Experimental evidence of stable wave patterns on deep water

被引:18
|
作者
Henderson, Diane M. [1 ]
Segur, Harvey [2 ]
Carter, John D. [3 ]
机构
[1] Penn State Univ, Dept Math, University Pk, PA 16803 USA
[2] Univ Colorado, Dept Appl Math, Boulder, CO 80309 USA
[3] Seattle Univ, Dept Math, Seattle, WA 98122 USA
基金
美国国家科学基金会;
关键词
stability; surface gravity waves; SHORT-CRESTED WAVES; MODULATIONAL INSTABILITY; PERMANENT FORM; SURFACE-WAVES; GRAVITY-WAVES; EVOLUTION; TRAINS; STABILITY; BREAKING; EQUATION;
D O I
10.1017/S0022112010001643
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
Recent predictions from competing theoretical models have disagreed about the stability/instability of bi-periodic patterns of surface waves on deep water. We present laboratory experiments to address this controversy. Growth rates of modulational perturbations are compared to predictions from: (i) inviscid coupled nonlinear Schrodinger (NLS) equations, according to which the patterns are unstable and (ii) dissipative coupled NLS equations, according to which they are linearly stable. For bi-periodic wave patterns of small amplitude and nearly permanent form, we find that the dissipative model predicts the experimental observations more accurately. Hence, our experiments support the claim that these bi-periodic wave patterns are linearly stable in the presence of damping. For bi-periodic wave patterns of large enough amplitude or subject to large enough perturbations, both models fail to predict accurately the observed behaviour, which includes frequency downshifting.
引用
收藏
页码:247 / 278
页数:32
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