4.6 Article

Lagrangian Data Assimilation for Improving Model Estimates of Velocity Fields and Residual Currents in a Tidal Estuary

期刊

APPLIED SCIENCES-BASEL
卷 11, 期 22, 页码 -

出版社

MDPI
DOI: 10.3390/app112211006

关键词

estuary; hydrodynamic model; Lagrangian assimilation; Eulerian assimilation; residual currents; OpenDA

资金

  1. Australian Research Council [LP150101172]
  2. Australian Research Council [LP150101172] Funding Source: Australian Research Council

向作者/读者索取更多资源

The study demonstrates that assimilating Lagrangian data obtained from GPS-tracked drifters into a tidal channel for a few hours can significantly improve the modeled velocity fields (up to 30% herein). Additionally, a 40% improvement in residual current direction was achieved when assimilating both Lagrangian and Eulerian data.
Numerical models are associated with uncertainties that can be reduced through data assimilation (DA). Lower costs have driven a recent tendency to use Lagrangian instruments such as drifters and floats to obtain information about water bodies. However, difficulties emerge in their assimilation, since Lagrangian data are set out in a moving frame of reference and are not compatible with the fixed grid locations used in models to predict flow variables. We applied a pseudo-Lagrangian approach using OpenDA, an open-source DA tool to assimilate Lagrangian drifter data into an estuarine hydrodynamic model. Despite inherent challenges with using drifter datasets, the work showed that low-cost, low-resolution drifters can provide a relatively higher improvement over the Eulerian dataset due to the larger area coverage of the drifter. We showed that the assimilation of Lagrangian data obtained from GPS-tracked drifters in a tidal channel for a few hours can significantly improve modelled velocity fields (up to 30% herein). A 40% improvement in residual current direction was obtained when assimilating both Lagrangian and Eulerian data. We conclude that the best results are achieved when both Lagrangian and Eulerian datasets are assimilated into the hydrodynamic model.

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