Optimization of Salinity Data Assimilation for an Accurate Prediction of Density Variations during Marine Works
Data assimilation improves the accuracy of numerical models by integrating observational data into model predictions, with the ensemble Kalman filter (EnKF) being a widely used technique. Despite its effectiveness, EnKF is often computationally demanding, which limits its practical use in large-scale, high-resolution, and real-time operational models. To overcome this limitation, the present study applied an alternative approach: optimal interpolation (OI). In OI, the Kalman gain was parametrized and precomputed based on prior model statistics, eliminating the need for extensive ensemble simulations. As a result, the computational cost of a data assimilation run becomes comparable to that of a stand-alone hydrodynamic simulation, making it suitable for real-world applications. This method was implemented in TELEMAC-3D, a three-dimensional hydrodynamic modeling software based on the shallow-water equations, and tested in the Scheldt Estuary, where measured salinity data were assimilated into an operational forecasting system supporting a tunnel immersion project near Antwerp of Belgium. The results show that the model maintains stable salinity fields, progressively reduces relative errors over time, and captures the main hydrodynamic conditions in the estuary. These findings demonstrate the potential of OI as a computationally efficient and accurate data assimilation method, suitable for both real-time forecasting and engineering applications in which efficiency and precision are critical.
Authors
- Boudewijn Decrop
- W. Alexander Breugem
- Gert Leyssen
- Kai Chu
- Tijs Cornu
Institutions
- International Marine and Dredging Consultants (BE)
Publication Details
- Journal
- Journal of Waterway Port Coastal and Ocean Engineering
- Published
- 2026-02-04
- DOI
- https://doi.org/10.1061/jwped5.wweng-2421
- Primary Topic
- Oceanographic and Atmospheric Processes
- Type
- article
- Field-Weighted Citation Impact
- 0.00