Articles | Volume 8, issue 5
https://doi.org/10.5194/gmd-8-1315-2015
https://doi.org/10.5194/gmd-8-1315-2015
Development and technical paper
 | 
05 May 2015
Development and technical paper |  | 05 May 2015

Structure of forecast error covariance in coupled atmosphere–chemistry data assimilation

S. K. Park, S. Lim, and M. Zupanski

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Cited articles

Buehner, M.: Ensemble-derived stationary and flow-dependent background-error covariances, Q. J. R. Meteorol. Soc., 131, 1013–1043, 2005.
Buehner, M., Houtekamer, P. L., Charette, C., Mitchell, H. L., and He, B.: Intercomparison of variational data assimilation and the ensemble kalman filter for global deterministic NWP. Part I: Description and single-observation experiments, Mon. Weather Rev., 138, 1567–1586, 2010.
Constantinescu, E. M., Chai, T., Sandu, A., and Carmichael, G. R.: Autoregressive models of background errors for chemical data assimilation, J. Geophys. Res., 112, D12309, https://doi.org/10.1029/2006JD008103, 2007.
Eibern, H. and Schmidt, H.: A four-dimensional variational chemistry data assimilation scheme for Eulerian chemistry transport modeling, J. Geophys. Res., 104, 18583–18598, 1999.
Evensen, G.: The ensemble Kalman filter: theoretical formulation and practical implementation, Ocean Dynam., 53, 343–367, 2003.
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Short summary
The structure of an ensemble-based coupled atmosphere-chemistry forecast error covariance is examined using the WRF-Chem, a coupled atmosphere-chemistry model. It is found that the coupled error covariance has important cross-variable components that allow a physically meaningful adjustment of all control variables. Additional benefit of the coupled error covariance is that a cross-component impact is allowed; e.g., atmospheric observations can exert impact on chemistry analysis, and vice versa.
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