在瓜达尔基维尔河河口的形态变化引起的水力动力学效应的数值模拟研究
Sara Sirviente1, Jairo Sánchez-Rodríguez2, Juan Jesús Gomiz-Pascual1
1Department of Applied Physics, Faculty of Marine and Environmental Sciences, Marine Research Institute (INMAR), International Campus of Excellence of the Sea (CEI·MAR), University of Cadiz, Puerto Real, 11510, Cadiz, Spain.
The Science of the total environment
|August 7, 2023
概括
瓜达尔基维尔河口的疏引起的深化放大了潮波,增强了共振. 河口深度和宽度的变化显著影响潮动态和波幅.
科学领域:
- 海洋学 海洋学 海洋学
- 沿海工程 沿海工程
- 环境科学 环境科学
背景情况:
- 河口是动态的环境,受到各种因素的影响.
- 潮动态对于河口生态系统和航行至关重要.
- 人类干预,如疏,可以改变河口形态和水力动力学.
研究的目的:
- 分析底部深度变化对瓜达尔基维尔河口的潮动态的影响.
- 调查疏操作在修改河口潮特征中的作用.
- 了解河口几何变化如何影响潮波共振.
主要方法:
- 开发和应用一个现实的非线性1D数值模型.
- 将河口宽度和底部深度的变化纳入模型.
- 在改变的浴度下模拟潮波传播和放大.
主要成果:
- 观测到的M2潮波的显著放大向上游河口.
- 河口的深化,归因于疏,增强了它对共振的倾向.
- 降低底部摩擦和较小的潮波幅度由于深入而降低.
结论:
- 河口的深化对潮动力学和波浪放大有重大影响.
- 深度和宽度的变化对于潮波的共振反应至关重要.
- 疏操作对瓜达尔基维尔河口的潮行为有深远的影响.
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