The wall speed setsUsing as the local streamwise length giveswhich is large when . The boundary-layer scalingthen givesso the stretching-sheet layer has constant thickness to leading order.
With zero imposed pressure gradient, the two-dimensional boundary-layer equations areIntroduce the stream function byThe boundary conditions areThe additive constant in may be chosen so that .
PutThenSubstitution in the boundary-layer momentum equation, using , givesThe wall and far-field conditions becomeThese are the similarity equations for the boundary layer over a linearly stretching sheet.
Set with . The differential equation reduces toso . The two wall conditions giveHence , and positivity of yieldsor
As ,Thus the tangential velocity matches the quiescent outer fluid, but the normal velocity tends toThe stretching sheet entrains fluid toward itself at a constant leading-order speed. Consequently a globally stationary exterior flow is impossible: the outer flow must provide this normal influx and complete the mass balance away from the local boundary-layer approximation.
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