Oceanic internal solitary waves (ISWs) produce strong nonlinear variations in density stratification and flow fields, posing considerable risks to submerged body navigation. In this study, high-resolution ISW data in the South China Sea were simulated using the Massachusetts Institute of Technology General Circulation Model (MITgcm), and a continuous three-dimensional visualization of ISWs was developed based on isopycnal depth extraction. A multi-degree-of-freedom dynamic model was employed to investigate the motion responses of a submerged body under different initial depths, propeller rotational speeds, and ballast-water discharge durations. For a high-amplitude ISW with an amplitude of 70 m, wavelength of 2000 m, and phase speed of −1.5 m/s, the maximum vertical displacement reached approximately −80 m at an initial depth of −150 m. At −250 m, the maximum pitch and yaw amplitudes were about 40° and 57°. Coordinated regulation of propeller speed and ballast-water discharge achieved a depth correction of 30.9 m and gradually restored stability after leaving the ISW environment. Furthermore, a fluid–structure coupled visualization framework with immersive human–computer interaction was established using a Logitech X56 controller and a VIVE Pro Eye headset.
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Liu et al. (2026) studied this question.
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