Wave dispersion

Wave dispersion means that phase velocity depends on wavenumber or, equivalently, wavelength. Wave packets generally travel with group velocity, which need not equal phase velocity. The linear rotating shallow-water dispersion relation ${\omega }^2=f^2+c^2{k}^2$ has faster long-wave phase motion but slower long-wave packet motion when $f\ne 0$.

The change of an optical propagation angle with wavelength. A diffraction grating at normal incidence has $d\sin \theta =m\lambda$, so differentiating gives $d\theta /d\lambda =m/(d\cos \theta )$. This converts a small spectral-line separation into angular separation, but resolving the two images also requires sufficient aperture and a narrow source image.

Intermodal dispersion is the temporal separation of components in different propagating normal modes because their group velocities differ. A pulse exciting several modes can therefore broaden even when its individual modal components have negligible bandwidth. It is distinct from group velocity dispersion within a single mode.

A nondispersive wave has constant phase velocity on a propagation branch. For $\omega =ck$, its group velocity is also $c$. A frequency relation with a nonzero offset, such as $\omega =ck+b$, has constant group velocity but a phase velocity $c+b/k$ depending on wavenumber; constant group velocity alone is therefore not sufficient for nondispersion.