Let be a representative mixing-layer thickness, , and let be a representative streamwise velocity. Use the scales
The transverse velocity scale follows from the mean continuity equation. For turbulent transverse transport to balance streamwise inertia,
With this ordering, the streamwise eddy-stress divergence is
Thus transverse diffusion of streamwise linear momentum is retained, while streamwise diffusion and the contribution are smaller by . Molecular kinematic viscosity is neglected where .
In the transverse momentum equation, inertia and the retained eddy stresses have scale , whereas an order-one transverse pressure variation would give . Hence the leading dimensionless transverse balance is . The resulting boundary layer equations for the planar turbulent mixing layer are
Here . The effective pressure convention explained in part (a)(iii) is understood. Since the outer streams have uniform horizontal velocities, their inviscid momentum equations give ; choosing the far-field gauge pressure as zero gives throughout this approximation.
A planar turbulent mixing layer develops between two parallel streams of different mean velocities. Their shear flow generates turbulence that transports streamwise linear momentum across the interface. A thin-layer eddy viscosity model with has thickness proportional to downstream distance. For , its leading mean velocity transition is an error function.
For a planar turbulent mixing layer, let , , , , and . The stream function enforces mean incompressibility. Substitution into gives the displayed ordinary differential equation, with . When is small, its linear approximation is , so is a Gaussian function and an error function.