WATER WAVES GENERATED BY DISTURBANCES AT
This paper is concerned with two-dimensional unsteady motion of water waves gener-ated by an initial disturbance created at an ice sheet covering the water. The ice cover is modeled as a thin elastic plate. Using linear theory, the problem is formulated as an ini-tial value problem for the velocity...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.526.3473 2023-05-15T16:40:47+02:00 WATER WAVES GENERATED BY DISTURBANCES AT Paramita Maiti B. N. Mandal The Pennsylvania State University CiteSeerX Archives 2004 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.526.3473 http://emis.maths.adelaide.edu.au/journals/HOA/IJMMS/Volume2005_5/746.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.526.3473 http://emis.maths.adelaide.edu.au/journals/HOA/IJMMS/Volume2005_5/746.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://emis.maths.adelaide.edu.au/journals/HOA/IJMMS/Volume2005_5/746.pdf text 2004 ftciteseerx 2016-01-08T10:22:26Z This paper is concerned with two-dimensional unsteady motion of water waves gener-ated by an initial disturbance created at an ice sheet covering the water. The ice cover is modeled as a thin elastic plate. Using linear theory, the problem is formulated as an ini-tial value problem for the velocity potential describing the motion in the liquid. In the mathematical analysis, the Laplace and Fourier transform techniques have been utilized to obtain the depression of the ice-covered surface in the form of an infinite integral. For the special case of initial disturbance concentrated at the origin, taken on the ice cover, this integral is evaluated asymptotically by the method of a stationary phase for a long time and large distance from the origin. The form of the ice-covered surface is graphi-cally depicted for two types of initial disturbances. 1. Text Ice Sheet Unknown Laplace ENVELOPE(141.467,141.467,-66.782,-66.782) |
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ftciteseerx |
language |
English |
description |
This paper is concerned with two-dimensional unsteady motion of water waves gener-ated by an initial disturbance created at an ice sheet covering the water. The ice cover is modeled as a thin elastic plate. Using linear theory, the problem is formulated as an ini-tial value problem for the velocity potential describing the motion in the liquid. In the mathematical analysis, the Laplace and Fourier transform techniques have been utilized to obtain the depression of the ice-covered surface in the form of an infinite integral. For the special case of initial disturbance concentrated at the origin, taken on the ice cover, this integral is evaluated asymptotically by the method of a stationary phase for a long time and large distance from the origin. The form of the ice-covered surface is graphi-cally depicted for two types of initial disturbances. 1. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Paramita Maiti B. N. Mandal |
spellingShingle |
Paramita Maiti B. N. Mandal WATER WAVES GENERATED BY DISTURBANCES AT |
author_facet |
Paramita Maiti B. N. Mandal |
author_sort |
Paramita Maiti |
title |
WATER WAVES GENERATED BY DISTURBANCES AT |
title_short |
WATER WAVES GENERATED BY DISTURBANCES AT |
title_full |
WATER WAVES GENERATED BY DISTURBANCES AT |
title_fullStr |
WATER WAVES GENERATED BY DISTURBANCES AT |
title_full_unstemmed |
WATER WAVES GENERATED BY DISTURBANCES AT |
title_sort |
water waves generated by disturbances at |
publishDate |
2004 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.526.3473 http://emis.maths.adelaide.edu.au/journals/HOA/IJMMS/Volume2005_5/746.pdf |
long_lat |
ENVELOPE(141.467,141.467,-66.782,-66.782) |
geographic |
Laplace |
geographic_facet |
Laplace |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
http://emis.maths.adelaide.edu.au/journals/HOA/IJMMS/Volume2005_5/746.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.526.3473 http://emis.maths.adelaide.edu.au/journals/HOA/IJMMS/Volume2005_5/746.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766031206380470272 |