Antidune 2026-10-31
An antidune is a bedform associated with supercritical free-surface flow, in which bed and surface undulations are approximately in phase. In the elementary erodible-bed model with suspended sediment, an unstable branch can migrate upstream. Its growth and migration depend on the hydraulic and sediment-response parameters; the high-wavenumber antidune dispersion calculation makes the required supercritical regime explicit.
Write , and introduce perturbations to water depth, velocity, concentration and bed height. Take the leading quasi-steady approximation for the fast water and suspension response, retaining the small friction parameter . For , the linearized equations are
Here surface height is , and linearization of gives . Eliminating gives the dispersion relation
In particular, putting and expanding at large ,
Thus the temporal growth rate tends to a finite constant, while the phase velocity is
For supercritical flow , the waves propagate upstream. They grow if ; at leading order in small , this holds for fixed positive away from critical flow. They are antidunes, upstream-migrating bedforms coupled to the free surface. Indeed and , so surface height is in phase with the bed perturbation in this regime.
For clarity, neglecting completely gives the exact leading-order expressions
These also identify the missing qualification in the source: the unstable upstream branch requires . For this leading model gives decay and downstream propagation. The near-critical case needs a different balance; it is not covered by the expansion. Small nonzero perturbs the slow bedform branch and adds fast water modes, so the stated result concerns the leading slow morphodynamic branch. This is the high-wavenumber antidune dispersion calculation.