The conduit equation evolves the positive cross-sectional area of a viscous buoyant conduit. Its scaling uses axial length and velocity , where . Linearization at gives : phase velocity is upward but group velocity changes sign at . Nonlinear elevation waves obey the solitary-wave amplitude-speed relation for the conduit equation.
A positive travelling wave on a uniform background has first integral , with . Equating the crest and background potentials gives the displayed speed relation for crest ratio . The elevation-wave speed exceeds and approaches that long-wave speed as . The formula requires the positive-area branch, rather than continuation through .
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