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18 results were found for WA 0852 2611 9277 Anggaran Dana Untuk Membangun Plafon Gypsum Classic Murah Limo Kota Depok.


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  • 11. CES_D2.4_task1

    2609 BEITO NO +61:14:35 +08:51:20 754 P 2610 BIRI NO +60:57:10 +10:35:49 190 P 2611 ABJORSBRATEN NO +60:55:05 +09:17:25 639 TP 2612 BOVERDAL NO +61:43:14 +08:14:39 701 P 2613 ESPEDALEN NO +61:25:00 +09:32:04 752 P 2614 LUNNER NO +60:17:39 +10:34:49 /media/ces/CES_D2.4_task1.pdf
  • 12. VI_2021_008

  • 13. 2010_016

    for. Extended melt approach was used to account for melting on glaciers where the effects of radiation are added to a classic degree-day model. For infiltration, a methodology of Peschke, based on the approach of Green and Ampt, was used. To calculate the fluxes within the unsaturated soil zone, the Richards equation was used. The groundwater table was modelled in both the unsaturated zone module /media/ces/2010_016.pdf
  • 14. 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
  • 15. 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 ied .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
  • 16. Lorenzoni_Pidgeon_2006

    ”); standard deviations are in brackets. Psychometric characteristics Climate change Unknown consequences 4.13 (0.88) Risks to future generations 4.31 (0.73) Dread 3.06 (1.12) Well informed 2.80 (1.14) Control any risks to myself 2.48 (1.07) Unfair distribution of risks 3.00 (1.00) Moral concerns 3.44 (1.03) (Source: Poortinga and Pidgeon, 2003a). change (i.e. the ‘dread’ factor in the classic /media/loftslag/Lorenzoni_Pidgeon_2006.pdf
  • 17. VI_2020_011_en

    of submarine vents identified later in this report. 1.3 Framework of the project The 1973 Eldfell eruption crisis and citizen response on Heimaey provides a classic example of the risks to, and mitigation actions that can be taken by, communities close to volcanoes. The fissure was located only 200 m east of the town, whose infrastructure was significantly harmed by the eruption. Over /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
  • 18. VI_2013_008

    to ensure timely warnings. A classic approach for producing short- and medium-range streamflow forecasts consists of coupling a hydrologic model with a NWP model. The use of hydrologic models at IMO has until now been limited to the simulation of historical and future streamflow series in relation to climate change research projects, water resources management and hydropower planning (Jónsdóttir, 2008 /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

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