19 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Baja Fortress Prime Kuta Raja Banda Aceh.

Results:

• 11. Water_resources_man_Veijalainen_etal

  winters with very low accumulated snow and high winter runoffs will become more common and the modified regulations should take this into account. Results showed that minimum water levels during summer and early autumn decreased because of longer and warmer summers and decreasing and earlier spring runoff peaks. Since summer is the prime time for recreational use and navigation, it is important /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 12. 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

• 13. VI_2021_008

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

• 14. Keskitalo_et_al-MLG_and_adaptation_FINAL

  /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 15. NONAM_1st_workshop_summary_v3

  policies in public and private organization. The prime theme area of NONAM is: risk management and decision support with respect to adaptation policy development and related investments, notably regarding infrastructures of various kinds (energy, transport, water & sanitation, communication) and the overarching planning and management systems that create the context in which these systems /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 16. 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

• 17. 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

• 18. 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

• 19. Moellenkampetal_etal-2010

  /media/loftslag/Moellenkampetal_etal-2010.pdf