16 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Baja Fortress Ukuran Mam Nduga.

Results:

• 11. VI_2021_008

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

• 12. VI_2020_004

  /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 13. 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

• 14. Water_resources_man_Veijalainen_etal

  in Lake Pielinen and Lake Saimaa (Table 2), but the seasonal changes were significant (Fig. 4). The water levels increased during winter and decreased during summer months. Student t-tests for the average seasonal (winter [DJF], spring [MAM], summer [JJA], autumn [SON]) water levels showed that in 2040–2069 and 2070–2099 the changes in water levels from the reference period were on average /media/ces/Water_resources_man_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 i
  ed .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. 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