A High-Order Asymptotic Analysis of the Benjamin-Feir Instability Spectrum in Arbitrary Depth
Ryan Creedon, Bernard Deconinck

TL;DR
This paper provides a high-order asymptotic analysis of the Benjamin-Feir instability spectrum for Stokes waves in water of arbitrary depth, offering precise estimates and revealing different instability regimes.
Contribution
It introduces a perturbation method for high-order spectral analysis of the Benjamin-Feir instability, aligning well with numerical and rigorous results, and compares it with high-frequency instability spectra.
Findings
High-order asymptotic expansions match numerical results.
Derived estimates for growth rates of the instability.
Identified three regimes of Stokes wave instabilities.
Abstract
We investigate the Benjamin-Feir (or modulational) instability of Stokes waves, i.e., small-amplitude, one-dimensional periodic gravity waves of permanent form and constant velocity, in water of finite and infinite depth. We develop a perturbation method to describe to high-order accuracy the unstable spectral elements associated with this instability, obtained by linearizing Euler's equations about the small-amplitude Stokes waves. These unstable elements form a figure-eight curve centered at the origin of the complex spectral plane, which is parameterized by a Floquet exponent. Our asymptotic expansions of this figure-eight are in excellent agreement with numerical computations as well as recent rigorous results by Berti, Maspero, and Ventura. From our expansions, we derive high-order estimates for the growth rates of the Benjamin-Feir instability and for the parameterization of the…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsOcean Waves and Remote Sensing · Coastal and Marine Dynamics · Oceanographic and Atmospheric Processes
