Hostname: page-component-78c5997874-mlc7c Total loading time: 0 Render date: 2024-11-10T06:51:48.266Z Has data issue: false hasContentIssue false

The current-modified nonlinear Schrödinger equation

Published online by Cambridge University Press:  25 November 1999

J. R. STOCKER
Affiliation:
School of Mathematics, University of Bristol, University Walk, Bristol BS8 1TW, UK
D. H. PEREGRINE
Affiliation:
School of Mathematics, University of Bristol, University Walk, Bristol BS8 1TW, UK

Abstract

By comparison with both experimental and numerical data, Dysthe's (1979) O4) modified nonlinear Schrödinger; equation has been shown to model the evolution of a slowly varying wavetrain well (here ε is the wave steepness). In this work, we extend the equation to include a prescribed, large-scale, O2) surface current which varies about a mean value. As an introduction, a heuristic derivation of the O3) current-modified equation, used by Bakhanov et al. (1996), is given, before a more formal approach is used to derive the O4) equation. Numerical solutions of the new equations are compared in one horizontal dimension with those from a fully nonlinear solver for velocity potential in the specific case of a sinusoidal surface current, such as may be due to an underlying internal wave. The comparisons are encouraging, especially for the O4) equation.

Type
Research Article
Copyright
© 1999 Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)