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...

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Published in:Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
Main Authors: Părău, Emilian I., Vanden-Broeck, Jean-Marc
Format: Article in Journal/Newspaper
Language:unknown
Published: 2011
Subjects:
Online Access:https://ueaeprints.uea.ac.uk/id/eprint/35651/
https://doi.org/10.1098/rsta.2011.0115
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spelling 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
institution Open Polar
collection University of East Anglia: UEA Digital Repository
op_collection_id 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
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