasper & Kaufmann, 2003) was first set up /media/ces/2010_017.pdf

• 13. Journal_of_Hydrology_Veijalainen_etal

  The hydrological simulations were performed with the Wa- tershed Simulation and Forecasting System (WSFS) developed and operated in the Finnish Environment Institute (Vehviläinen et al., 2005). The WSFS is used in Finland for operational hydrolog- ical forecasting and flood warnings (www.environment.fi/water- forecast/), regulation planning and research purposes (Vehviläinen and Huttunen, 1997 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 14. Minor jökulhlaup in Grímsvötn

  of October this year. (Click on the image for a larger view)Volcanic activity monitored closely There are examples of volcanic eruptions in Grímsvötn coinsiding with glacial floods. It is likely that the sudden pressure relief due to decreasing water level can trigger eruptions. The last time such a scenario happened was in 2004, and before that in 1934 and 1922. However, Grímsvötn have much more /about-imo/news/minor-jokulhlaup-in-grimsvotn

• 15. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  will continue alongside the gradual anthropogenic climate changes. Figure 1.1. A schematic view of sources of uncertainty in climate change as a function of time (see text for further discussion). The relative importance of these uncertainties depends on the time period considered (Figure 1.1). Scenario uncertainty is very important in the long run. For example, the Intergovernmental Panel /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 16. Group4

  Abackcastingscenario was developed which built upon a set of normative assumptions.These normative assumptionsare intended toestablish a pathway for Finnish society to achieve a low-impact mobility system. The scenarios are designed for use internally within the Finnish Transport Agency to assist in long-range planning and strategic investment, explicitly grounded in adaptive management principles of multiple /media/loftslag/Group4.pdf

• 17. Grimsvotn_status_2011-05-30_IES_IMO

  Since Thursday the tremor had been intermittent. Today, Monday 30 May, it has been confirmed by the participants of Iceland Glaciological Society's spring expedition that the eruption has ended. The end of the Grímsvötn eruption is set to 7 UTC Saturday morning 28 May 2011. /media/jar/Grimsvotn_status_2011-05-30_IES_IMO.pdf

• 18. Hare-2011-ParticipatoryModelling

  - work. The second half of the article discusses the potential for participatory modelling to progress from being a mainly research-driven activity in the water sector to one being adopted for widespread use by water managers. By widespread adoption I mean that participatory modelling becomes mainstream in the sector and that managers set up their own organizing teams, independent of researchers /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 19. BIIS_windrose_2005-2014

  1 6 Wind rose BIIS March 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 2 4 6 8 10 12 Frequency of wind direction (%) Aerodrome Total observations: 2611 Calm: 9.8% Variable winds: 16% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 360 N /media/vedur/BIIS_windrose_2005-2014.pdf

• 20. CES_D2_2_poster_3x3

  @fmi.fi THIS POSTER IS A SUBSET OF A DELIVERABLE REPORT AVAILABLE FROM http://www.atm.helsinki.fi/~jaraisan/CES_D2.2/CES_D2.2.html SOURCES OF UNCERTAINTY IN CLIMATE CHANGE FORECASTS A schematic view of sources of uncertainty in climate change as a function of time. In the long run, most of the uncertainty relates to the magnitude of greenhouse gas emissions (unknown future behaviour /media/ces/CES_D2_2_poster_3x3.pdf