Take without loss of generality, so , and require decay as . The base velocity is everywhere; there is no jump in its derivative. Let and . A decaying representation that already solves the layer equations is
It is continuous at both interfaces. At the value is and the derivative jump is ; at they are and . The density anomaly drops by one across each interface. The jump conditions for stratified inviscid shear flow therefore reduce to
For nonreal the displacement denominators do not vanish. Neutral limiting values are obtained by continuation, rather than by dividing by zero at an interface.
Set . A nonzero mode requires the determinant to vanish:
Expansion gives the dispersion relation for two density interfaces in uniform shear,
Uniform shear throughout the exterior is important: replacing it with constant exterior velocities would introduce vorticity jumps and give a different dispersion relation.

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