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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Online Access: | https://ueaeprints.uea.ac.uk/id/eprint/35651/ https://doi.org/10.1098/rsta.2011.0115 |
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ftuniveastangl:oai:ueaeprints.uea.ac.uk:35651 2023-05-15T16:39:33+02:00 Three-dimensional waves beneath an ice sheet due to a steadily moving pressure Părău, Emilian I. Vanden-Broeck, Jean-Marc 2011 https://ueaeprints.uea.ac.uk/id/eprint/35651/ https://doi.org/10.1098/rsta.2011.0115 unknown Părău, Emilian I. and Vanden-Broeck, Jean-Marc (2011) Three-dimensional waves beneath an ice sheet due to a steadily moving pressure. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 369 (1947). pp. 2973-2988. ISSN 1364-503X doi:10.1098/rsta.2011.0115 Article PeerReviewed 2011 ftuniveastangl https://doi.org/10.1098/rsta.2011.0115 2023-01-30T21:32:01Z 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 University of East Anglia: UEA Digital Repository Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 369 1947 2973 2988 |
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Open Polar |
collection |
University of East Anglia: UEA Digital Repository |
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ftuniveastangl |
language |
unknown |
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 |
publishDate |
2011 |
url |
https://ueaeprints.uea.ac.uk/id/eprint/35651/ https://doi.org/10.1098/rsta.2011.0115 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
Părău, Emilian I. and Vanden-Broeck, Jean-Marc (2011) Three-dimensional waves beneath an ice sheet due to a steadily moving pressure. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 369 (1947). pp. 2973-2988. ISSN 1364-503X doi:10.1098/rsta.2011.0115 |
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_ |
1766029885369745408 |