Abstract

Abstract The author uses an approximation of the extended Kalman filter to estimate the forecast and analysis error covariances of an operational assimilation system. The fundamental differences with Kalman filtering are the basic-state trajectory, which is kept close to the operational analyses, and the analysis weights, which follow the usual approximations of optimal interpolation with local data selection. The estimation error covariances for the model state are updated during the analysis and prediction cycles. Although no model error term is specified, the estimation error variances grow according to the dynamics on poorly observed areas. The unbounded error growth found in the Southern Hemisphere has to be limited by a representation of error saturation to account for nonlinearities in the atmosphere. A weak relaxation to climatology is introduced in order to improve the independence on the initial covariances. The behavior of the error variances and correlations is shown to be particularly interes...

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.