
The atmosphere is a chaotic system, and negligible initial errors will give rise to gradual deviation of the forecast state from the true path, eventually resulting in chaos. This means that the weather has a predictability limit beyond which forecasts will lose all skills. Therefore, any single forecast is simply an estimate of the future state of the atmosphere within a stochastic framework, and provides no information regarding its reliability.
Ensemble prediction offers one approach to generate probabilistic forecasts of the future state of the system based on a statistical sampling approach. In the past two decades, ensemble forecasting has been developed substantially to become a powerful approach that improves numerical weather prediction. Data assimilation schemes were further combined with the dynamical methods to better sample the analysis uncertainties, such as in the ensemble transform Kalman filter (ETKF) scheme.
The concept of ensemble forecasting is depicted schematically in the center, in which it is demonstrated that the initial error will cause the forecast uncertainty. The Lorenz attractor, shown scattered in green, just like the wings of a butterfly, indicates the initial uncertainty. (Image by AAS)
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