Slowly varying solitary waves in deep fluids

Abstract
The slowly varying solitary wave is constructed as an asymptotic solution of the deep fluid equation of Benjamin (1967), Davis & Acrivos (1967), and Ono (1975). A multiple scale method is used to determine the amplitude and phase of the wave to second order in the perturbation parameter. Behind the solitary wave a shelf develops. Outer expansions are intro­duced to remove certain non-uniformities in the expansion. The results are interpreted from conservation laws. Finally the effect of damping, either due to radiating internal waves or due to friction, is considered.

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