Effects of Triad Interactions on Wave Attenuation by Vegetation

被引:5
作者
Zhu, Ling [1 ]
Chen, Qin [1 ]
机构
[1] Louisiana State Univ, Dept Civil & Environm Engn, Baton Rouge, LA 70803 USA
基金
美国国家科学基金会;
关键词
Wave attenuation; Vegetation; Energy transfers; Triad interactions; Evolution equations; Energy dissipation models; SALT-MARSH VEGETATION; SHALLOW-WATER; ENERGY-DISSIPATION; BREAKING WAVES; GRAVITY-WAVES; NONLINEAR TRANSFORMATION; SPECTRAL DISTRIBUTION; BOUSSINESQ EQUATIONS; EVOLUTION-EQUATIONS; SURF ZONE;
D O I
10.1061/(ASCE)EM.1943-7889.0001328
中图分类号
TH [机械、仪表工业];
学科分类号
0802 ;
摘要
Wave attenuation in vegetated shallow water is mainly attributed to actual drag-induced dissipation and near-resonant triad interactions. The latter is neglected in existing theoretical models for vegetation-induced dissipation. In this study, a set of evolution equations describing the spatial evolution of three near-resonant wave components was extended to include vegetation effects. The contributions of triad interactions to the attenuation of individual harmonics were investigated. The authors found that neglecting the energy cycling caused by triad interactions gives an underestimation of damping rates. The triad interactions have greater effects on the attenuation of higher harmonics. A fully nonlinear, fully dispersive wave model was used to explore the effects of triad interactions on spectral dissipation of random waves. After isolating the energy transfers caused by triad interactions and the actual drag-induced dissipation, the authors found that triad interactions transfer energy to higher harmonics, which experience greater damping. Due to the energy transfers from spectral peak (f(p)) to high frequencies (2f(p)), the energy losses in f(p) and 2f(p) are overestimated and underestimated, respectively, by existing models based on linear wave theory. (C) 2017 American Society of Civil Engineers.
引用
收藏
页数:13
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