On transformation of flexural gravity waves

In the present paper, flexural gravity wave transformation due to a heterogeneous ice-sheet floating on the free surface with change in bottom topography is analyzed in finite water depth. In case of flexural gravity waves, the wave energy density is defined as a combina-tion of strain energy of the...

Full description

Bibliographic Details
Main Authors: J. Bhattacharjee, D. Karmakar, T. Sahoo
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Ice Sheet
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.525.5419
http://www.iwwwfb.org/Abstracts/iwwwfb22/iwwwfb22_02.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.525.5419
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.525.5419 2023-05-15T16:39:49+02:00 On transformation of flexural gravity waves J. Bhattacharjee D. Karmakar T. Sahoo The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.525.5419 http://www.iwwwfb.org/Abstracts/iwwwfb22/iwwwfb22_02.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.525.5419 http://www.iwwwfb.org/Abstracts/iwwwfb22/iwwwfb22_02.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.iwwwfb.org/Abstracts/iwwwfb22/iwwwfb22_02.pdf text ftciteseerx 2016-01-08T10:20:26Z In the present paper, flexural gravity wave transformation due to a heterogeneous ice-sheet floating on the free surface with change in bottom topography is analyzed in finite water depth. In case of flexural gravity waves, the wave energy density is defined as a combina-tion of strain energy of the ice sheet, the potential energy and kinetic energy. Using the Text Ice Sheet Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description In the present paper, flexural gravity wave transformation due to a heterogeneous ice-sheet floating on the free surface with change in bottom topography is analyzed in finite water depth. In case of flexural gravity waves, the wave energy density is defined as a combina-tion of strain energy of the ice sheet, the potential energy and kinetic energy. Using the
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author J. Bhattacharjee
D. Karmakar
T. Sahoo
spellingShingle J. Bhattacharjee
D. Karmakar
T. Sahoo
On transformation of flexural gravity waves
author_facet J. Bhattacharjee
D. Karmakar
T. Sahoo
author_sort J. Bhattacharjee
title On transformation of flexural gravity waves
title_short On transformation of flexural gravity waves
title_full On transformation of flexural gravity waves
title_fullStr On transformation of flexural gravity waves
title_full_unstemmed On transformation of flexural gravity waves
title_sort on transformation of flexural gravity waves
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.525.5419
http://www.iwwwfb.org/Abstracts/iwwwfb22/iwwwfb22_02.pdf
genre Ice Sheet
genre_facet Ice Sheet
op_source http://www.iwwwfb.org/Abstracts/iwwwfb22/iwwwfb22_02.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.525.5419
http://www.iwwwfb.org/Abstracts/iwwwfb22/iwwwfb22_02.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
_version_ 1766030160248700928

Similar Items