Field measurements of wave and flow dynamics along a high-energy meso-macrotidal coast adjacent to a large estuary mouth

The North-Médoc coast, located to the south of the Gironde estuary, exhibits complex hydrodynamic conditions driven by high-energy incident waves and large tides, which are influenced by large-scale rocky outcrops, shoals, and tidal channels on the inner shelf. These wave- and tide-driven hydrodynamics result in rapid morphological changes, with shoreline erosion peaking locally at 5 m/year. In autumn 2022, an intensive two-week field campaign was conducted along three cross-shore transects distributed across the North-Médoc coast to, for the first time, document and analyze the hydrodynamics in this area. The campaign involved collecting measurements of waves and currents across both the inner shelf and nearshore regions, using six current profilers and 13 pressure sensors. Tides were found to predominantly modulate wave transformation and flow in both the nearshore and inner shelf regions of the North-Médoc coast. Strong alongshore currents were measured across the entire study site, increasing southward, which is linked to the overall morphology of a tidal channel. Tidal currents are flood-dominated in the northern part and ebb-dominated in the southern and central parts of the study area. Total currents and wave heights are modulated by tidal elevation, with, for example, increased wave height at the coast during higher tide levels. Nearshore waves, which undergo complex transformation across the inner shelf, such as wave refraction over shoals and rocky outcrops, also drive longshore currents in the surf zone, superimposed on the tidal current. These conditions result in a strong, net, northeastward longshore current, even during low-energy wave conditions. These observations provide new insights into the hydrodynamics of this rapidly evolving coastline and establish a comprehensive dataset that will be crucial for the development and validation of process-based and reduced-complexity models in this region.

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Publication Details

Journal
Estuarine Coastal and Shelf Science
Published
2025-02-26
DOI
https://doi.org/10.1016/j.ecss.2025.109205
Citations
3
Primary Topic
Coastal and Marine Dynamics
Type
article
Field-Weighted Citation Impact
5.01

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article

Field measurements of wave and flow dynamics along a high-energy meso-macrotidal coast adjacent to a large estuary mouth

Bruno Castelle, Kévin Martins, Alexandre Nicolae Lerma, Marine Vandenhove et al.
3 citations
Estuarine Coastal and Shelf Science
Coastal and Marine Dynamics
5.01
article

Field measurements of wave and flow dynamics along a high-energy meso-macrotidal coast adjacent to a large estuary mouth

Bruno Castelle, Kévin Martins, Alexandre Nicolae Lerma, Marine Vandenhove, Vincent Marieu, Vincent Mazeiraud
article en
3 citations

Abstract

The North-Médoc coast, located to the south of the Gironde estuary, exhibits complex hydrodynamic conditions driven by high-energy incident waves and large tides, which are influenced by large-scale rocky outcrops, shoals, and tidal channels on the inner shelf. These wave- and tide-driven hydrodynamics result in rapid morphological changes, with shoreline erosion peaking locally at 5 m/year. In autumn 2022, an intensive two-week field campaign was conducted along three cross-shore transects distributed across the North-Médoc coast to, for the first time, document and analyze the hydrodynamics in this area. The campaign involved collecting measurements of waves and currents across both the inner shelf and nearshore regions, using six current profilers and 13 pressure sensors. Tides were found to predominantly modulate wave transformation and flow in both the nearshore and inner shelf regions of the North-Médoc coast. Strong alongshore currents were measured across the entire study site, increasing southward, which is linked to the overall morphology of a tidal channel. Tidal currents are flood-dominated in the northern part and ebb-dominated in the southern and central parts of the study area. Total currents and wave heights are modulated by tidal elevation, with, for example, increased wave height at the coast during higher tide levels. Nearshore waves, which undergo complex transformation across the inner shelf, such as wave refraction over shoals and rocky outcrops, also drive longshore currents in the surf zone, superimposed on the tidal current. These conditions result in a strong, net, northeastward longshore current, even during low-energy wave conditions. These observations provide new insights into the hydrodynamics of this rapidly evolving coastline and establish a comprehensive dataset that will be crucial for the development and validation of process-based and reduced-complexity models in this region.

Estuarine Coastal and Shelf ScienceVol. 317
Centre National de la Recherche Scientifique (FR), Université de Bordeaux (FR), LIttoral ENvironnement et Sociétés (FR), Environnements et Paléoenvironnements Océaniques et Continentaux (FR), Laboratoire du Futur (FR), Bureau de Recherches Géologiques et Minières (FR), Institut Polytechnique de Bordeaux (FR), La Rochelle Université (FR), Lantiq (Germany) (DE)
Agence Nationale de la Recherche, Centre National de la Recherche Scientifique, Université de Bordeaux, Bureau de Recherches Géologiques et Minières
Openalex Percentile: Top 6%
Coastal and Marine Dynamics
5.01
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