Marine Vandenhove , Bruno Castelle , Alexandre Nicolae Lerma , Vincent Marieu , Kévin Martins , Vincent Mazeiraud
{"title":"靠近大河口的高能中巨潮海岸波浪和流动动力学的野外测量","authors":"Marine Vandenhove , Bruno Castelle , Alexandre Nicolae Lerma , Vincent Marieu , Kévin Martins , Vincent Mazeiraud","doi":"10.1016/j.ecss.2025.109205","DOIUrl":null,"url":null,"abstract":"<div><div>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.</div></div>","PeriodicalId":50497,"journal":{"name":"Estuarine Coastal and Shelf Science","volume":"317 ","pages":"Article 109205"},"PeriodicalIF":2.6000,"publicationDate":"2025-02-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Field measurements of wave and flow dynamics along a high-energy meso-macrotidal coast adjacent to a large estuary mouth\",\"authors\":\"Marine Vandenhove , Bruno Castelle , Alexandre Nicolae Lerma , Vincent Marieu , Kévin Martins , Vincent Mazeiraud\",\"doi\":\"10.1016/j.ecss.2025.109205\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>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. 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引用次数: 0
摘要
位于吉伦特河口以南的北-姆萨姆多克海岸,受内大陆架上大规模的岩石露出地面、浅滩和潮汐通道的影响,表现出由高能入射波和大潮汐驱动的复杂水动力条件。这些波浪和潮汐驱动的水动力导致了快速的形态变化,海岸线侵蚀在局部达到5米/年的峰值。在2022年秋季,沿着分布在北-姆萨姆多克海岸的三个跨海岸横断面进行了为期两周的密集实地调查,首次记录和分析了该地区的水动力学。这次活动包括使用6个电流分析器和13个压力传感器,收集内部大陆架和近岸地区的波浪和电流测量数据。发现潮汐在北- m - m - 3海岸的近岸和内陆架区域主要调节波浪变换和流动。整个研究地点都测量到了强劲的沿岸水流,并向南增加,这与潮汐通道的整体形态有关。研究区北部以洪水为主,南部和中部以退潮为主。总海流和波浪高度受潮汐高度的调节,例如,在较高的潮汐高度时,海岸的波浪高度会增加。近岸波在大陆架内部经历了复杂的转变,比如浅滩和露出地面的岩石上的波浪折射,也推动了冲浪区的沿岸流,叠加在潮流上。即使在低能波条件下,这些条件也会导致强劲的、净的、东北方向的海岸流。这些观测结果为这一快速演变的海岸线的流体动力学提供了新的见解,并建立了一个全面的数据集,这对该地区基于过程和降低复杂性的模型的开发和验证至关重要。
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.
期刊介绍:
Estuarine, Coastal and Shelf Science is an international multidisciplinary journal devoted to the analysis of saline water phenomena ranging from the outer edge of the continental shelf to the upper limits of the tidal zone. The journal provides a unique forum, unifying the multidisciplinary approaches to the study of the oceanography of estuaries, coastal zones, and continental shelf seas. It features original research papers, review papers and short communications treating such disciplines as zoology, botany, geology, sedimentology, physical oceanography.