Turbulent dissipation along contrasting internal tide paths off the Amazon shelf from AMAZOMIX

<p>The Amazon shelf break is a key oceanic region where strong internal tides (ITs) are generated, playing a substantial role in climate processes and ecosystems through vertical dissipation and mixing. During the AMAZOMIX survey (2021), currents, hydrography, and turbulence were measured over...

Full description

Saved in:
Bibliographic Details
Main Authors: F. Kouogang, A. Koch-Larrouy, J. Magalhaes, A. Costa da Silva, D. Kerhervé, A. Bertrand, E. Cervelli, F. Assene, J.-F. Ternon, P. Rousselot, J. Lee, M. Rollnic, M. Araujo
Format: Article
Language:English
Published: Copernicus Publications 2025-07-01
Series:Ocean Science
Online Access:https://os.copernicus.org/articles/21/1589/2025/os-21-1589-2025.pdf
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1839609794114093056
author F. Kouogang
F. Kouogang
A. Koch-Larrouy
J. Magalhaes
A. Costa da Silva
D. Kerhervé
A. Bertrand
E. Cervelli
F. Assene
F. Assene
J.-F. Ternon
P. Rousselot
J. Lee
M. Rollnic
M. Araujo
author_facet F. Kouogang
F. Kouogang
A. Koch-Larrouy
J. Magalhaes
A. Costa da Silva
D. Kerhervé
A. Bertrand
E. Cervelli
F. Assene
F. Assene
J.-F. Ternon
P. Rousselot
J. Lee
M. Rollnic
M. Araujo
author_sort F. Kouogang
collection DOAJ
description <p>The Amazon shelf break is a key oceanic region where strong internal tides (ITs) are generated, playing a substantial role in climate processes and ecosystems through vertical dissipation and mixing. During the AMAZOMIX survey (2021), currents, hydrography, and turbulence were measured over the M<span class="inline-formula"><sub>2</sub></span> tidal period (12.42 h) at multiple stations along both high (HTE) and low (LTE) tidal energy paths, covering IT generation and propagation regions off the Amazon shelf. This dataset provides a unique opportunity to assess IT-driven vertical dissipation and quantify its spatial extent and influence in the region.</p> <p>Microstructure analyses, integrated with hydrographic data, highlighted contrasting dissipation rates. The highest rates occurred at IT generation sites along the HTE paths, while the lowest rates were observed on the slope along the LTE path. Near generation sites, the dissipation rates were elevated, [<span class="inline-formula">10<sup>−6</sup></span>] <span class="inline-formula">W kg<sup>−1</sup></span>, with IT shear contributing <span class="inline-formula">∼60</span> % compared to the mean baroclinic current (MBC) shear. Along IT paths, rates decreased to [<span class="inline-formula">10<sup>−8</sup></span>] <span class="inline-formula">W kg<sup>−1</sup></span> but remained substantial, driven by nearly equal contributions from IT and MBC shear.</p> <p>A key finding was the relative increase in turbulent dissipation ([<span class="inline-formula">10<sup>−7</sup></span>] <span class="inline-formula">W kg<sup>−1</sup></span>) <span class="inline-formula">∼230</span> km from two distinct IT generation sites at the shelf break. This zone of high mixing was located in an area where the general circulation vanished, coinciding with a region of potential constructive interference of IT rays originating from different generation sites. It also aligned with the occurrence of large-amplitude internal solitary waves (ISWs), suggesting that constructive IT ray interference may generate nonlinear ISWs that lead to enhanced dissipation.</p>
format Article
id doaj-art-c0645bcdc74940f1806a3b6c5850c67b
institution Matheson Library
issn 1812-0784
1812-0792
language English
publishDate 2025-07-01
publisher Copernicus Publications
record_format Article
series Ocean Science
spelling doaj-art-c0645bcdc74940f1806a3b6c5850c67b2025-07-30T05:51:14ZengCopernicus PublicationsOcean Science1812-07841812-07922025-07-01211589160810.5194/os-21-1589-2025Turbulent dissipation along contrasting internal tide paths off the Amazon shelf from AMAZOMIXF. Kouogang0F. Kouogang1A. Koch-Larrouy2J. Magalhaes3A. Costa da Silva4D. Kerhervé5A. Bertrand6E. Cervelli7F. Assene8F. Assene9J.-F. Ternon10P. Rousselot11J. Lee12M. Rollnic13M. Araujo14CECI, Université de Toulouse, CERFACS/CNRS/IRD, Toulouse, FranceDepartamento de Oceanografia, Universidade Federal de Pernambuco, DOCEAN/UFPE, Recife, BrazilCECI, Université de Toulouse, CERFACS/CNRS/IRD, Toulouse, FranceDepartment of Geoscience, Environment and Spatial Planning (DGAOT), Faculty of Sciences, University of Porto, Porto, PortugalCentro Euro-Mediterraneo sui Cambiamenti Climatici, Bologna, ItalyCECI, Université de Toulouse, CERFACS/CNRS/IRD, Toulouse, FranceDepartamento de Oceanografia, Universidade Federal de Pernambuco, DOCEAN/UFPE, Recife, BrazilRockland Scientific Inc, Lunenburg, Nova Scotia, CanadaCentro Euro-Mediterraneo sui Cambiamenti Climatici, Bologna, ItalyDepartment of Maritime Navigation and Information Systems, National Advanced School of Maritime and Ocean Science and Technology (ENSTMO), University of Ebolowa, Ebolowa, CameroonMARBEC, Université de