Abstract
Straightforward application of the extended Kalman filter yields mixed results. The ability of the extended Kalman filter to track transitions of the double-well system from one stable critical point to the other depends on the frequency and accuracy of the observations relative to the mean-square amplitude of the stochastic forcing. The ability of the filter to track the chaotic trajectories of the Lorenz model is limited to short times, as is the ability of strong-constraint variational methods. Examples are given to illustrate the difficulties involved, and qualitative explanations for these difficulties are provided. -from Authors
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CITATION STYLE
Miller, R. N., Ghil, M., & Gauthiez, F. (1994). Advanced data assimilation in strongly nonlinear dynamical systems. Journal of the Atmospheric Sciences, 51(8), 1037–1056. https://doi.org/10.1175/1520-0469(1994)051<1037:ADAISN>2.0.CO;2
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