Waves due to initial disturbances at the inertial surface in a stratified fluid of finite depth

This paper is concerned with a Cauchy-Poisson problem in a weakly stratified ocean of uniform finite depth bounded above by an inertial surface (IS). The inertial surface is composed of a thin but uniform distribution of noninteracting materials. The techniques of Laplace transform in time and eithe...

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Main Authors: Prity Ghosh, Uma Basu, B. N. Mandal
Format: Article
Language:English
Published: Wiley 2000-01-01
Series:International Journal of Mathematics and Mathematical Sciences
Subjects:
Online Access:http://dx.doi.org/10.1155/S0161171200001605
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author Prity Ghosh
Uma Basu
B. N. Mandal
author_facet Prity Ghosh
Uma Basu
B. N. Mandal
author_sort Prity Ghosh
collection DOAJ
description This paper is concerned with a Cauchy-Poisson problem in a weakly stratified ocean of uniform finite depth bounded above by an inertial surface (IS). The inertial surface is composed of a thin but uniform distribution of noninteracting materials. The techniques of Laplace transform in time and either Green's integral theorem or Fourier transform have been utilized in the mathematical analysis to obtain the form of the inertial surface in terms of an integral. The asymptotic behaviour of the inertial surface is obtained for large time and distance and displayed graphically. The effect of stratification is discussed.
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institution Kabale University
issn 0161-1712
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language English
publishDate 2000-01-01
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series International Journal of Mathematics and Mathematical Sciences
spelling doaj-art-81b2ce03836a43ecab9b954f77c5bf6b2025-02-03T07:26:14ZengWileyInternational Journal of Mathematics and Mathematical Sciences0161-17121687-04252000-01-0124426527610.1155/S0161171200001605Waves due to initial disturbances at the inertial surface in a stratified fluid of finite depthPrity Ghosh0Uma Basu1B. N. Mandal2Physics and Applied Mathematics Unit, Indian Statistical Institute, 203 B. T. Road, Calcutta 700 035, IndiaDepartment of Applied Mathematics, University of Calcutta, 92 A. P. C. Road, Calcutta 700 009, IndiaPhysics and Applied Mathematics Unit, Indian Statistical Institute, 203 B. T. Road, Calcutta 700 035, IndiaThis paper is concerned with a Cauchy-Poisson problem in a weakly stratified ocean of uniform finite depth bounded above by an inertial surface (IS). The inertial surface is composed of a thin but uniform distribution of noninteracting materials. The techniques of Laplace transform in time and either Green's integral theorem or Fourier transform have been utilized in the mathematical analysis to obtain the form of the inertial surface in terms of an integral. The asymptotic behaviour of the inertial surface is obtained for large time and distance and displayed graphically. The effect of stratification is discussed.http://dx.doi.org/10.1155/S0161171200001605Stratified fluidBoussinesq approximation initial disturbanceinertial surface.
spellingShingle Prity Ghosh
Uma Basu
B. N. Mandal
Waves due to initial disturbances at the inertial surface in a stratified fluid of finite depth
International Journal of Mathematics and Mathematical Sciences
Stratified fluid
Boussinesq approximation
initial disturbance
inertial surface.
title Waves due to initial disturbances at the inertial surface in a stratified fluid of finite depth
title_full Waves due to initial disturbances at the inertial surface in a stratified fluid of finite depth
title_fullStr Waves due to initial disturbances at the inertial surface in a stratified fluid of finite depth
title_full_unstemmed Waves due to initial disturbances at the inertial surface in a stratified fluid of finite depth
title_short Waves due to initial disturbances at the inertial surface in a stratified fluid of finite depth
title_sort waves due to initial disturbances at the inertial surface in a stratified fluid of finite depth
topic Stratified fluid
Boussinesq approximation
initial disturbance
inertial surface.
url http://dx.doi.org/10.1155/S0161171200001605
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AT umabasu wavesduetoinitialdisturbancesattheinertialsurfaceinastratifiedfluidoffinitedepth
AT bnmandal wavesduetoinitialdisturbancesattheinertialsurfaceinastratifiedfluidoffinitedepth