Journal
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY
Volume 140, Issue 682, Pages 1479-1492Publisher
WILEY-BLACKWELL
DOI: 10.1002/qj.2233
Keywords
radiance bias correction; data assimilation; GSI
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Radiance bias correction is an important and necessary step in the proper use of satellite observations in a data assimilation system. The original radiance bias-correction scheme used in the Gridpoint Statistical Interpolation (GSI) data assimilation system consists of two components: a variational air-mass dependent component and a scan-angle component. The air-mass component is updated within the GSI, while the scan-angle component is updated outside the GSI. This study examines and enhances several aspects of the radiance bias-correction problem. First, a modified pre-conditioning is applied to the bias-correction coefficients and the analysis variables to speed up convergence of the minimization process. A new procedure for applying the modified pre-conditioning in the GSI is utilized. Second, capabilities for detecting any new/missing/recovering radiance data and initializing the bias correction for new radiance data are implemented. A new scheme is proposed and employed to adjust the background-error variances for the bias-correction coefficients automatically, using an approximation of the analysis-error variances from the previous cycle, and to remove the pre-specified predictor scaling parameters. Finally, the capability to perform bias correction for passive channels within the GSI is developed with a new approach. The two-step bias-correction procedure originally used is replaced with a one-step variational bias-correction scheme within the GSI. Experiment results with the GSI-based hybrid ensemble-variational system show that using the modified pre-conditioning leads to a better convergence rate. Moreover, with the one-step scheme, the anomaly correlation of geopotential height at 500mb is neutral in the Northern Hemisphere but improved in the Southern Hemisphere. The root-mean-square (RMS) error of wind is comparable to that of the two-step scheme and the biases of the global temperature 24 h and 48 h forecasts fitted to the rawinsonde are reduced.
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