76 results were found for WA 0821 1305 0400 Pemborong Pemasangan Interior Rumah 5 X 12 Di Kebayoran Baru Jakarta Selatan.

Results:

• 21. 2010_017

  ) storage coefficient of interflow ki; (3) drainage density d; (4) the fraction of surface runoff from snowmelt; and (5) the recession constant krec for the decreasing saturated hydraulic conductivity with increasing depth. For the groundwater flow, adjusted parameters (6–7) are the hydraulic conductivity in the X and Y direction. The hydraulic conductivity is adjusted in distributed grids unlike /media/ces/2010_017.pdf

• 22. vonKorff_etal-2010

  Management: Recent Advances in Theory, Practice and Evaluation Designing Participation Processes for Water Management and Beyond Yorck von Korff 1,2, Patrick d'Aquino 3, Katherine A. Daniell 2,4, and Rianne Bijlsma 5 ABSTRACT. This article addresses the question of how to design participation processes in water management and other fields. Despite a lot of work on participation, and especially its /media/loftslag/vonKorff_etal-2010.pdf

• 23. VI_2020_011_en

  Veðurstofa Íslands 2 Almannavarnadeild Ríkislögreglustjóra 3 Jarðvísindastofnun Háskólans 4 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Bologna 5 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Pisa 6 Jarðvísindadeild Háskóla Íslands 7 Agricultural University of Iceland 8 Consultant Skýrsla nr. Dags. ISSN Opin Lokuð VÍ 2020-011 Desember 2020 1670-8261 Skilmálar: Heiti skýrslu /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 24. GA_2009_91A_4_Andreassen

  Kjøllmoenet al. 2007).Storbreen is located just east of the main waterdivide between east and west in southern Norwayand receives precipitation from both directions(Liestøl 1967). The glacier is part of an east–west mass balance transect in southern Norway where mass turnover is largest near the western coast anddecreases towards the drier interior (Andreassen etal. 2005). Storbreen is in this respect /media/ces/GA_2009_91A_4_Andreassen.pdf

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

  6University of Washington, Seattle, WA 98195, USA. 7NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA. *Author for correspondence. E-mail: cmilly@usgs.gov. An uncertain future challenges water planners. Published by AAAS on July 12, 201 1 www.sciencemag.or g Downloaded from 1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574 POLICYFORUM combined with opera- tions /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 26. ces_geus_paakitsoq_full_report

  ). Melt at the margin of the ice sheet seems somewhat overestimated. However, it must be considered that observations from the Paakitsôk stake network are only available from 1982–1987 (Ahlstrøm et al., 2007) and thus exclude more recent years with strongly increased melt. 5 RCM Evaluation The reference period where RCM output is compared to measurements is January 1 1981 to June 1 2006. This period /media/ces/ces_geus_paakitsoq_full_report.pdf

• 27. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  climate changes between the CMIP3 and ENSEMBLES simulations 15 4. Impact of RCM data on forecasts of climate change 18 5. Probabilistic projections of temperature and precipitation change 24 5.1 Best estimates and uncertainty ranges of temperature and precipitation change 24 5.2 How probably will temperature increase (precipitation change) by at least X°C (Y%)? 28 6. Conclusions 34 References /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 28. 2010_016

  the following five parameters were adjusted: (1) Storage coefficient of direct runoff kd; (2) storage coefficient of interflow ki; (3) drainage density d; (4) the fraction of surface runoff from snowmelt; and (5) the recession constant krec for the decreasing saturated hydraulic conductivity with increasing depth. For the groundwater flow, adjusted parameters (6–7) are the hydraulic conductivity in the X /media/ces/2010_016.pdf

• 29. 2010_005_

  scenario, precipitation increased by 10–15% from 1961–90 to 2070–99, and by 5–10% for the lower emitting scenarios (corresponding to approximately 0.5–1% per decade). The CE project also examined RCM results for Iceland based on the HIRHAM model (Haugen and Iversen, 2006). These results showed enhanced warming over the interior of Iceland compared with the coastal zone, and a tendency for enhanced /media/ces/2010_005_.pdf

• 30. Adalgeirsdottir-etal-tc-5-961-2011

  half of the 21st century and the glacier thins and is nearly vanished at the end of the simulation. The average mass balance – elevation relationship for 10 yr periods at the same 50 yr intervals is shown in panel F in Fig. 12. Compar- ison with observed mass balances (Fig. 5) indicates that the degree-day mass balance model simulates the current mass balance distribution of the glacier reasonably /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf