Write , , and denote the slow density and velocity field amplitudes by and . Acting on the rapid phase, gives , where . Spatial differentiation gives , while derivatives of the amplitudes and the mean shear flow are . The leading continuity equation and linearized Euler equations therefore become
Eliminating on the nonzero acoustic branch gives the acoustic eikonal equation in a shear flow:
The mean-shear term is small here because ; retaining advection does not require retaining that gradient in the leading phase equation. The positive intrinsic-frequency acoustic dispersion relation is , with group velocity .
In a stationary wall boundary layer, horizontal homogeneity preserves and along a Hamiltonian ray-tracing equations trajectory. For a two-dimensional ray,
Suppose increases from zero at the wall to a positive free-stream value. For a downstream-directed wave normal, , increasing decreases and . The wave normal bends towards the wall, and the ray becomes more nearly parallel to it. If reaches , then : the ray turns and returns towards the wall rather than reaching the free stream. With launch angle above the wall and free-stream Mach number , the escape condition is
For upstream-directed wave normals, , and increase through the layer; there is no such downstream turning barrier on this branch. A wavefront normal is parallel to , while the energy ray follows the group velocity: advection makes their directions different. In particular, a wall-normal wave normal with can still have a ray drifting downstream. The ordinary WKB method needs a local turning-point continuation at ; the ray sketch depicts that qualitative continuation.
Figure 1.
Acoustic energy rays through a wall shear layer, showing downstream escape, downstream turning and downstream drift of a wall-normal wave normal
. Details.