the results for all catchments, with
that method. The deterministic predictions were also compared to two benchmark determinis-
tic predictions, i) monthly climate in the period 1961–2000, i.e. F(t0 +
D) = E[A(M)], and ii)
persistence, i.e. F(t0 +
D) = A(t0), where F is the forecast and A the observation or analysis.
Figures 5 to 8 present the scatter plots of observed temperature and precipitation versus
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