Mapping internal lee wave generation and dissipation in the deep South China sea

• Using spectral methods and advanced flow field data, we provide the first basin-scale estimation for lee wave generation in the South China Sea. • The Luzon Strait generates 19.7 GW of lee wave energy, with 1.3 GW of total energy flux in the South China Sea, 70% of which occurs in the deep basin. • The lee wave is modulated by seasonal signals from the LS and potentially contributes to deep mixing in the South China Sea. Abyssal mixing induced by internal wave breaking has been proposed as an essential process that maintains and modulates the deep cyclonic circulation and meridional overturning circulation in the South China Sea (SCS). Previous studies have primarily focused on internal tides, leaving limited exploration on internal lee waves and their roles in mixing the SCS. This study represents the first basin-scale estimation of the lee-wave energy flux from the geostrophic flow and exploration of lee-wave-induced mixing in the SCS. Utilizing an improved spectra method with the synthetic full-scaled bathymetry, lee wave generation is estimated employing Bell theory with the outputs from the China Sea Multi-Scale Ocean Modeling System. The Luzon Strait (LS) features the strongest lee wave generation, reaching up to 19.7 GW. In the SCS interior, the total energy flux is estimated at 1.3 GW, with 70% occurring in the deep basin. In the basin area, energy flux from the mean flow surpasses that from eddy flow, whereas in the marginal area, the dominant energy flux is from eddy flow. This study reveals seasonal variation in lee wave generation, closely related to the seasonality of the deep-water overflow from the LS. The mixing driven by lee waves is found comparable with that driven by internal tides in the deep SCS basin. This study emphasizes the potentially significant lee wave energy and induced mixing in the deep SCS basin, which should be well-mapped and parameterized in ocean models for a better characterization of multiscale dynamics and energetics in the SCS.

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Publication Details

Journal
Progress In Oceanography
Published
2025-04-19
DOI
https://doi.org/10.1016/j.pocean.2025.103474
Primary Topic
Oceanographic and Atmospheric Processes
Type
article
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article

Mapping internal lee wave generation and dissipation in the deep South China sea

Peiwen Zhang, Jianping Gan, Zhenhua Xu, Ji Li et al.
Progress In Oceanography
Oceanographic and Atmospheric Processes
article

Mapping internal lee wave generation and dissipation in the deep South China sea

Peiwen Zhang, Jianping Gan, Zhenhua Xu, Ji Li, Jia You
article en

Abstract

• Using spectral methods and advanced flow field data, we provide the first basin-scale estimation for lee wave generation in the South China Sea. • The Luzon Strait generates 19.7 GW of lee wave energy, with 1.3 GW of total energy flux in the South China Sea, 70% of which occurs in the deep basin. • The lee wave is modulated by seasonal signals from the LS and potentially contributes to deep mixing in the South China Sea. Abyssal mixing induced by internal wave breaking has been proposed as an essential process that maintains and modulates the deep cyclonic circulation and meridional overturning circulation in the South China Sea (SCS). Previous studies have primarily focused on internal tides, leaving limited exploration on internal lee waves and their roles in mixing the SCS. This study represents the first basin-scale estimation of the lee-wave energy flux from the geostrophic flow and exploration of lee-wave-induced mixing in the SCS. Utilizing an improved spectra method with the synthetic full-scaled bathymetry, lee wave generation is estimated employing Bell theory with the outputs from the China Sea Multi-Scale Ocean Modeling System. The Luzon Strait (LS) features the strongest lee wave generation, reaching up to 19.7 GW. In the SCS interior, the total energy flux is estimated at 1.3 GW, with 70% occurring in the deep basin. In the basin area, energy flux from the mean flow surpasses that from eddy flow, whereas in the marginal area, the dominant energy flux is from eddy flow. This study reveals seasonal variation in lee wave generation, closely related to the seasonality of the deep-water overflow from the LS. The mixing driven by lee waves is found comparable with that driven by internal tides in the deep SCS basin. This study emphasizes the potentially significant lee wave energy and induced mixing in the deep SCS basin, which should be well-mapped and parameterized in ocean models for a better characterization of multiscale dynamics and energetics in the SCS.

Progress In OceanographyVol. 235
Ocean Park Conservation Foundation (HK), Institute of Oceanology (CN), Qingdao National Laboratory for Marine Science and Technology (CN), OceanX Technology (China) (CN), University of Chinese Academy of Sciences (CN)
Life below water
Openalex Percentile: Top 89%
Oceanographic and Atmospheric Processes
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