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This article is about scattering of waves on a water surface. For different types of scattering, see Scattering (disambiguation).

In liquid progress, scattering of water waves by and large alludes to recurrence scattering, which implies that floods of various wavelengths go at various stage speeds. Water waves, in this connection, are waves engendering on the water surface, and constrained by gravity and surface strain. Thus, water with a free surface is by and large thought to be a dispersive medium.

Surface gravity waves, moving under the compelling by gravity, engender quicker to increase wavelength. For a given wavelength, gravity waves in more profound water have a bigger stage speed than in shallower water. Interestingly with this, hairlike waves just constrained by surface strain, proliferate quicker for shorter wavelengths.

Other than recurrence scattering, water waves additionally show adequacy scattering. This is a nonlinear impact, by which influxes of bigger abundancy have an alternate stage speed from little plentifulness waves. On the off chance that the wave speed depends just on the physical properties of the medium (i.e., the flexible and dormancy properties of a mechanical medium, or the relative penetrability and permittivity for EM waves) then the wave pace is a steady, free of recurrence. Such a medium is known as a non-dispersive medium and waves going through this medium will keep up a steady shape. This is delineated by the dark wave beat in the movement at left. The beat is a Gaussian capacity, containing various frequencies. Subsequent to the wave velocity is consistent, all frequencies go at the same pace and the beat keeps up steady shape.

Be that as it may, there are numerous samples of dispersive media where, for different reasons, the wave speed relies on upon the recurrence of the wave. The blue wave beat in the liveliness is the same Gaussian capacity as the dark heartbeat, comprising of countless segments included. Be that as it may, now the wave speed relies on upon recurrence, with higher frequencies voyaging speedier than lower frequencies. Accordingly, the wave beat spreads out and changes shape as it ventures.

The “middles” of both wave beats go at the same velocity. This prompts the idea of a “gathering speed” which is the pace with which the vitality conveyed by the wave ventures. The gathering speed is the same for every wave beat.