Montpellier, CNRS, Ifremer, IRD, Sète, FranceIMAGO, Université de Bretagne Occidentale, CNRS, Ifremer, IRD, Brest, FranceDepartamento de Oceanografia, Universidade Federal do Pará, UFPA, Belém, BrazilDepartamento de Oceanografia, Universidade Federal do Pará, UFPA, Belém, BrazilDepartamento de Oceanografia, Universidade Federal de Pernambuco, DOCEAN/UFPE, Recife, Brazil<p>The Amazon shelf break is a key oceanic region where strong internal tides (ITs) are generated, playing a substantial role in climate processes and ecosystems through vertical dissipation and mixing. During the AMAZOMIX survey (2021), currents, hydrography, and turbulence were measured over the M<span class="inline-formula"><sub>2</sub></span> tidal period (12.42 h) at multiple stations along both high (HTE) and low (LTE) tidal energy paths, covering IT generation and propagation regions off the Amazon shelf. This dataset provides a unique opportunity to assess IT-driven vertical dissipation and quantify its spatial extent and influence in the region.</p> <p>Microstructure analyses, integrated with hydrographic data, highlighted contrasting dissipation rates. The highest rates occurred at IT generation sites along the HTE paths, while the lowest rates were observed on the slope along the LTE path. Near generation sites, the dissipation rates were elevated, [<span class="inline-formula">10<sup>−6</sup></span>] <span class="inline-formula">W kg<sup>−1</sup></span>, with IT shear contributing <span class="inline-formula">∼60</span> % compared to the mean baroclinic current (MBC) shear. Along IT paths, rates decreased to [<span class="inline-formula">10<sup>−8</sup></span>] <span class="inline-formula">W kg<sup>−1</sup></span> but remained substantial, driven by nearly equal contributions from IT and MBC shear.</p> <p>A key finding was the relative increase in turbulent dissipation ([<span class="inline-formula">10<sup>−7</sup></span>] <span class="inline-formula">W kg<sup>−1</sup></span>) <span class="inline-formula">∼230</span> km from two distinct IT generation sites at the shelf break. This zone of high mixing was located in an area where the general circulation vanished, coinciding with a region of potential constructive interference of IT rays originating from different generation sites. It also aligned with the occurrence of large-amplitude internal solitary waves (ISWs), suggesting that constructive IT ray interference may generate nonlinear ISWs that lead to enhanced dissipation.</p>https://os.copernicus.org/articles/21/1589/2025/os-21-1589-2025.pdf
spellingShingle F. Kouogang
F. Kouogang
A. Koch-Larrouy
J. Magalhaes
A. Costa da Silva
D. Kerhervé
A. Bertrand
E. Cervelli
F. Assene
F. Assene
J.-F. Ternon
P. Rousselot
J. Lee
M. Rollnic
M. Araujo
Turbulent dissipation along contrasting internal tide paths off the Amazon shelf from AMAZOMIX
Ocean Science
title Turbulent dissipation along contrasting internal tide paths off the Amazon shelf from AMAZOMIX
title_full Turbulent dissipation along contrasting internal tide paths off the Amazon shelf from AMAZOMIX
title_fullStr Turbulent dissipation along contrasting internal tide paths off the Amazon shelf from AMAZOMIX
title_full_unstemmed Turbulent dissipation along contrasting internal tide paths off the Amazon shelf from AMAZOMIX
title_short Turbulent dissipation along contrasting internal tide paths off the Amazon shelf from AMAZOMIX
title_sort turbulent dissipation along contrasting internal tide paths off the amazon shelf from amazomix
url https://os.copernicus.org/articles/21/1589/2025/os-21-1589-2025.pdf
work_keys_str_mv AT fkouogang turbulentdissipationalongcontrastinginternaltidepathsofftheamazonshelffromamazomix
AT fkouogang turbulentdissipationalongcontrastinginternaltidepathsofftheamazonshelffromamazomix
AT akochlarrouy turbulentdissipationalongcontrastinginternaltidepathsofftheamazonshelffromamazomix
AT jmagalhaes turbulentdissipationalongcontrastinginternaltidepathsofftheamazonshelffromamazomix
AT acostadasilva turbulentdissipationalongcontrastinginternaltidepathsofftheamazonshelffromamazomix
AT dkerherve turbulentdissipationalongcontrastinginternaltidepathsofftheamazonshelffromamazomix
AT abertrand turbulentdissipationalongcontrastinginternaltidepathsofftheamazonshelffromamazomix
AT ecervelli turbulentdissipationalongcontrastinginternaltidepathsofftheamazonshelffromamazomix
AT fassene turbulentdissipationalongcontrastinginternaltidepathsofftheamazonshelffromamazomix
AT fassene turbulentdissipationalongcontrastinginternaltidepathsofftheamazonshelffromamazomix
AT jfternon turbulentdissipationalongcontrastinginternaltidepathsofftheamazonshelffromamazomix
AT prousselot turbulentdissipationalongcontrastinginternaltidepathsofftheamazonshelffromamazomix
AT jlee turbulentdissipationalongcontrastinginternaltidepathsofftheamazonshelffromamazomix
AT mrollnic turbulentdissipationalongcontrastinginternaltidepathsofftheamazonshelffromamazomix
AT maraujo turbulentdissipationalongcontrastinginternaltidepathsofftheamazonshelffromamazomix