A nonlinear Schrodinger equation for gravity waves slowly modulated by linear shear flow

被引:10
|
作者
Li, Shaofeng [1 ]
Chen, Juan [1 ]
Cao, Anzhou [1 ]
Song, Jinbao [1 ]
机构
[1] Zhejiang Univ, Ocean Coll, Zhoushan 316000, Peoples R China
基金
中国国家自然科学基金;
关键词
nonlinear Schrodinger equation; gravity waves; linear shear flow; modulational instability; WATER-WAVES; ROGUE WAVES; SURFACE; DEPTH; INSTABILITY; EVOLUTION; PACKETS;
D O I
10.1088/1674-1056/ab53cf
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
Assume that a fluid is inviscid, incompressible, and irrotational. A nonlinear Schrodinger equation (NLSE) describing the evolution of gravity waves in finite water depth is derived using the multiple-scale analysis method. The gravity waves are influenced by a linear shear flow, which is composed of a uniform flow and a shear flow with constant vorticity. The modulational instability (MI) of the NLSE is analyzed, and the region of the MI for gravity waves (the necessary condition for existence of freak waves) is identified. In this work, the uniform background flows along or against wave propagation are referred to as down-flow and up-flow, respectively. Uniform up-flow enhances the MI, whereas uniform down-flow reduces it. Positive vorticity enhances the MI, while negative vorticity reduces it. Hence, the influence of positive (negative) vorticity on MI can be balanced out by that of uniform down (up) flow. Furthermore, the Peregrine breather solution of the NLSE is applied to freak waves. Uniform up-flow increases the steepness of the free surface elevation, while uniform down-flow decreases it. Positive vorticity increases the steepness of the free surface elevation, whereas negative vorticity decreases it.
引用
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页数:8
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