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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Main Authors: Paramita Maiti, B. N. Mandal
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2004
Subjects:
Online Access: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
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spelling 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)
institution Open Polar
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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
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