The Eta 3D-Var analysis system uses a variable transform that justifies the neglect of cross correlations of the background errors, and applies the isotropic assumption to the auto-correlation functions. The use of the pseudo-relative humidity as the transformed moisture variable leads to some desirable anisotropy in the increments of the specific humidity. We propose to improve the Eta 3D-Var analysis system by relaxing the isotropic assumption for the moisture variable in the transformed space. While retaining the simplicity inherent to the isotropic model, we introduce an exponential factor defined in terms of the model background state and parameterized correlation lengths. The "look-up" tables for the correlation lengths are derived from error statistics obtained with the NMC method. Results from applying this approach will be presented, and a discussion on the extension of the method to the other analysis variables will be offered. The necessary adjustments of the recursive filter used to convolve the observation increments with the background error covariance matrix will also be discussed. Finally, some thoughts on the use of ensemble forecasting to determine the appropriate filtering directions will also be offered.
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