Articles | Volume 33, issue 3
https://doi.org/10.5194/npg-33-489-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/npg-33-489-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Data assimilation of coherent structures in parametric and gridded spaces: an idealized ocean eddy study
Solène Dealbera
CORRESPONDING AUTHOR
IMT Atlantique, Lab-STICC, UMR 6285, 29238, CNRS, Brest, France
ODYSSEY Team-Project, INRIA Ifremer IMT-Atl., 35042, CNRS, Brest, France
Stéphane Raynaud
Shom, 29200 Brest, France
Carlos Granero Belinchon
IMT Atlantique, Lab-STICC, UMR 6285, 29238, CNRS, Brest, France
ODYSSEY Team-Project, INRIA Ifremer IMT-Atl., 35042, CNRS, Brest, France
Brahim Boussidi
LEGOS Observatoire Midi-Pyrénées, 14 avenue Édouard Belin, 31400 Toulouse, France
Clément Le Goff
LEGOS Observatoire Midi-Pyrénées, 14 avenue Édouard Belin, 31400 Toulouse, France
Pierre Tandeo
IMT Atlantique, Lab-STICC, UMR 6285, 29238, CNRS, Brest, France
ODYSSEY Team-Project, INRIA Ifremer IMT-Atl., 35042, CNRS, Brest, France
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Short summary
The goal of data assimilation in geoscience is to merge information from models and observations. In the presence of structures such as ocean eddies, classic assimilation schemes fail to merge those two sources, resulting in position and shape errors. Here, we propose a new scheme which assimilates only the parameters describing a simplified eddy structure. Comparison with classic schemes shows that our approach preserves the eddy parameters and may reduce the computational cost.
The goal of data assimilation in geoscience is to merge information from models and...