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In total, each set of re-forecasts consists of 20 years x 9 runs x 11 ensemble members = 1980 re-forecast values. These are available for each forecast parameter, forecast lead-time, calendar start date, location, at forecast intervals of 6 hours.
A lhigher number of re-forecasts than for evaluating SUBS-M-climate is justified because the tails are rather more important and it is preferable to have a larger sample size.
The M-climate is used in association with the ensemble forecast:
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