This paper considers the dispersion of a 2-D non-buoyant jet discharge
d beneath a series of progressive gravity waves. A new experimental in
vestigation is described in which the dispersion of a jet in a wave en
vironment is compared to an identical discharge in a stagnant ambient.
This comparison highlights the additional wave-induced mixing and sho
ws that the oscillatory wave motion has a significant effect upon both
the mean velocity profiles and the magnitude of the turbulent fluctua
tions. In particular, the experimental data suggests that the wave mot
ion encourages a transfer of energy into the turbulent components of t
he flow field. This effect is most pronounced within the ''zone of flo
w establishment'', and leads to a significant increase in the effectiv
e Reynolds stresses. This in turn creates a region of intense fluid mi
xing which is characterised by a large reduction in the axial velocity
components and a substantial increase in the rate of entrainment. The
experimental data is also compared to both the existing integral solu
tions and a Lagrangian formulation which is similar to that proposed b
y Chin (1988). Although neither of these solutions is able to model th
e flow immediately downstream of the outlet, the Lagrangian solution p
rovides an improved description of the mean velocity within the ''zone
of established flow''.