The Joukowski map is a holomorphic function for , withA holomorphic function is a local conformal map wherever its derivative is nonzero. Hence the two finite nonzero critical points areThey lie on the boundary of the fluid region. At the displayed formula has a pole and is undefined as a map to the finite complex plane; zero is outside the fluid region. Thus is locally conformal everywhere in the fluid.
For ,Both factors are positive in the fluid region, so its image is contained in the upper half-plane. The boundary correspondence is also explicit: on the upper unit semicircle, gives , while the real rays and map onto the rays and .
To prove the image is the whole upper half-plane, fix any . The equation isIts roots have product one. Neither root can have unit modulus, since that would make real. Exactly one root therefore has modulus greater than one. For that root the formula for forces , so it belongs to the fluid region. Moreover, if , thenTwo distinct roots in the fluid region would require , impossible when both moduli exceed one. Thus the Joukowski map of the upper exterior of a unit disk is a bijection from the fluid region onto the upper half-plane.
The quadratic formula gives two algebraic possibilities. To select one consistent holomorphic square root, setwhere each factor is the principal square root. Both arguments lie in the upper half-plane, so neither crosses its branch cut. This choice satisfies and at large in the upper half-plane. The required inverse function isFor , , this gives , whose modulus exceeds one. As varies continuously in the upper half-plane, this root cannot cross , since that would make real. Hence the selected root always lies in the fluid region. The other root is its reciprocal and lies inside the unit disk. Simply writing the principal square root of would not specify this branch correctly throughout the upper half-plane.
The line vortex is mapped toIts imaginary part is positive because lies in the fluid region. A conformal map preserves the circulation of the local line vortex, so its strength in the mapped complex plane is still .
Take positive to mean counterclockwise circulation. A line vortex at has complex potential of a two-dimensional potential flow . The method of images imposes the no-penetration boundary condition on the real axis by placing an image line vortex of strength at . ThusFor real , the numerator and denominator have equal modulus, so the streamfunction isThe real axis is therefore a streamline. The image line vortex lies outside the mapped fluid region, while the complex velocitydecays as . This selects the flow due to the line vortex and the boundary, without superposing an imposed background velocity field.
The physical complex potential of a two-dimensional potential flow is . Applying the chain rule gives the complex velocityThe physical velocity is . A useful equivalent expression follows fromFactoring the image expression in the same way makes the terms cancel, leavingThis represents the physical line vortex at , an image line vortex of the same strength at , and image point vortices of opposite strength at and . All three image locations are outside the fluid region. Both boundary pieces inherit the constant streamfunction of the real axis in the mapped complex plane.
A free point vortex is advected by the regular part of the velocity field at its position. Its own singular complex velocity must first be subtracted. The image expression therefore givesEquivalently, is the complex conjugate of the boxed expression. This is the instantaneous velocity, evaluated with the current value of .
To see why mapping the image velocity alone would miss a term, expand the mapped physical singularity:Thus the same point-vortex drift under a conformal map can be writtenThe finite term involving is part of the physical regular velocity field.
If with , direct substitution into the image expression givesThe bracket is strictly positive, and the result is real. Hence a positive line vortex initially moves horizontally to the right, a negative line vortex moves to the left, and the initial vertical velocity is zero. As , the leading term is the familiar drift of a point vortex above a straight wall.
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