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Towards validating a last generation, integrated wave-current-sediment numerical model in coastal regions using video measurements

机译:试图通过视频测量验证沿海地区的上一代综合波流沉积数值模型

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This paper presents the first steps in the implementation of a morphological numerical model to be applied in the Bevano River region, a shallow water area in the Adriatic Sea, with the aim of helping the identification and assessment of erosional patterns and bottom morphological modifications induced by severe marine storms. The numerical modeling, performed using a fully 3D coupled wave-current-sediment version of the ROMS model, has been complemented with in situ data analysis and observations: a first qualitative validation of the results was given by the analysis of images acquired via an ARGUS video station. Hydrodynamic modeling highlighted how shear bottom stresses and bottom currents fields were heavily influenced by severe storm situations, and had large effects on the morphology of shallow regions. The correlation between the wave-current induced bottom stresses and the resulting topography was investigated. Nearshore hydrodynamics modeling results demonstrated the dominant role played by alongshore sediment transport, with the magnitude of both cross- and along-shore wave-induced currents strongly depending on wave height and direction. We found a good qualitative conformity between the results of the numerical models applied during a "Bora" storm and the corresponding video observations; both techniques indicated the migration of the existing sandbar within the range of about 40 m seaward. Results show how integrated numerical open source tools, often used in oceanography, are becoming suitable for both preliminary investigations and for planning the effective littoral management, and how their calibration can be supported by the use of new low cost techniques, such as video measurements.
机译:本文介绍了实施在亚得里亚海浅水区贝瓦诺河地区应用的形态学数值模型的第一步,目的是帮助识别和评估由侵蚀引起的侵蚀模式和底部形态变化。严重的海洋风暴。使用ROMS模型的完全3D耦合波流沉积版本进行的数值建模已得到原位数据分析和观察的补充:通过对通过ARGUS采集的图像进行分析,对结果进行了首次定性验证视频站。流体力学模型强调了剪切底部应力和底部流场如何受到严重暴风雪的严重影响,并对浅层区域的形态产生了很大影响。研究了波浪电流引起的底部应力与所产生的形貌之间的相关性。近岸水动力模拟结果表明,沿岸沉积物运输起主要作用,跨岸和沿岸波浪感应电流的大小强烈取决于波浪的高度和方向。我们发现在“波拉”风暴期间应用的数值模型结果与相应的视频观测结果之间具有很好的定性一致性;两种技术均表明现有沙洲在向海约40 m的范围内迁移。结果表明,通常在海洋学中使用的集成数字开源工具如何适合于初步调查和规划有效的沿海管理,以及如何通过使用新型低成本技术(例如视频测量)来支持其校准。

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