High-level Green–Naghdi model for internal solitary waves generated by time-varying boundaries

This paper extends the two-layer high-level Green–Naghdi (HLGN) internal-wave model to study boundary time-varying problems, involving moving bottom or surface disturbances. The equations for the two-layer HLGN model with time-varying boundaries are presented, accompanied by a time-domain algorithm for solving these equations. The wave profiles predicted by the HLGN model for internal waves generated by boundary disturbances, whether occurring at the bottom or at the surface, show excellent agreement with results obtained by the fully nonlinear potential-flow (FNPF) solution. For internal waves generated by a surface moving disturbance, the results obtained by the HLGN model show good agreement with the experimental observations and the FNPF solution, including the relationships between the disturbance speed and the resulting wave amplitude and phase speed. Furthermore, the HLGN model is applied to analyse the evolution of the wave profiles and speed generated by the surface disturbance with different moving speeds. In addition, the extended HLGN model incorporates background linear shear currents to examine internal waves generated by a moving bottom disturbance with a linear shear current. The results reveal that background vorticity exerts a pronounced modulation effect on the wave profile and velocity field. Counter-flow narrows the waves and increases their phase speed, whereas co-flow broadens the waves and enhances their amplitude.

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Publication Details

Journal
Journal of Fluid Mechanics
Published
2026-01-13
DOI
https://doi.org/10.1017/jfm.2025.10996
Primary Topic
Oceanographic and Atmospheric Processes
Type
article
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article

High-level Green–Naghdi model for internal solitary waves generated by time-varying boundaries

Z. Wang, Natalya Shmakova, А. А. Чесноков, Binbin Zhao et al.
Journal of Fluid Mechanics
Oceanographic and Atmospheric Processes
article

High-level Green–Naghdi model for internal solitary waves generated by time-varying boundaries

Z. Wang, Natalya Shmakova, А. А. Чесноков, Binbin Zhao, Wenyang Duan, Tianyu Zhang, R. Cengiz Ertekin, Masoud H. Davoodi
article en

Abstract

This paper extends the two-layer high-level Green–Naghdi (HLGN) internal-wave model to study boundary time-varying problems, involving moving bottom or surface disturbances. The equations for the two-layer HLGN model with time-varying boundaries are presented, accompanied by a time-domain algorithm for solving these equations. The wave profiles predicted by the HLGN model for internal waves generated by boundary disturbances, whether occurring at the bottom or at the surface, show excellent agreement with results obtained by the fully nonlinear potential-flow (FNPF) solution. For internal waves generated by a surface moving disturbance, the results obtained by the HLGN model show good agreement with the experimental observations and the FNPF solution, including the relationships between the disturbance speed and the resulting wave amplitude and phase speed. Furthermore, the HLGN model is applied to analyse the evolution of the wave profiles and speed generated by the surface disturbance with different moving speeds. In addition, the extended HLGN model incorporates background linear shear currents to examine internal waves generated by a moving bottom disturbance with a linear shear current. The results reveal that background vorticity exerts a pronounced modulation effect on the wave profile and velocity field. Counter-flow narrows the waves and increases their phase speed, whereas co-flow broadens the waves and enhances their amplitude.

Journal of Fluid MechanicsVol. 1027
Harbin Engineering University (CN), National University of Defense Technology (CN), University of Hawaii–West Oahu (US), Lavrentyev Institute of Hydrodynamics (RU)
Openalex Percentile: Top 89%
Oceanographic and Atmospheric Processes
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High-level Green–Naghdi model for internal solitary waves generated by time-varying boundaries — Z. Wang, Natalya Shmakova, et al. · Journal of Fluid Mechanics (2026) | TGRS Research Map | TGRS