Abstract

We systematically compare the performance of ETKF-4DVAR, 4DVAR-BEN and 4DENVAR with respect to two traditional methods (4DVAR and ETKF) and an ensemble transform Kalman smoother (ETKS) on the Lorenz 1963 model. We specifically investigated this performance with increasing non-linearity and using a quasi-static variational assimilation algorithm as a comparison. Using the analysis root mean square error (RMSE) as a metric, these methods have been compared considering (1) assimilation window length and observation interval size and (2) ensemble size to investigate the influence of hybrid background error covariance matrices and non-linearity on the performance of the methods. For short assimilation windows with close to linear dynamics, it has been shown that all hybrid methods show an improvement in RMSE compared to the traditional methods. For long assimilation window lengths in which non-linear dynamics are substantial, the variational framework can have difficulties finding the global minimum of the cost function, so we explore a quasi-static variational assimilation (QSVA) framework. Of the hybrid methods, it is seen that under certain parameters, hybrid methods which do not use a climatological background error covariance do not need QSVA to perform accurately. Generally, results show that the ETKS and hybrid methods that do not use a climatological background error covariance matrix with QSVA outperform all other methods due to the full flow dependency of the background error covariance matrix which also allows for the most non-linearity.

Highlights

  • Hybrid data assimilation methods are becoming more widely used in Numerical Weather Prediction (NWP)

  • For long assimilation window lengths in which non-linear dynamics are substantial, the variational framework can have difficulties finding the global minimum of the cost function, so we explore a quasi-static variational assimilation (QSVA) framework

  • Results show that the ensemble transform Kalman smoother (ETKS) and hybrid methods that do not use a climatological background error covariance matrix with QSVA outperform all other methods due to the full flow dependency of the background error covariance matrix which allows for the most non-linearity

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Summary

Introduction

Hybrid data assimilation methods are becoming more widely used in Numerical Weather Prediction (NWP). The motivation behind hybrid methods is to make use of a flow-dependent background error covariance matrix (Pb) in a variational setting. Their implementation is very similar to the ETKF4DVAR which we used in this paper They use a weak constraint 4DVAR system (named NAVDAS-AR), but their implementation of the background error covariance matrix is a combination of a static error covariance matrix with a flow-dependent error covariance matrix based on an ensemble transform technique of 80 members. They found that a hybrid blend of static and flow-dependent error covariances significantly reduces forecast error in comparison to just using a static error covariance. The final section concludes the paper and gives plans for future work

The hybrid methods
Ensemble Transform Kalman Filter
Ensemble Transform Kalman Smoother
ETKF-4DVAR
Lorenz 1963
Does the initial point change the result?
Improvements from QSVA
Ensemble size versus observation interval
Assimilation window length and observation interval
Findings
Conclusion
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