Articles | Volume 22, issue 3
https://doi.org/10.5194/os-22-1545-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-22-1545-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Internal tides–cyclonic eddy interaction and intermodal energy pathways: evidence from 3 km NEMO-AMAZON36 simulations
Fabius Kouogang
CORRESPONDING AUTHOR
CECI, Université de Toulouse, CERFACS/CNRS/IRD, Toulouse, France
Departamento de Oceanografia, Universidade Federal de Pernambuco, DOCEAN/UFPE, Recife, Brazil
Ariane Koch-Larrouy
CECI, Université de Toulouse, CERFACS/CNRS/IRD, Toulouse, France
Xavier Carton
Physical and Spatial Oceanography Laboratory, European Institute for Marine Studies, University of Western Brittany, Plouzane, France
Fernand Assene
Department of Maritime Navigation and Information System, National Advanced School of Maritime and Ocean Science and Technology (NASMOST), University of Ebolowa, Kribi, Cameroon
Guillaume Morvan
Université de Toulouse, LEGOS (CNES/CNRS/IRD/UT3), Toulouse, France
Moacyr Araujo
Departamento de Oceanografia, Universidade Federal de Pernambuco, DOCEAN/UFPE, Recife, Brazil
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Twin simulations, with and without tides, are used to assess the impact of internal tides (ITs) on ocean temperature off the Amazon mouth at a seasonal scale. We found that in the surface layers, ITs and barotropic tides cause a cooling effect on sea surface temperature, subsequently leading to an increase in the net heat flux between the atmosphere and ocean. Vertical mixing is identified as the primary driver, followed by vertical and horizontal advection.
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Edward D. Zaron, Tonia A. Capuano, and Ariane Koch-Larrouy
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Editorial statement
This study shows that the fate of internal tide energy is not uniform but is dictated by interactions with mesoscale eddies features, affecting the intensity and distribution of energy flux. The study finds that the specific response of an internal tide—whether it propagates freely or deviates—is dually controlled by the internal tide vertical modal structure, and the ocean state it encounters together with its associated background conditions. In additions, it is also found that the redistribution of energy via intermodal transfers is governed by a hierarchy of synergistic interactions between the topographic features and the background flow of the ocean state.
This study shows that the fate of internal tide energy is not uniform but is dictated by...
Short summary
Our research investigates how large waves travel deep within the ocean. Using a detailed computer model, we show that when these deep waves meet giant ocean circulation, their path is dramatically changed. They can be bent off course, split apart, or stopped completely. An underwater mountain works with this circulation to transfer the wave energy between different ocean layers. Understanding this process is vital because it controls ocean mixing.
Our research investigates how large waves travel deep within the ocean. Using a detailed...