Earlier investigations of internal solitary waves in stable, stratified shear flows are generalized on the hypothesis that cubic and quadratic nonlinearity may be of comparable significance—or, equivalent, that ? = O(? 2 ), where ?? a / h < 1 and ? = ( h / l ) < 1 for a wave of amplitude a (which may be positive or negative) and length l in a fluid of depth h . An infinite, discrete set of internal solitary waves is possible for prescribed density and horizontal velocity in the primary flow, and to each of these modes there corresponds a relation ? = ?(?), 0 < |?| < |? n |. Cubic nonlinearity is significant vis-a-vis quadratic nonlinearity if and only if ? n = O (?), and h |? n | then appears as a maximum achievable amplitude. The limit ?n ? 0 (which corresponds to a critical combination of the basic flow parameters) implies a ? 0 and l ? ? if the mass carried by the wave is fixed. DOI: 10.1111/j.2153-3490.1979.tb00924.x
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John W. Miles (1979) studied this question.
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