A balanced Kalman filter ocean data assimilation system with application to the South Australian Sea. (August 2017)

• Record Type: Journal Article
• Authors: Li, Yi; Toumi, Ralf
• Is Part Of: Ocean modelling. Volume 116(2017:Aug.)
• Page Start: 159
• Page End: 172
• Publication Date: 2017-08
• Subjects: ROMS -- EnKF -- Multivariate balance; Oceanography -- Periodicals; Océanographie -- Périodiques; Oceanography; Periodicals; 551.46
• DOI: 10.1016/j.ocemod.2017.06.007
• Languages: English
• ISSNs: 1463-5003

Abstract

Highlights: A DART/ROMS data assimilation system is developed. Physical constraints are implemented to eliminate the spurious waves. The balance operator improves the estimation of both SSH and velocity in an idealised model. Assimilation improves both SST and SSH in real case and balance operator shows great advantage for ocean current. Abstract: In this paper, an Ensemble Kalman Filter (EnKF) based regional ocean data assimilation system has been developed and applied to the South Australian Sea. This system consists of the data assimilation algorithm provided by the NCAR Data Assimilation Research Testbed (DART) and the Regional Ocean Modelling System (ROMS). We describe the first implementation of the physical balance operator (temperature-salinity, hydrostatic and geostrophic balance) to DART, to reduce the spurious waves which may be introduced during the data assimilation process. The effect of the balance operator is validated in both an idealised shallow water model and the ROMS model real case study. In the shallow water model, the geostrophic balance operator eliminates spurious ageostrophic waves and produces a better sea surface height (SSH) and velocity analysis and forecast. Its impact increases as the sea surface height and wind stress increase. In the real case, satellite-observed sea surface temperature (SST) and SSH are assimilated in the South Australian Sea with 50 ensembles using the Ensemble Adjustment Kalman Filter (EAKF). Assimilating SSH and SST enhances the estimation of SSH and SST in the entire domain, respectively. Assimilation with the balance operator produces a more realistic simulation of surface currents and subsurface temperature profile. The best improvement is obtained when only SSH is assimilated with the balance operator. A case study with a storm suggests that the benefit of the balance operator is of particular importance under high wind stress conditions. Implementing the balance operator could be a general benefit to ocean data assimilation systems.