1. Data assimilation with residual nudging
A finite, often small, ensemble size has some well-known effects that may substantially influence the behavior of an ensemble Kalman filter (EnKF). These effects include, for instance, rank deficient sample error covariance matrices, systematically underestimated error variances, and, in contrast, exceedingly large error cross covariances of the model state variables (Whitaker and Hamill 2002). In the literature, the latter two issues are often tackled through covariance localization (Hamill et al. 2001), while the first issue, underestimation of sample variances, is often handled by covariance inflation (Anderson and Anderson 1999), in which one artificially increases the sample variances, either multiplicatively (see, e.g., Anderson and Anderson 1999; Anderson 2007, 2009; Bocquet and Sakov 2012; Miyoshi 2011) or additively (see, e.g., Hamill and Whitaker 2011), or in a hybrid way by combining both multiplicative and additive inflation methods (see, e.g., Whitaker and Hamill 2012), or through other ways such as relaxation to the prior (Zhang et al. 2004), multischeme ensembles (Meng and Zhang 2007), modification of the eigenvalues of sample error covariance matrices (Altaf et al. 2013; Luo and Hoteit 2011; Ott et al. 2004; Triantafyllou et al. 2013), or back projection of the residuals to construct new ensemble members Song et al. (2010), to name but a few. In general, covariance inflation tends to increase the robustness of the EnKF against uncertainties in data assimilation (Luo and Hoteit 2011) and, often, also improves the filter performance in terms of estimation accuracy.
The focus of this article is on the study of the effect of covariance inflation from the point of view of residual nudging (Luo and Hoteit 2012). Here, the “residual” with respect to an m-dimensional system state x is a vector in the observation space, defined as






































In Luo and Hoteit (2012), we introduced DARN to the analysis
2. Covariance inflation from the point of view of residual nudging











Our objective here is to examine under which conditions the residual norm

































































Depending on the signs and magnitudes of μmax and μmin, there are in general four possible scenarios: (a) μmax ≥ 0 and μmin ≥ 0, so that ‖Φ‖2 = μmax; (b) μmax ≤ 0 and μmin ≤ 0, so that ‖Φ‖2 = −μmin; (c) μmax ≥ 0, μmin ≤ 0, and μmax + μmin ≥ 0, so that ‖Φ‖2 = μmax; and (d) μmax ≥ 0, μmin ≤ 0, and μmax + μmin ≤ 0, so that ‖Φ‖2 = −μmin. Inserting (21) into the above conditions, one obtains some inequalities with respect to the variables δ and γ (subject to δ > 0 and γ > 0), which are omitted in this paper for brevity.




























Inequality (25) suggests that the upper and lower bounds of γ are related to the minimum and maximum eigenvalues of
























3. Numerical verification
Here, we focus on using the 40-dimensional Lorenz 96 (L96) model (Lorenz and Emanuel 1998) to verify the above analytic results, while more intensive filter (with residual nudging) performance investigations are reported in Luo and Hoteit (2012). The experiment settings are the following. A reference trajectory (truth) is generated by numerically integrating the L96 model (with the driving force term F = 8) forward through the fourth-order Runge–Kutta method, with the integration step being 0.05 and the total number of integration steps being 1500. The first 500 steps are discarded to avoid the transition effect, and the remaining 1000 steps are used for data assimilation. To obtain a long-term “background covariance”
For distinction later, we call the ETKF without residual nudging the normal ETKF, and the ETKF with residual nudging the ETKF-RN. In the normal ETKF, (6) is used for the mean update, with
In the ETKF-RN, we adopt the hybrid scheme
An additional remark is that the normal ETKF and the ETKF-RN share the same square root update formula as in Wang et al. (2004), where it is the sample error covariance
The procedures in the ETKF-RN are summarized as follows. Because the matrix
The experiment below aims to show that, at each data assimilation cycle, if a γ value lies in the interval
Figure 1 shows the time series of the background (dashed–dotted) and analysis (thick solid) residual norms in different filter settings (for convenience of visualization, the residual norm values are plotted in the logarithmic scale). For reference we also plot the targeted lower and upper bounds (dashed and thin solid lines, respectively),

Time series of the analysis residual norms in (a) the normal ETKF without residual nudging and (b)–(f) the ETKF-RN with the following different c values: (b) 0, (c) 1, (d) [0, 1], (e) 2.5, and (f) −0.005. For the normal ETKF there are no targeted lower and upper residual norm bounds. For reference, though, we still plot the targeted upper bound
Citation: Monthly Weather Review 141, 10; 10.1175/MWR-D-13-00067.1

Time series of the analysis residual norms in (a) the normal ETKF without residual nudging and (b)–(f) the ETKF-RN with the following different c values: (b) 0, (c) 1, (d) [0, 1], (e) 2.5, and (f) −0.005. For the normal ETKF there are no targeted lower and upper residual norm bounds. For reference, though, we still plot the targeted upper bound
Citation: Monthly Weather Review 141, 10; 10.1175/MWR-D-13-00067.1
Time series of the analysis residual norms in (a) the normal ETKF without residual nudging and (b)–(f) the ETKF-RN with the following different c values: (b) 0, (c) 1, (d) [0, 1], (e) 2.5, and (f) −0.005. For the normal ETKF there are no targeted lower and upper residual norm bounds. For reference, though, we still plot the targeted upper bound
Citation: Monthly Weather Review 141, 10; 10.1175/MWR-D-13-00067.1
4. Discussion and conclusions
We derived some sufficient inflation constraints in order for the analysis residual norm to be bounded in a certain interval. The analytic results showed that these constraints are related to the maximum and minimum eigenvalues of certain matrices [cf. (11)]. In certain circumstances, the constraint with respect to the minimum eigenvalue [e.g., (13)] may impose a nonsingularity requirement on relevant matrices. A few strategies in the literature that can be adopted to address or mitigate this issue are highlighted.
Some remaining issues are manifest in our deduction. These include, for instance, the nonlinearity in the observation operator and the choice of βu and βl. For the former problem, under a suitable smoothness assumption on the observation operator, one may also obtain inflation constraints similar to those in section 2. On the other hand, though, more investigations may be needed to make the results more practical in terms of computational complexity. For the latter problem, numerical results in Luo and Hoteit (2012) show that the β values influence the overall performance of the EnKF in terms of filter stability and accuracy. Intuitively, smaller (larger) β values tend to make residual nudging happen more (less) often. Therefore, if the normal EnKF performs well (poorly), then a larger (smaller) β value may be suitable. In this aspect, it is expected that an objective criterion is needed. This will be investigated in the future.
Acknowledgments
We thank two anonymous reviewers for their constructive comments and suggestions. The first author would also like to thank the IRIS/CIPR cooperative research project “Integrated Workflow and Realistic Geology,” which is funded by industry partners ConocoPhillips, Eni, Petrobras, Statoil, and Total, as well as the Research Council of Norway (PETROMAKS) for financial support.
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In the literature, the vector with the opposite sign, y −
An exception is in the case that γ = +∞ and ξl = 1. This implies that
One may also let