39 results were found for WA 0821 1305 0400 Tukang Batu Paving Block K300 Teluknaga Kab Tangerang.

Results:

31. VI_2021_008

/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
32. 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
33. Bardarbunga_kafli20140825

is underlain by a dense intrusive complex (probably gabbro), about 12 km in diameter. Below the centre of the caldera, material with lower density occurs, possibly a caldera fill, a subsided block or both. Existence of magma chamber is uncertain. If a shallow level magma chamber exists below the Bárðarbunga volcano a likely location is at the base of the lower density region. Earthquakes occur /media/jar/Bardarbunga_kafli20140825.pdf
34. 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
35. 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
36. Gudmundsson-etal-2011-PR-7282-26519-1-PB

Icelandic glaciers. Jo¨kull 58, 365386. Bjo¨rnsson H., Pa´lsson F. & Haraldsson H.H. 2002. Mass balance of Vatnajo¨kull (19912001) and Langjo¨kull (19962001), Iceland. Jo¨kull 51, 7578. Bouillon A., Bernard M., Gigord P., Orsoni A., Rudowski V. & Baudoin A. 2006. SPOT 5 HRS geometry performance: using block adjustments as a key issue to improve quality of DEM generation. ISPRS Journal /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
37. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

on an already dense area might be beneficial for the developer and for the buyer, but the decision to build more homes will also entail negative externalities for the public; it might deteriorate urban ecosystem services (e.g. remove parks and trees or block the sea view) and increase the problems that already exist in urban areas (e.g. urban flooding enhanced by nonporous surfaces or the heat /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
38. ces-oslo2010_proceedings

/media/ces/ces-oslo2010_proceedings.pdf
39. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf