Consider a nonreal phase velocity , so never vanishes. Substitute into the Rayleigh equation for inviscid shear flow. Differentiating cancels the two terms involving , leaving
For , the wall condition on normal velocity gives , hence , at both walls. Multiply by and use integration by parts to obtain the weighted identity for Howard's semicircle theorem:
For a nonzero normal mode, . The imaginary and real parts of this identity give, respectively,
Since , these imply
The first equation says that is a positive weighted mean of , and consequently . The division by is essential: the weighted-mean assertion concerns nonreal modes. A neutral mode may have a critical level where and the substitution for is singular.
Pointwise, . Integrating against the nonnegative weight and substituting both identities yields
Completing the square proves Howard's semicircle theorem:
Thus all nonreal phase velocities lie in the closed disk with the real interval as diameter. For the convention and , exponentially growing normal modes occupy its upper semicircle, while decaying modes occupy its lower semicircle.
Away from the velocity-profile corners, and an unstable normal mode satisfies . On the upper half of the jet write
The exterior solution is selected by decay at infinity. From the given velocity components, the perturbation pressure is
Continuity of normal velocity and pressure therefore gives continuity of and pressure matching at a piecewise-linear shear interface:
At the slope of jumps from to zero. Using yields
The lower interface then follows by parity.
For the even sinuous mode of a planar jet, the derivative can jump at the center: being an even function does not require the one-sided derivative to vanish. The slope jump at is , whereas . Thus
Substitute into the upper-interface relation. With , division by and multiplication by give
Collecting powers of the phase velocity gives the required dispersion relation:
These equations can also be treated as a homogeneous two-by-two system in , avoiding division by any potentially zero amplitude or phase-velocity factor.
For the odd varicose mode of a planar jet, , so ; the central pressure matching at a piecewise-linear shear interface is automatic. The upper-interface equation becomes , and therefore
This phase velocity is real for every , so the discrete varicose mode of a planar jet is neutral and there is no exponentially unstable odd mode.
To determine the unstable even modes, factor the reduced discriminant of the quadratic:
The second factor vanishes at zero and has derivative for , so it is positive there. The first factor starts at , is strictly increasing, and tends to infinity. It therefore has one positive zero . The even phase velocities are
It follows that
For , one member of the complex conjugate pair grows at rate and the other decays. At the speeds merge and there is no exponential growth; for both speeds are real. This is inviscid instability of a triangular jet. The unstable sinuous mode of a planar jet also satisfies Howard's semicircle theorem with and : its speed lies in the upper half-disk centered at with radius .
Figure 1.
Triangular jet profile and unstable sinuous phase velocities inside the Howard semicircle
. Details.
First suppose and put . The wall condition gives . Substitution into the Rayleigh equation for inviscid shear flow gives
Multiply by and use integration by parts. The resulting weighted identity for Howard's semicircle theorem is
Its imaginary part gives , and its real part then gives . Set and . Since ,
Completing the square proves Howard's semicircle theorem:
In particular every growing normal mode lies in the upper semicircle for . If is real and outside , is again regular, but the same identity has a strictly positive integrand unless the mode vanishes. Such a neutral mode is impossible. Consequently neutral regular modes also satisfy the bound; no division by is needed for this last conclusion. The nonreal proof avoids critical-level singularities altogether.
Put . The Rayleigh equation for inviscid shear flow becomes
Multiplication by and integration gives
For , its real and imaginary parts imply
Thus is a weighted mean of and is its weighted variance. If , the sharp bounded-variable variance estimate gives
Completing the square proves Howard's semicircle theorem:
For a nonreal regular Rayleigh equation for inviscid shear flow mode vanishing at the walls, put . The equation becomes . Multiplication by and integration by parts gives the displayed identity. With , its imaginary and real parts give and . Since , these imply Howard's semicircle theorem.