47 results were found for WA 0821 1305 0400 Biaya Buat Coating Lantai Vinyl Floor Di Cipayung Jakarta Timur.

Results:

• 31. 2010_017

  m J M5 [C°] -3 obs. [C°] -4 nce 1 re 5. Comp 26); an int temperatu this system y gridded v picion abo -Jökulsá w similar dif han observ h elevation ces the effe months No ly only on high the tem n band wi refore be s onthly tem an Feb Ma .2 -3.1 -3. .3 -4.1 -3. .1 1.0 0.6 arison of m erpolation re is shown atic differe alues, see T ut the qual atershed; b ference wa ations for t gradient fo /media/ces/2010_017.pdf

• 32. VI_2021_008

  /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 33. VI_2014_001

  at each site i with the same method used to estimate qR(D;T ), but instead of pooling AMF series for a given duration D from different sites, the estimation is made individually for each site i by pooling AMF series for different durations D (see Crochet, 2012c). The index flood µi(D), is modeled at each site i as a continuous function of D, as follows: µi(D) = µi 1+(D=Di)li ; (5) where µi, Di /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 34. 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

• 35. Daniell_etal-2010

  participants each, representing relevant interests in the Dhuenn basin (Fig. 3). The aim of the first workshop was to open the floor and create ideas for potential management solutions and measures. It also introduced previously agreed upon measures that resulted from other projects (such as Regionale 2010) or bilateral proceedings (also see Regionale 2010, 2008). The second workshop focused /media/loftslag/Daniell_etal-2010.pdf

• 36. VI_Arsskyrsla_2018_vef

  by the inhabitants on a daily basis for driving between towns and villages for work, school, hobbies or di?erent services. Public avalanche bulletins are also published for selected areas, aimed towards the increasing number of backcountry travellers in Iceland during winter time. The number of human-triggered avalanches recorded by the Meteorological O>ce has increased substantially over /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 37. VI_2009_006_tt

  than can be expected to originate from the cauldrons, three to four times the wa- ter equivalent of the accumulation of snow over the watershed of the cauldrons. It has been estimated that flow from the cauldrons, in addition to the jökulhlaups, could be 2–5 m3 s 1 at maximum (Vatnaskil, 2005). It is possible that part of the sulfate-rich groundwater from the glacier comes from the cauldrons /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 38. VI_2014_005

  with vertical boundary-layer profiles calculated di- rectly from HARMONIE model levels. Due to the temporal and spatial variability of model level heights, for the calculation of average vertical profiles, individual model profiles above 6The large positive bias northeast of Vatnajökull is due to the unusually cold summertime temperatures measured at Station 5932, situated near the edge /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 39. Keskitalo_et_al-MLG_and_adaptation_FINAL

  /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 40. VI_2016_006_rs

  in a collaboration between the Austrian engineering company Ingenieurbüro Illmer Daniel e.U. (DI), Efla consulting engineers and the Icelandic Meteorological Office (IMO). Daniel Illmer carried out the analysis of landslide protection measures, Jón Kristinn Helgason, Tómas Jóhannesson and Eiríkur Gíslason wrote sections about the geographical setting, the land- slide history and the assessment /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf