Wave dispersion means that different frequencies propagate with different phase velocities, so a wave packet generally changes shape. Equivalently the dispersion relation is not proportional to over the relevant band. Three natural examples are the colour separation in a rainbow, where the refractive index of water depends on wavelength; deep-water surface gravity waves, for which and long waves have larger phase velocity; and capillary waves, whose short-wave limit is and whose shorter waves have larger phase velocity. Here is gravitational acceleration, is surface tension, and is fluid mass density, with positive and negligible viscosity.
A distinct application is an optical prism spectrometer: the wavelength-dependent refractive index produces different refraction angles, separating spectral components for measurement. This exploits wave dispersion deliberately.

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