31 results were found for WA 0859 3970 0884 Biaya Jasa Grafiti Tembok 3d Mojosongo Boyolali.

Results:

• 21. 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

• 22. VI_2021_008

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

• 23. IMO_AnnualReport2014

  probably a few meters. An interactive 3D model of the earthquakes during the magma intrusion. The di?rent colours represent the activity in time from 16 August to 12 September. During the magma intrusion, intense earthquake activity related to subsidence of the Bárðarbunga caldera was located at the caldera rim. Over 70 earthquakes above magnitude 5 occurred in the first four months after the onset /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 24. ces_geus_paakitsoq_full_report

  in winter(Fig. 3d). Standard deviation of monthly mean Ta are in reasonable agreement to the observations except for summer and autumn on the ice sheet where the model underestimates (Fig. 4c and d). 5.2 Global Radiation Measurements of global radiation are only available from the stations Swiss Camp and Crawford on the ice sheet for a limited time period (1995–2006), including a number of data gaps /media/ces/ces_geus_paakitsoq_full_report.pdf

• 25. Refsgaard_2-uncertainty

  6 – Nordjylland 9934 47649 Omr. 7 – Bornholm 2358 10106 DK-model - The hydrological model Model code MIKE SHE/MIKE11 • 3D groundwater flow • 2D overland flow • Drain flow (pipes, ditches) • 1D river routing • 1D unsaturated zone, Two- layer module (evapotranspiration) • Degree-day snow melt/accumulation •Borehole data •Geological interpretation •Incorporation of knowledge from more than 50 /media/loftslag/Refsgaard_2-uncertainty.pdf

• 26. 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

• 27. 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

• 28. VI_2014_006

  /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 29. 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

• 30. VI_2020_004

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