Orbital stability of internal waves

TL;DR

This paper proves the orbital stability of small-amplitude internal capillary-gravity waves in a two-fluid system, using Hamiltonian reformulation and spectral analysis, extending stability results to near-critical surface tension regimes.

Contribution

It establishes the orbital stability of small-amplitude internal waves for a two-fluid Euler system, including near-critical surface tension regimes, using a Hamiltonian framework and spectral analysis.

Findings

Small-amplitude solitary waves are orbitally stable under certain conditions.

The trivial solution is conditionally stable in specific parameter regions.

Stability or instability can be inferred from a dispersive PDE model in near-critical regimes.

Abstract

This paper studies the nonlinear stability of capillary-gravity waves propagating along the interface dividing two immiscible fluid layers of finite depth. The motion in both regions is governed by the incompressible and irrotational Euler equations, with the density of each fluid being constant but distinct. A diverse collection of small-amplitude solitary wave solutions for this system have been constructed by several authors in the case of strong surface tension (as measured by the Bond number) and slightly subcritical Froude number. We prove that all of these waves are (conditionally) orbitally stable in the natural energy space. Moreover, the trivial solution is shown to be conditionally stable when the Bond and Froude numbers lie in a certain unbounded parameter region. For the near critical surface tension regime, we prove that one can infer conditional orbital stability or orbital instability of small-amplitude traveling waves solutions to the full Euler system from considerations of a dispersive PDE model equation. These results are obtained by reformulating the problem as an infinite-dimensional Hamiltonian system, then applying a version of the Grillakis--Shatah--Strauss method recently introduced by Varholm, Wahl\'en, and Walsh. A key part of the analysis consists of computing the spectrum of the linearized augmented Hamiltonian at a shear flow or small-amplitude wave. For this, we generalize an idea used by Mielke to treat capillary-gravity water waves beneath vacuum.