Let , stretch and write the original transverse velocity as . Continuity then gives . In the streamwise momentum equation is order one, while is negligible. The transverse equation gives to leading order, so pressure is supplied by the outer Euler flow. Its streamwise balance is . Consequently
For a stationary impermeable plate, , with matching as . The transverse velocity must match the outer displacement flow; it is generally wrong to impose independently at infinity.
At the leading edge the wall no-slip data meet the external stream abruptly, and the boundary-layer approximation is nonuniform. For a constant external speed, the thickness is , whose ratio to ceases to be small when the local Reynolds number is order one. A leading-edge region retaining neglected derivatives is needed there. An adverse pressure gradient can also cause separation farther downstream; a large global Reynolds number alone does not prevent it.
Use , , and put , . Then
Matching requires . Equating the powers in streamwise inertia and transverse diffusion gives
The two convective terms combine to , while . Hence the Falkner-Skan equation in this scaling is
The additive stream-function constant is fixed by ; when this also encodes no penetration. For it is a harmless choice of additive constant choice. Existence of an attached physical branch for a given is a separate issue from deriving the similarity reduction.
On an attached branch with away from the wall, use itself as the independent variable. The chain rule gives and . Therefore
If the wall shear , then , so . Thus is singular at zero while is finite. Imposing a finite arbitrary would remove the usual attached branch. This is the velocity as dependent variable in the Falkner-Skan equation reduction.

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