Harbor resonance induced by subaerial landslide-generated impact waves

被引:60
作者
Dong, Guohai [1 ]
Wang, Gang [1 ]
Ma, Xiaozhou [1 ]
Ma, Yuxiang [1 ]
机构
[1] Dalian Univ Technol, State Key Lab Coastal & Offshore Engn, Dalian 116023, Peoples R China
关键词
Harbor resonance; Impact waves; Solitary waves; Seiche; Wavelet spectra; NONLINEAR BOUSSINESQ MODEL; TSUNAMI;
D O I
10.1016/j.oceaneng.2010.03.005
中图分类号
U6 [水路运输]; P75 [海洋工程];
学科分类号
0814 ; 081505 ; 0824 ; 082401 ;
摘要
Past studies of harbor resonance have mainly been restricted to the quasi-steady oscillations induced by steady wave conditions. This paper investigates the response of a rectangular harbor to subaerial landslide-generated impact waves based on physical models, in order to compare the oscillations induced by steady and transient waves. In response to steady incident waves, oscillations within the harbor need to experience a long process to obtain their maximum value before the input energy and the losses are balanced. Landslide-generated impact waves usually include components with solitary wave characteristics and also components with dispersive wave characteristics. Each component travels with a different celerity. Usually, solitary wave components propagate faster, and arrive in the harbor first. Oscillations attain their maximum status as soon as these components arrive. The subsequently arriving components with dispersive characteristics do not enhance the resonance oscillations. So the waves with solitary characteristics are considered to play an important role in harbor resonance. Numerical experiments, using the FUNWAVE model, were conducted in order to further verify these conclusions. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:927 / 934
页数:8
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