Generalized background error covariance matrix model (GEN-BE v2.0)

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Abstract

The specification of state background error statistics is a key component of data assimilation since it affects the impact observations will have on the analysis. In the variational data assimilation approach, applied in geophysical sciences, the dimensions of the background error covariance matrix (B) are usually too large to be explicitly determined and B needs to be modeled. Recent efforts to include new variables in the analysis such as cloud parameters and chemical species have required the development of the code to GENerate the Background Errors (GEN-BE) version 2.0 for the Weather Research and Forecasting (WRF) community model. GEN-BE allows for a simpler, flexible, robust, and community-oriented framework that gathers methods used by some meteorological operational centers and researchers. We present the advantages of this new design for the data assimilation community by performing benchmarks of different modeling of B and showing some of the new features in data assimilation test cases. As data assimilation for clouds remains a challenge, we present a multivariate approach that includes hydrometeors in the control variables and new correlated errors. In addition, the GEN-BE v2.0 code is employed to diagnose error parameter statistics for chemical species, which shows that it is a tool flexible enough to implement new control variables. While the generation of the background errors statistics code was first developed for atmospheric research, the new version (GEN-BE v2.0) can be easily applied to other domains of science and chosen to diagnose and model B Initially developed for variational data assimilation, the model of the B matrix may be useful for variational ensemble hybrid methods as well.

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Descombes, G., Auligné, T., Vandenberghe, F., Barker, D. M., & Barré, J. (2015). Generalized background error covariance matrix model (GEN-BE v2.0). Geoscientific Model Development, 8(3), 669–696. https://doi.org/10.5194/gmd-8-669-2015

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