Rigidity of symmetric doubly-periodic water waves near shear flows
Douglas Svensson Seth, Kristoffer Varholm, Erik Wahlén, Jörg Weber
TL;DR
The paper analyzes symmetric, doubly periodic capillary-gravity waves in finite depth near non-uniform shear flows. By flattening the free boundary, expanding in a small amplitude parameter, and performing a careful linear and quadratic solvability analysis, the authors show that the leading-order bifurcating waves are two-dimensional if the background shear $U(x_3)$ is non-constant and non-stagnant. The linear problem has a finite-dimensional kernel $N(U)$ determined by a dispersion relation, and the quadratic solvability imposes a resonance-type obstruction unless all modal amplitudes vanish, thereby precluding genuinely three-dimensional leading-order bifurcations. This rigidity contrasts with the uniform-flow case and clarifies when higher-dimensional wave structures may (or may not) arise under symmetric, doubly periodic settings. The approach also accommodates variations of the dynamic boundary condition and extends to other boundary phenomena such as hydroelastic waves.
Abstract
We prove that symmetric, doubly periodic, capillary-gravity water waves in finite depth bifurcating from non-uniform non-stagnant shear flows are necessarily two-dimensional to leading order. This is in stark contrast to the case of uniform background flows, where the existence of truly three-dimensional bifurcating waves is well known. While this paper focuses on capillary-gravity water waves, our proof also applies to other suitable types of dynamic boundary conditions, such as hydroelastic waves.
