Three-dimensional waves beneath an ice sheet due to a steadily moving pressure
Solutions of the nonlinear water wave equations under an ice sheet are computed using a boundary integral equation method. The ice sheet is modelled as a thin elastic plate and the fluid equations are nonlinear. Depending on the velocity of the moving disturbance generating the flow, different types...
Published in: | Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences |
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Language: | English |
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crroyalsociety:10.1098/rsta.2011.0115 2024-09-15T18:12:06+00:00 Three-dimensional waves beneath an ice sheet due to a steadily moving pressure Părău, Emilian I. Vanden-Broeck, Jean-Marc 2011 http://dx.doi.org/10.1098/rsta.2011.0115 https://royalsocietypublishing.org/doi/pdf/10.1098/rsta.2011.0115 https://royalsocietypublishing.org/doi/full-xml/10.1098/rsta.2011.0115 en eng The Royal Society https://royalsociety.org/journals/ethics-policies/data-sharing-mining/ Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences volume 369, issue 1947, page 2973-2988 ISSN 1364-503X 1471-2962 journal-article 2011 crroyalsociety https://doi.org/10.1098/rsta.2011.0115 2024-08-12T04:27:49Z Solutions of the nonlinear water wave equations under an ice sheet are computed using a boundary integral equation method. The ice sheet is modelled as a thin elastic plate and the fluid equations are nonlinear. Depending on the velocity of the moving disturbance generating the flow, different types of responses of the floating ice sheet are discussed. Article in Journal/Newspaper Ice Sheet The Royal Society Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 369 1947 2973 2988 |
institution |
Open Polar |
collection |
The Royal Society |
op_collection_id |
crroyalsociety |
language |
English |
description |
Solutions of the nonlinear water wave equations under an ice sheet are computed using a boundary integral equation method. The ice sheet is modelled as a thin elastic plate and the fluid equations are nonlinear. Depending on the velocity of the moving disturbance generating the flow, different types of responses of the floating ice sheet are discussed. |
format |
Article in Journal/Newspaper |
author |
Părău, Emilian I. Vanden-Broeck, Jean-Marc |
spellingShingle |
Părău, Emilian I. Vanden-Broeck, Jean-Marc Three-dimensional waves beneath an ice sheet due to a steadily moving pressure |
author_facet |
Părău, Emilian I. Vanden-Broeck, Jean-Marc |
author_sort |
Părău, Emilian I. |
title |
Three-dimensional waves beneath an ice sheet due to a steadily moving pressure |
title_short |
Three-dimensional waves beneath an ice sheet due to a steadily moving pressure |
title_full |
Three-dimensional waves beneath an ice sheet due to a steadily moving pressure |
title_fullStr |
Three-dimensional waves beneath an ice sheet due to a steadily moving pressure |
title_full_unstemmed |
Three-dimensional waves beneath an ice sheet due to a steadily moving pressure |
title_sort |
three-dimensional waves beneath an ice sheet due to a steadily moving pressure |
publisher |
The Royal Society |
publishDate |
2011 |
url |
http://dx.doi.org/10.1098/rsta.2011.0115 https://royalsocietypublishing.org/doi/pdf/10.1098/rsta.2011.0115 https://royalsocietypublishing.org/doi/full-xml/10.1098/rsta.2011.0115 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences volume 369, issue 1947, page 2973-2988 ISSN 1364-503X 1471-2962 |
op_rights |
https://royalsociety.org/journals/ethics-policies/data-sharing-mining/ |
op_doi |
https://doi.org/10.1098/rsta.2011.0115 |
container_title |
Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences |
container_volume |
369 |
container_issue |
1947 |
container_start_page |
2973 |
op_container_end_page |
2988 |
_version_ |
1810449684422983680 |