The factor is the signed curvature of the graph, so the pressure jump is surface tension times curvature, the planar Young–Laplace equation.
Take total velocity potentials and . Each disturbance potential satisfies the Laplace equation. The interface moves with the fluid: for , the material equation gives . Keeping only first-order terms and evaluating at yields
The unsteady Bernoulli equation is , with any common gravitational contribution canceling across this equal-density interface. Subtracting the basic flow and linearizing gives and . The linearized pressure jump is . Hence
Use complex modes with real parts understood:
The decaying vertical factors solve the Laplace equation in their respective half-planes. The kinematic conditions give and . Substitution in the dynamic condition gives
When the discriminant is nonnegative, the phase speeds are . They are two dispersive capillary-wave branches advected by the mean velocity .
When , the frequencies are complex conjugates and one mode grows exponentially, with growth rate . This is Kelvin-Helmholtz instability. Surface tension stabilizes sufficiently short waves, while for any nonzero shear, sufficiently long waves are unstable in this gravity-free equal-density model. A real cosine with real frequency describes the stable branches; the unstable case is represented by the real part of the corresponding growing complex mode.

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