Abstract

The strong‐constraint formulation of four‐dimensional variational data assimilation (4D‐Var) assumes that the model used in the process perfectly describes the true dynamics of the system. However, this assumption often does not hold and the use of an erroneous model in strong‐constraint 4D‐Var can lead to a sub‐optimal estimation of the initial conditions. We show how the presence of model error can be correctly accounted for in strong constraint 4D‐Var by allowing for errors in both the observations and the model when considering the statistics of the innovation vector. We demonstrate that, when these combined model error and observation‐error statistics are used in place of the standard observation error statistics in the strong‐constraint formulation of 4D‐Var, a statistically more accurate estimate of the initial state is obtained.The calculation of the combined model error and observation‐error statistics requires the specification of model error covariances, which in practice are often unknown. We present a method to estimate the combined statistics from innovation data that does not require explicit specification of the model error covariances. Numerical experiments using the linear advection equation and a simple nonlinear coupled model demonstrate the success of the new methods in reducing the error in the estimate of the initial state, even in the case when only the uncorrelated part of the model error is accounted for.

Highlights

  • Four-dimensional variational data assimilation (4D-Var) is a method for combining a time window of observations with a model

  • We propose that use of the combined model-error and observation-error covariance matrix R∗ (14), as opposed to R, in the cost function (4), will statistically improve the analysis accuracy when random error is present in the model

  • We find that accounting for errors in the model with the combined error statistics reduces the number of minimization iterations required to reach the tolerance level

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Summary

Introduction

Four-dimensional variational data assimilation (4D-Var) is a method for combining a time window of observations with a model. The model equations are often implemented as a strong constraint within the 4D-Var algorithm (SC4DVar) This assumes that the observations over the time window (accounting for the observation-error statistics) are consistent with the model if initialized with the true state. Instead of trying to correct the model, a method is developed to account for the model error when comparing the model evolution to the observations by combining the modelerror and observation-error statistics This is seen to effectively inflate the observation errors over time, giving the observations nearer the end of the time window less weight in the analysis.

Observations and background
Strong-constraint 4D-Var
The effect of an erroneous model in strong-constraint 4D-Var
Improvements to analysis accuracy
An alternative 4D-Var approach
Simple scalar example
Estimation of the combined model-error and observationerror statistics
Linear advection equation
Idealized coupled atmosphere–ocean model
Estimation of the combined error statistics
Use of combined error statistics in 4D-Var
Sensitivity of results
Findings
Conclusion

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