The differential equation ym+yy" + A(1 — y'2) = 0 is of importance in boundary-layer theory. H. Weyl has shown that the equation has a solution which satisfies certain boundary conditions. The present paper gives a simple proof of Weyl’s result and then investigates in detail the properties of all solutions of the equation.
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W. A. Coppel (1960) studied this question.
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