net balances are wellcorrelated and (obviously) best modelled as the
sum of bw measured and bs modelled (bs-m2). Thebest obtained correlations of modelled bw (0.86), bs(0.87) and bn (0.94) for 1949–2006, show that themodel could explain 73, 76 and 88% of the variance
over this period.From each year we also extracted the day with
maximum bw (bwd) and minimum bs (bsd, mini-mum values as bs is negative
/media/ces/GA_2009_91A_4_Andreassen.pdf
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
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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf