Optimality of variational data assimilation and its relationship with the Kalman filter and smoother

Authors
Citation
Zj. Li et Im. Navon, Optimality of variational data assimilation and its relationship with the Kalman filter and smoother, Q J R METEO, 127(572), 2001, pp. 661-683
Citations number
62
Categorie Soggetti
Earth Sciences
Journal title
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY
ISSN journal
00359009 → ACNP
Volume
127
Issue
572
Year of publication
2001
Part
B
Pages
661 - 683
Database
ISI
SICI code
0035-9009(200101)127:572<661:OOVDAA>2.0.ZU;2-W
Abstract
The known properties of equivalence between four-dimensional variational (4 D-Var) data assimilation and the Kalman filter as well as the fixed-interva l Kalman smoother point to particular optimal properties of 4D-Var. In the linear context, the 4D-Var solution is optimal, not only with respect to th e model trajectory segment over the assimilation time interval, but also wi th respect to any model state at a single observation time level; in the ba tch processing (cycling 4D-Var) method, the information in 4D-Var is fully transferred from one batch to the next by the background term; 4D-Var allow s the processing of observations in subsets, while the final solution is op timal as all observations are processed simultaneously. These properties ho ld even for models that are imperfect, as well as not invertible. Various p roperties of equivalence of 4D-Var to the Kalman filter and smoother result from these optimality properties of 4D-Var. Further, we show that the fixe d-lag Kalman smoother may also be constructed in an optimal way using a mul tiple batch-processing 4D-Var approach. While error covariances are crucial for the equivalence, practical techniques for evaluating error covariances in the framework of cycling 4D-Var are discussed.