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February 20, 2026Physics of Fluids4 citationsOpen Access

Planing hull dynamics in water waves: Physical insights from nonlinear strip theory models and fully nonlinear computational fluid dynamics simulations

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STSasan TavakoliRBRasul Niazmand BilandiFRFatemeh Roshan

Key Points

  • The research aims to investigate the dynamics of planing hulls in nonlinear water wave conditions using advanced modeling techniques.
  • Developed two-dimensional plus time (2D+t) nonlinear strip theory models.
  • Utilized a fully nonlinear computational fluid dynamics (CFD) model with a Reynolds-averaged Navier-Stokes solver.
  • Analyzed the effects of wave conditions on heave and pitch motions of planing hulls.
  • Heave motion second harmonics increase with wave steepness, while pitch motion may decrease.
  • Higher harmonics arise from intermittency in wetted surfaces and wave scattering.
  • CFD simulations reveal phenomena like water detachment and subsurface vorticity that 2D+t models cannot capture.

Abstract

The dynamic motions of planing hulls in water waves represent a well-known example of a strongly nonlinear fluid–structure interaction problem, where wave-induced motions are governed by intermittent contact, spray formation, transom wake flow, and higher-harmonic responses. In this study, nonlinear strip theory models, namely, two-dimensional plus time (2D+t) models, extending classical strip theory formulations by incorporating nonlinear wave kinematics and an improved analytical water-entry solution that captures nonlinearity, are developed alongside a fully nonlinear computational fluid dynamics (CFD) model based on a Reynolds–averaged Navier–Stokes solver. These models are employed to investigate the physics of nonlinear unsteady planing motions under different wave conditions. Results show that the second harmonic of the heave motion tends to increase with wave steepness, whereas that of the pitch motion may decrease due to the onset of airborne phases. The higher harmonics of heave and pitch in short waves are primarily caused by intermittent wetted-surface variations and wave scattering, the latter introducing irregularities in the response that are absent in the 2D+t model. At intermediate wavelengths, nonlinearities arise mainly from airborne motion and subsequent slamming impacts, while at long-wave conditions, additional effects, including water detachment and subsurface vorticity generation, contribute to the nonlinear response, phenomena captured only by the CFD simulations. Consequently, the response amplitude operators of heave and pitch are seen to increase with wave steepness in long-wave conditions when computed using the CFD model. This distinction highlights that, although the second-order and earlier 2D+t formulations remain valuable predictive tools, they cannot fully reproduce the nonlinear behavior observed in steep-wave regimes. Specifically, they can have application in the early-stage design, rapid parametric studies for physical studies, and long-duration simulations due to its low computational cost and clear physical interpretability.

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Cite This Study

Tavakoli et al. (2026) studied this question.

synapsesocial.com/papers/6997f9c9ad1d9b11b3452789https://doi.org/10.1063/5.0311446
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