A Gaussian Packet on Water: Three Fates of One Wave ✛

Original: "Nonlinear Reshaping of Gaussian Water Wave Packets"
arXiv:2609.03259v1 · 2026-09-03 · CC BY 4.0 · 2 min
A wave packet with a Gaussian envelope can spread, hold its shape, or focus, depending on the balance between dispersion and nonlinearity.

A wave packet is like a traveler who either loses steam and spreads out along the way, holds a steady pace, or gathers into a fist. In a 50-meter flume with water 5 meters deep, scientists tracked how a bell-shaped group of waves behaves when its height is changed but not its width. A Gaussian packet is a wave with a smooth rise and fall, like a hill on the water. Its fate depends on how strongly the wave pushes itself along.

In the calm regime, when the amplitude is small, the packet spreads. Waves of different lengths travel at different speeds, and the group loses its shape, like a crowd on a long-distance run. The amplitude drops by half, and the width increases fourfold. But if you tune the height to match the parameters of a stable solitary wave, the packet travels unchanged, as if it were a soliton.

At amplitude parameters N=0.8 and 1.0, the packet held its shape over a distance of 1.07 dispersion lengths. That is like a traveler walking at a steady pace without tiring.

When the amplitude is increased further, the wave begins to focus: its crest grows and its base narrows. The peak moves faster than the group, like a runner breaking ahead. For N=1.2 and 1.4, the standard equation describes this process, but for N=1.6 and 1.8, additional corrections are needed because the wave becomes too steep and no longer resembles a smooth hill.

At N=1.8, the amplitude had grown by 80% by the last sensor. That is like a traveler suddenly speeding up and coiling into a spring.

Earlier it was clear that a Gaussian packet is not an exact solution for a stable wave, but no one had mapped its behavior in such detail. Now it is evident: if the amplitude and width are matched to the soliton parameters, the packet can travel almost unchanged. This knowledge will help control extreme waves in the ocean and tune pulses in optical fibers. The traveler, it turns out, can not only tire but also hold its shape, and sometimes gather into a fist.

The 5-meter-deep wave flume ensures deep-water conditions for waves with wavenumber k=2.4 m⁻¹, since kh≥12. Wave amplitudes in the experiments ranged from 1.2 cm to 10 cm, comparable to the height of a matchbox.

\partial_x A + \frac{i\beta_2}{2}\partial_{tt} A + i\gamma |A|^2 A = 0
This equation describes the evolution of the complex envelope A in a frame moving with the group velocity, where β₂ is dispersion and γ is nonlinearity.
\partial_x A + \frac{i}{g}\partial_{tt} A + ik^3 |A|^2 A - \frac{k^3}{\omega}\left(6|A|^2\partial_t A + 2A\partial_t |A|^2 - 2iA H[\partial_t |A|^2]\right) = 0
This equation includes terms up to fourth order in wave steepness, accounting for self-steepening, nonlinear gradient corrections, and wave-induced mean flow (via the Hilbert transform H).
Concepts
wave packet wave propagation Vlasov equation magnetic soliton Gross–Pitaevskii equation dispersion relation gravitational waves Gaussian distribution anisotropic light propagation non gaussianity patterned fluid dynamics Boltzmann equation Schrödinger equation Snell's law of refraction wave equation density waves dispersion reflection