Abstract

Data assimilation is often performed in a perfect‐model scenario, where only errors in initial conditions and observations are considered. Errors in model equations are increasingly being included, but typically using rather adhoc approximations with limited understanding of how these approximations affect the solution and how these approximations interfere with approximations inherent in finite‐size ensembles.We provide the first systematic evaluation of the influence of approximations to model errors within a time window of weak‐constraint ensemble smoothers. In particular, we study the effects of prescribing temporal correlations in the model errors incorrectly in a Kalman smoother, and in interaction with finite‐ensemble‐size effects in an ensemble Kalman smoother.For the Kalman smoother we find that an incorrect correlation time‐scale for additive model errors can have substantial negative effects on the solutions, and we find that overestimating of the correlation time‐scale leads to worse results than underestimating. In the ensemble Kalman smoother case, the resulting ensemble‐based space–time gain can be written as the true gain multiplied by two factors, a linear factor containing the errors due to both time‐correlation errors and finite ensemble effects, and a nonlinear factor related to the inverse part of the gain. Assuming that both errors are relatively small, we are able to disentangle the contributions from the different approximations. The analysis mean is affected by the time‐correlation errors, but also substantially by finite‐ensemble effects, which was unexpected. The analysis covariance is affected by both time‐correlation errors and an in‐breeding term. This first thorough analysis of the influence of time‐correlation errors and finite‐ensemble‐size errors on weak‐constraint ensemble smoothers will aid further development of these methods and help to make them robust for e.g. numerical weather prediction.

Highlights

  • Data assimilation (DA) combines incomplete and imperfect sources of information of a system to obtain a better estimate of that system, including uncertainties

  • We examine in detail the effect that temporal correlation of model error has on the analysis values over the whole time window

  • Model errors have been ignored in atmospheric data assimilation far too long

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Summary

INTRODUCTION

Data assimilation (DA) combines incomplete and imperfect sources of information of a system to obtain a better estimate of that system, including uncertainties. Besides the direct sampling (Monte-Carlo) error, there is a more subtle indirect sampling error which comes from the use of sample covariance statistics in the gain required in the analysis step of the smoothers These issues were recognised by Houtekamer and Mitchel (1998) and analysed by van Leeuwen (1999), and studied in more detail by Sacher and Bartello (2008) and Furrer and Bengsston (2007) in the filtering setting. We study the interactions between these finite-size sample effects and the errors arising from incorrect specification of the temporal-correlation, or memory, of the model error This is done within a single (forecast/assimilation) time window. For an exponential autocorrelation memory function, we illustrate the propagation of information from observations inside the assimilation window To aid the reader we have underlined the most important expressions which often have significance throughout the whole work

KALMAN SMOOTHER WITH TEMPORAL-CORRELATED MODEL ERROR
The weak-constraint Kalman smoother
Solution in terms of state variables
Illustration in the scalar case
INEXACT TIME CORRELATION AND FINITE ENSEMBLE SIZE
Errors from inexact time autocorrelation
Direct and indirect errors coming from ensemble statistics
Effects of the two sources of imperfection
Small error approximations
Behaviour of the sample estimators
ILLUSTRATION WITH A NUMERICAL EXPERIMENT
SUMMARY AND DISCUSSION
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