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User Guide to ECMWF Forecast Products > The ECMWF forecasting and assimilation system > Some characteristics of deterministic NWP > 
Forecast trends cannot be extrapolated The Ensemble Prediction System (EPS)  
   

Other state-of-the-art deterministic models

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Forecast error growth
Downstream spread of influence
The relation between scale and predictive skill
Forecast “jumpiness”
Flip-flopping forecasts
Jumpiness and forecast skill
Forecast trends cannot be extrapolated
Other state-of-the-art deterministic models
 
 

What has been said so far applies, in principle, to all major state-of-the-art deterministic NWP models, spectral- or grid-point-based, global or limited area, hydrostatic or non-hydrostatic. The differences in their average forecast quality are less significant than the daily variability of the scores. Hence, the best NWP model, on average, is not necessarily the best on a particular day. An NWP model that has recently performed significantly better (or worse) than other models (of about the same average skill), is not likely to continue to do so.

However, as mentioned in Section 2.6.2 and further discussed in Section 4.2, it is as difficult to determine the “model of the day” from one of several NWP model forecasts as it is from consecutive forecasts from the same model. Forecasters are advised to treat forecasts from different NWP models as a “multi-model ensemble” whose members differ slightly in their initial conditions and model characteristics. The better forecasters learn to handle the deterministic output in this way, the better they will be able to manage the ensemble forecasts, where these problems are more consistently addressed (see Chapter 4).





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Forecast trends cannot be extrapolated The Ensemble Prediction System (EPS)  
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