64 results were found for WA 0821 1305 0400 Jasa Pemborong Interior Set Kamar Lengkap Setiabudi Jakarta Selatan.

Results:

• 21. 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

• 22. 2010_016

  The location of the watersheds (and the two subcatchments of vhm 144, vhm 269 and vhm 167) is shown on Figure 1. 9 Figure 1. Location of the partly glacier covered watershed Austari-Jökulsá, vhm 144 (and its subcatchments vhm 167 and vhm 269) and the non-glacier covered watershed Sandá í Þistilfirði, vhm 26. The WaSiM model (Jasper et al., 2002; Jasper & Kaufmann, 2003) was first set up /media/ces/2010_016.pdf

• 23. IPPC-2007-ar4_syr

  /media/loftslag/IPPC-2007-ar4_syr.pdf

• 24. ces_geus_paakitsoq_full_report

  for melt (Qm) is calculated as follows: Qm = (1 − α)Sin + C0 + C1Ta (2) Where α is the albedo for the surface (three fixed albedo values are applied: snow = 0.8, firn = 0.55 and ice = 0.42), Ta is in ◦C and C0 +C1Ta is the sum of the longwave radiation balance and the turbulent exchange (Oerlemans, 2001). C1 is set to 10 Wm−2 K−1 (Oerlemans, 2001) and C0 is tuned to −45 Wm−2 K−1. Accumulation equals /media/ces/ces_geus_paakitsoq_full_report.pdf

• 25. 2005EO260001

  Dashed lines encompass the V-shaped zone of tephra deposition. (c) Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November. The top portion shows its projection on an EW-vertical plane. The minimum detection height for Grímsvötn is seen at 6 km, and the plume extends /media/jar/myndsafn/2005EO260001.pdf

• 26. 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

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

  the set- tlement, glaciers were smaller than at present. They started to advance in the 13th century at the onset of the Little Ice Age that lasted until late 19th century when most glaciers in Iceland reached their maximum extent. In the 20th century, the climate was significantly warmer than during the Little Ice Age, with higher temperatures in the period 1930–1945 and again at the end /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 28. vonKorff_etal-2010

  ). a71 There are other stakeholders who may need to be involved in the design and then in the participation process itself. a71 There is a set of contextual factors that need to be taken into consideration when designing the participation plan. These can include existing levels of conflict among stakeholders, their previous experiences with participation, relevant legal or regulatory settings /media/loftslag/vonKorff_etal-2010.pdf

• 29. 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

• 30. GA_2009_91A_4_Andreassen

  - elled using precipitation data southwest of the gla- cier. Results from the model compared well with re- ported mass balance values for the period 1949– 2006, obtained correlations (r) for bw and bs varied between 0.83 and 0.87 depending on model set up. Reconstruction of the mass balance series for the period 1924/1925–1948/1949 suggested a cumula- tive mass deficit of c. 30 m w.e. mainly due /media/ces/GA_2009_91A_4_Andreassen.pdf