Lagrangian coherent structures and internal wave attractors

For a nonuniformly stratified layer of fluid, internal gravity waves propagate at varying angles depending on the local buoyancy and Coriolis (in geophysical applications) frequencies. Relatively confined geometries, such as multiple submarine ridges, can support internal wave attractors, which can...

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Main Authors: Tang, Wenbo, Peacock, Thomas
Other Authors: Massachusetts Institute of Technology. Department of Mechanical Engineering
Format: Article
Language:en_US
Published: American Institute of Physics 2013
Online Access:http://hdl.handle.net/1721.1/79349
https://orcid.org/0000-0002-7639-0194
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author Tang, Wenbo
Peacock, Thomas
author2 Massachusetts Institute of Technology. Department of Mechanical Engineering
author_facet Massachusetts Institute of Technology. Department of Mechanical Engineering
Tang, Wenbo
Peacock, Thomas
author_sort Tang, Wenbo
collection MIT
description For a nonuniformly stratified layer of fluid, internal gravity waves propagate at varying angles depending on the local buoyancy and Coriolis (in geophysical applications) frequencies. Relatively confined geometries, such as multiple submarine ridges, can support internal wave attractors, which can be viewed as Lagrangian coherent structures for the energy density flux. Since traditional approaches for locating these structures prove cumbersome, here we develop an approach that efficiently extracts the locations of internal wave attractors, as well as quantifying the rate of attraction. Using realistic geometry and stratification from ocean observations, we find that a significant northern portion of the Luzon ridge can support internal wave attractors.
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spelling mit-1721.1/793492022-10-03T08:04:13Z Lagrangian coherent structures and internal wave attractors Tang, Wenbo Peacock, Thomas Massachusetts Institute of Technology. Department of Mechanical Engineering Peacock, Thomas For a nonuniformly stratified layer of fluid, internal gravity waves propagate at varying angles depending on the local buoyancy and Coriolis (in geophysical applications) frequencies. Relatively confined geometries, such as multiple submarine ridges, can support internal wave attractors, which can be viewed as Lagrangian coherent structures for the energy density flux. Since traditional approaches for locating these structures prove cumbersome, here we develop an approach that efficiently extracts the locations of internal wave attractors, as well as quantifying the rate of attraction. Using realistic geometry and stratification from ocean observations, we find that a significant northern portion of the Luzon ridge can support internal wave attractors. United States. Office of Naval Research (ONR Grant No. N00014-09-0282 ) 2013-06-20T14:27:30Z 2013-06-20T14:27:30Z 2010-01 2009-08 Article http://purl.org/eprint/type/JournalArticle 1089-7682 1054-1500 http://hdl.handle.net/1721.1/79349 Tang, Wenbo, and Thomas Peacock. Lagrangian Coherent Structures and Internal Wave Attractors. Chaos: An Interdisciplinary Journal of Nonlinear Science 20, no. 1 (2010): 017508. © 2010 American Institute of Physics. https://orcid.org/0000-0002-7639-0194 en_US http://dx.doi.org/10.1063/1.3273054 Chaos: An Interdisciplinary Journal of Nonlinear Science Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. application/pdf American Institute of Physics MIT web domain
spellingShingle Tang, Wenbo
Peacock, Thomas
Lagrangian coherent structures and internal wave attractors
title Lagrangian coherent structures and internal wave attractors
title_full Lagrangian coherent structures and internal wave attractors
title_fullStr Lagrangian coherent structures and internal wave attractors
title_full_unstemmed Lagrangian coherent structures and internal wave attractors
title_short Lagrangian coherent structures and internal wave attractors
title_sort lagrangian coherent structures and internal wave attractors
url http://hdl.handle.net/1721.1/79349
https://orcid.org/0000-0002-7639-0194
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