Large-scale, realistic laboratory modeling of M[subscript 2] internal tide generation at the Luzon Strait

The complex double-ridge system in the Luzon Strait in the South China Sea (SCS) is one of the strongest sources of internal tides in the oceans, associated with which are some of the largest amplitude internal solitary waves on record. An issue of debate, however, has been the specific nature of th...

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Main Authors: Mercier, Matthieu J., Gostiaux, Louis, Helfrich, Karl R., Sommeria, Joel, Viboud, Samuel, Didelle, Henri, Dauxois, Thierry, Peacock, Thomas, Ghaemsaidi, Sasan John
Other Authors: Massachusetts Institute of Technology. Department of Mechanical Engineering
Format: Article
Language:en_US
Published: American Geophysical Union (AGU) 2015
Online Access:http://hdl.handle.net/1721.1/97704
https://orcid.org/0000-0002-7639-0194
https://orcid.org/0000-0003-2548-3937
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author Mercier, Matthieu J.
Gostiaux, Louis
Helfrich, Karl R.
Sommeria, Joel
Viboud, Samuel
Didelle, Henri
Dauxois, Thierry
Peacock, Thomas
Ghaemsaidi, Sasan John
author2 Massachusetts Institute of Technology. Department of Mechanical Engineering
author_facet Massachusetts Institute of Technology. Department of Mechanical Engineering
Mercier, Matthieu J.
Gostiaux, Louis
Helfrich, Karl R.
Sommeria, Joel
Viboud, Samuel
Didelle, Henri
Dauxois, Thierry
Peacock, Thomas
Ghaemsaidi, Sasan John
author_sort Mercier, Matthieu J.
collection MIT
description The complex double-ridge system in the Luzon Strait in the South China Sea (SCS) is one of the strongest sources of internal tides in the oceans, associated with which are some of the largest amplitude internal solitary waves on record. An issue of debate, however, has been the specific nature of their generation mechanism. To provide insight, we present the results of a large-scale laboratory experiment performed at the Coriolis platform. The experiment was carefully designed so that the relevant dimensionless parameters, which include the excursion parameter, criticality, Rossby, and Froude numbers, closely matched the ocean scenario. The results advocate that a broad and coherent weakly nonlinear, three-dimensional, M[subscript 2] internal tide that is shaped by the overall geometry of the double-ridge system is radiated into the South China Sea and subsequently steepens, as opposed to being generated by a particular feature or localized region within the ridge system.
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spelling mit-1721.1/977042022-10-01T00:38:27Z Large-scale, realistic laboratory modeling of M[subscript 2] internal tide generation at the Luzon Strait Mercier, Matthieu J. Gostiaux, Louis Helfrich, Karl R. Sommeria, Joel Viboud, Samuel Didelle, Henri Dauxois, Thierry Peacock, Thomas Ghaemsaidi, Sasan John Massachusetts Institute of Technology. Department of Mechanical Engineering Mercier, Matthieu J. Ghaemsaidi, Sasan John Peacock, Thomas The complex double-ridge system in the Luzon Strait in the South China Sea (SCS) is one of the strongest sources of internal tides in the oceans, associated with which are some of the largest amplitude internal solitary waves on record. An issue of debate, however, has been the specific nature of their generation mechanism. To provide insight, we present the results of a large-scale laboratory experiment performed at the Coriolis platform. The experiment was carefully designed so that the relevant dimensionless parameters, which include the excursion parameter, criticality, Rossby, and Froude numbers, closely matched the ocean scenario. The results advocate that a broad and coherent weakly nonlinear, three-dimensional, M[subscript 2] internal tide that is shaped by the overall geometry of the double-ridge system is radiated into the South China Sea and subsequently steepens, as opposed to being generated by a particular feature or localized region within the ridge system. United States. Office of Naval Research (Grant N00014-09-1-0282) United States. Office of Naval Research (Grant N00014-09-1-0227) Centre National de la Recherche Scientifique (France). Projet international de cooperation scientifique (PICS) (Grant 5860) France. Agence nationale de la recherche (Grant 08-BLAN-0113-01) MIT-France Program 2015-07-07T18:58:55Z 2015-07-07T18:58:55Z 2013-11 2013-09 Article http://purl.org/eprint/type/JournalArticle 00948276 http://hdl.handle.net/1721.1/97704 Mercier, Matthieu J., Louis Gostiaux, Karl Helfrich, Joel Sommeria, Samuel Viboud, Henri Didelle, Sasan J. Ghaemsaidi, Thierry Dauxois, and Thomas Peacock. “Large-Scale, Realistic Laboratory Modeling of M[subscript 2] Internal Tide Generation at the Luzon Strait.” Geophys. Res. Lett. 40, no. 21 (November 4, 2013): 5704–5709. © 2013 American Geophysical Union https://orcid.org/0000-0002-7639-0194 https://orcid.org/0000-0003-2548-3937 en_US http://dx.doi.org/10.1002/2013GL058064 Geophysical Research Letters 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 Geophysical Union (AGU) American Geophysical Union
spellingShingle Mercier, Matthieu J.
Gostiaux, Louis
Helfrich, Karl R.
Sommeria, Joel
Viboud, Samuel
Didelle, Henri
Dauxois, Thierry
Peacock, Thomas
Ghaemsaidi, Sasan John
Large-scale, realistic laboratory modeling of M[subscript 2] internal tide generation at the Luzon Strait
title Large-scale, realistic laboratory modeling of M[subscript 2] internal tide generation at the Luzon Strait
title_full Large-scale, realistic laboratory modeling of M[subscript 2] internal tide generation at the Luzon Strait
title_fullStr Large-scale, realistic laboratory modeling of M[subscript 2] internal tide generation at the Luzon Strait
title_full_unstemmed Large-scale, realistic laboratory modeling of M[subscript 2] internal tide generation at the Luzon Strait
title_short Large-scale, realistic laboratory modeling of M[subscript 2] internal tide generation at the Luzon Strait
title_sort large scale realistic laboratory modeling of m subscript 2 internal tide generation at the luzon strait
url http://hdl.handle.net/1721.1/97704
https://orcid.org/0000-0002-7639-0194
https://orcid.org/0000-0003-2548-3937
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