Disentangling Fine-Scale Wind and Current Contributions to Wave Height and Wave Steepness Gradients in the Gulf Stream Region
The combined effects of fine‐scale wind—arising from air–sea coupling and intrinsic atmospheric dynamics—and current on sea states remain poorly understood, largely due to the scarcity of wave‐model analyses forced with high‐resolution coupled winds.
Authors
- Alexandre Barboni (ORCID: https://orcid.org/0000-0003-4104-9858)
- Gwendal Maréchal (ORCID: https://orcid.org/0000-0003-0378-5694)
- Marco Larrañaga (ORCID: https://orcid.org/0000-0003-0650-6021)
- Franck Dumas
- Lionel Renault (ORCID: https://orcid.org/0000-0002-3001-2091)
Institutions
- Florida State University (US)
- Centre National de la Recherche Scientifique (FR)
- Université Toulouse III - Paul Sabatier (FR)
- École Polytechnique (FR)
- Université Fédérale de Toulouse Midi-Pyrénées (FR)
- Service Hydrographique et Océanographique de la Marine (FR)
- Laboratoire de Météorologie Dynamique (FR)
- Laboratoire d’Études en Géophysique et Océanographie Spatiales (FR)
- Institut de Recherche pour le Développement (FR)
Publication Details
- Published
- 2025-08-25
- DOI
- https://doi.org/10.22541/essoar.175611211.15477792/v1
- Primary Topic
- Ocean Waves and Remote Sensing
- Type
- article
- Field-Weighted Citation Impact
- 0.00