Hostname: page-component-7b7567c8c-fvjsw Total loading time: 0 Render date: 2026-11-15T02:09:29.510Z Has data issue: false hasContentIssue false

Fourth-order nonlinear evolution equations for surface gravity waves in the presence of a thin thermocline

Published online by Cambridge University Press:  17 February 2009

Sudebi Bhattacharyya
Affiliation:
Department of Applied Mathematics, University of Calcutta, 92 Acharya Prafulla Chandra Road, Calcutta 700009, INDIA
K. P. Das
Affiliation:
Department of Applied Mathematics, University of Calcutta, 92 Acharya Prafulla Chandra Road, Calcutta 700009, INDIA
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the 'Save PDF' action button.

Two coupled nonlinear evolution equations correct to fourth order in wave steepness are derived for a three-dimensional wave packet in the presence of a thin thermocline. These two coupled equations are reduced to a single equation on the assumption that the space variation of the amplitudes takes place along a line making an arbitrary fixed angle with the direction of propagation of the wave. This single equation is used to study the stability of a uniform wave train. Expressions for maximum growth rate of instability and wave number at marginal stability are obtained. Some of the results are shown graphically. It is found that a thin thermocline has a stabilizing influence and the maximum growth rate of instability decreases with the increase of thermocline depth.

Information

Type
Research Article
Copyright
Copyright © Australian Mathematical Society 1997