R. Todling et al., SUBOPTIMAL SCHEMES FOR RETROSPECTIVE DATA ASSIMILATION BASED ON THE FIXED-LAG KALMAN SMOOTHER, Monthly weather review, 126(8), 1998, pp. 2274-2286
The fixed-lag Kalman smoother was proposed recently by S. E. Cohn et a
l. as a framework for providing retrospective data assimilation capabi
lity in atmospheric reanalysis projects. Retrospective data assimilati
on refers to the dynamically consistent incorporation of data observed
well past each analysis time into each analysis. Like the Kalman filt
er, the fixed-lag Kalman smoother requires statistical information tha
t is not available in practice and involves an excessive amount of com
putation if implemented by brute Force, and must therefore be approxim
ated sensibly to become feasible for operational use. In this article
the performance of suboptimal retrospective data assimilation systems
(RDASs) based on a variety of approximations to the optimal fixed-lag
Kalman smoother is evaluated. Since the fixed-lag Kalman smoother form
ulation employed in this work separates naturally into a (Kalman) filt
er portion and an optimal retrospective analysis portion, two suboptim
al strategies are considered: (i) viable approximations to the Kalman
filter portion coupled with the optimal retrospective analysis portion
, and (ii) viable approximations to both portions. These two strategie
s are studied in the context of a linear dynamical model and observing
system, since it is only under these circumstances that performance c
an be evaluated exactly. A shallow water model, linearized about an un
stable basic flow, is used for this purpose. Results indicate that ret
rospective data assimilation can be successful even when simple filter
ing schemes are used, such as one resembling current operational stati
stical analysis schemes. In this case, however, online adaptive tuning
of the forecast error covariance matrix is necessary. The performance
of this RDAS is similar to that of the Kalman filter itself. More sop
histicated approximate filtering algorithms, such as ones employing si
ngular values/vectors of the propagator or eigenvalues/vectors of the
error covariances, as a way to account For error covariance propagatio
n, lead to even better RDAS performance. Approximating both the filter
and retrospective analysis portions of the RDAS is also shown to be a
n acceptable approach in some cases.