HR: 1340h
AN: NG23B-0095 INVITED [Abstracts]
TI: Nonlinear Filtering: Ensemble-Based Approaches
AU: * Ueno, G
EM: gen@ism.ac.jp
AF: The Institute of Statistical Mathematics / JST CREST, 4-6-7 Minami-Azabu, Minato-ku, Tokyo, 106-8569
Japan
AU: Higuchi, T
EM: higuchi@ism.ac.jp
AF: The Institute of Statistical Mathematics / JST CREST, 4-6-7 Minami-Azabu, Minato-ku, Tokyo, 106-8569
Japan
AB:
A wide variety of time series models can be represented
within the framework of the state space model.
The state space model is composed by a system equation that
governs the temporal state evolution and by an observation equation
that maps the state to the observation.
The problem of state estimation is to evaluate conditional
distributions, that is, probability density functions of the state
given observations.
The Markovian property of the system equation gives us recursive
formulas for the evaluation of the conditional distributions.
If we assume a linear Gaussian state space model,
we can skip a direct evaluation of the conditional distributions
and it is sufficient to evaluate the mean vectors and the
covariance matrices of the distributions.
Under this assumption, the recursive formulas are automatically
reduced to simpler ones, dealing with the mean vectors
and covariance matrices,
and they are well known as the Kalman filter and the smoothing algorithms.
If we discard the assumption either of linearity or Gaussian,
on the other hand, we have to evaluate the conditional distributions
themselves.
In the ensemble-based filtering approaches,
the conditional distributions are expressed by many of their realizations.
Here three of ensemble-based nonlinear filters are reviewed:
the ensemble Kalman filter (EnKF), the particle filter (PF), and the
Monte-Carlo mixture Kalman filter (MCMKF).
In the EnKF, each of the realization develops according to the
system equation, then is modified by the observation
through the approximated Kalman gain matrix.
In the PF, while the realizations develop in the same way as in the EnKF,
their update step is resampling with weights proportion to
the predictive likelihoods.
The MCMKF deals with multiple models simultaneously, and
the realizations generated from the different models are resampled
with weights of the predictive likelihoods.
Application of these filters to geophysical phenomena are also presented.
DE: 3245 Probabilistic forecasting (3238)
DE: 3260 Inverse theory
DE: 3270 Time series analysis (1872, 4277, 4475)
DE: 3299 General or miscellaneous
SC: Nonlinear Geophysics [NG]
MN: Fall Meeting 2005