## Abstract We recall a theoretical analysis of the equivalence between the Kalman filter and the fourβdimensional variational (4DβVar) approach to solve dataβassimilation problems. This result is then extended to cover the comparison of the singular evolutive extended Kalman (SEEK) filter with a r
Conditioning and preconditioning of the variational data assimilation problem
β Scribed by S.A. Haben; A.S. Lawless; N.K. Nichols
- Publisher
- Elsevier Science
- Year
- 2011
- Tongue
- English
- Weight
- 234 KB
- Volume
- 46
- Category
- Article
- ISSN
- 0045-7930
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β¦ Synopsis
Numerical weather prediction (NWP) centres use numerical models of the atmospheric flow to forecast future weather states from an estimate of the current state. Variational data assimilation (VAR) is used commonly to determine an optimal state estimate that miminizes the errors between observations of the dynamical system and model predictions of the flow. The rate of convergence of the VAR scheme and the sensitivity of the solution to errors in the data are dependent on the condition number of the Hessian of the variational least-squares objective function. The traditional formulation of VAR is ill-conditioned and hence leads to slow convergence and an inaccurate solution. In practice, operational NWP centres precondition the system via a control variable transform to reduce the condition number of the Hessian. In this paper we investigate the conditioning of VAR for a single, periodic, spatially-distributed state variable. We present theoretical bounds on the condition number of the original and preconditioned Hessians and hence demonstrate the improvement produced by the preconditioning. We also investigate theoretically the effect of observation position and error variance on the preconditioned system and show that the problem becomes more ill-conditioned with increasingly dense and accurate observations. Finally, we confirm the theoretical results in an operational setting by giving experimental results from the Met Office variational system.
π SIMILAR VOLUMES
In the past decade the variational method has been successfully applied in data assimilation problems for atmospheric chemistry models. In 4D-var data assimilation, a minimization algorithm is used to find the set of control variables which minimizes the weighted least squares distance between model
## Abstract Two approaches can be used to solve the variational data assimilation problem. The primal form corresponds to the 3D/4DβVar used now in many operational NWP centres. An alternative approach, called dual or 3D/4DβPSAS, consists in solving the problem in the dual of observation space. Bot
## Abstract Variational data assimilation systems for numerical weather prediction rely on a transformation of model variables to a set of control variables that are assumed to be uncorrelated. Most implementations of this transformation are based on the assumption that the balanced part of the flo
## Abstract The variational data assimilation problem can be solved in either its primal (3D/4DβVar) or dual (3D/4DβPSAS) form. The methods are equivalent at convergence but the dual method exhibits a spurious behaviour at the beginning of the minimization which leads to less probable states than t
## Abstract The Met Office has developed a 4DβVar data assimilation system, which was implemented in the global forecast system on 5 October 2004. This followed a development path based on the previous 3DβVar configuration, with many aspects kept in common. A 4DβVar capability was provided by the i