Numerical Simulation of Shoaling Internal Solitary Waves in Two-layer Fluid Flow

In this paper, we look at the propagation of internal solitary waves over three different types of slowly varying region, i.e. a slowly increasing slope, a smooth bump and a parabolic mound in a two-layer fluid flow. The appropriate mathematical model for this problem is the variable-coefficient ext...

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Main Authors: Hooi, M. H., Tiong, Wei King, Tay, K.G., Chiew, Kang Leng, Sze, San Nah
Format: Article
Language:English
Published: Penerbit UTM Press 2018
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Online Access:http://ir.unimas.my/id/eprint/24301/1/Numerical%20Simulation%20of%20Shoaling%20Internal%20Solitary%20Waves%20in%20Two-layer%20Fluid%20Flow%20-%20Copy.pdf
http://ir.unimas.my/id/eprint/24301/
https://matematika.utm.my/index.php/matematika/article/view/1000
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spelling my.unimas.ir.243012022-09-29T02:41:39Z http://ir.unimas.my/id/eprint/24301/ Numerical Simulation of Shoaling Internal Solitary Waves in Two-layer Fluid Flow Hooi, M. H. Tiong, Wei King Tay, K.G. Chiew, Kang Leng Sze, San Nah QA Mathematics In this paper, we look at the propagation of internal solitary waves over three different types of slowly varying region, i.e. a slowly increasing slope, a smooth bump and a parabolic mound in a two-layer fluid flow. The appropriate mathematical model for this problem is the variable-coefficient extended Korteweg-de Vries equation. The governing equation is then solved numerically using the method of lines. Our numerical simulations show that the internal solitary waves deforms adiabatically on the slowly increasing slope. At the same time, a trailing shelf is generated as the internal solitary wave propagates over the slope, which would then decompose into secondary solitary waves or a wavetrain. On the other hand, when internal solitary waves propagate over a smooth bump or a parabolic mound, a trailing shelf of negative polarity would be generated as the results of the interaction of the internal solitary wave with the decreasing slope of the bump or the parabolic mound. The secondary solitary waves is observed to be climbing the negative trailing shelf. Penerbit UTM Press 2018 Article PeerReviewed text en http://ir.unimas.my/id/eprint/24301/1/Numerical%20Simulation%20of%20Shoaling%20Internal%20Solitary%20Waves%20in%20Two-layer%20Fluid%20Flow%20-%20Copy.pdf Hooi, M. H. and Tiong, Wei King and Tay, K.G. and Chiew, Kang Leng and Sze, San Nah (2018) Numerical Simulation of Shoaling Internal Solitary Waves in Two-layer Fluid Flow. Matematika, 34 (2). pp. 333-350. ISSN 0127-9602 https://matematika.utm.my/index.php/matematika/article/view/1000 DOI:.org/10.11113/matematika.v34.n2.1000
institution Universiti Malaysia Sarawak
building Centre for Academic Information Services (CAIS)
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Malaysia Sarawak
content_source UNIMAS Institutional Repository
url_provider http://ir.unimas.my/
language English
topic QA Mathematics
spellingShingle QA Mathematics
Hooi, M. H.
Tiong, Wei King
Tay, K.G.
Chiew, Kang Leng
Sze, San Nah
Numerical Simulation of Shoaling Internal Solitary Waves in Two-layer Fluid Flow
description In this paper, we look at the propagation of internal solitary waves over three different types of slowly varying region, i.e. a slowly increasing slope, a smooth bump and a parabolic mound in a two-layer fluid flow. The appropriate mathematical model for this problem is the variable-coefficient extended Korteweg-de Vries equation. The governing equation is then solved numerically using the method of lines. Our numerical simulations show that the internal solitary waves deforms adiabatically on the slowly increasing slope. At the same time, a trailing shelf is generated as the internal solitary wave propagates over the slope, which would then decompose into secondary solitary waves or a wavetrain. On the other hand, when internal solitary waves propagate over a smooth bump or a parabolic mound, a trailing shelf of negative polarity would be generated as the results of the interaction of the internal solitary wave with the decreasing slope of the bump or the parabolic mound. The secondary solitary waves is observed to be climbing the negative trailing shelf.
format Article
author Hooi, M. H.
Tiong, Wei King
Tay, K.G.
Chiew, Kang Leng
Sze, San Nah
author_facet Hooi, M. H.
Tiong, Wei King
Tay, K.G.
Chiew, Kang Leng
Sze, San Nah
author_sort Hooi, M. H.
title Numerical Simulation of Shoaling Internal Solitary Waves in Two-layer Fluid Flow
title_short Numerical Simulation of Shoaling Internal Solitary Waves in Two-layer Fluid Flow
title_full Numerical Simulation of Shoaling Internal Solitary Waves in Two-layer Fluid Flow
title_fullStr Numerical Simulation of Shoaling Internal Solitary Waves in Two-layer Fluid Flow
title_full_unstemmed Numerical Simulation of Shoaling Internal Solitary Waves in Two-layer Fluid Flow
title_sort numerical simulation of shoaling internal solitary waves in two-layer fluid flow
publisher Penerbit UTM Press
publishDate 2018
url http://ir.unimas.my/id/eprint/24301/1/Numerical%20Simulation%20of%20Shoaling%20Internal%20Solitary%20Waves%20in%20Two-layer%20Fluid%20Flow%20-%20Copy.pdf
http://ir.unimas.my/id/eprint/24301/
https://matematika.utm.my/index.php/matematika/article/view/1000
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score 13.188404