<p>Physics-informed neural networks (PINNs) are applied to solve forced-KdV (fKdV) equations and to assess their capability for nonlinear wave dynamics under external forcing. We first validate the solver in analytically tractable forced-KdV benchmarks with periodic and exponential time-dependent forcing, demonstrating accurate reproduction of two-soliton interactions. Robustness is sensitive to forcing characteristics and to the coupled choice of loss weights and sampling density: more rapidly varying forcing and imbalanced weighting increase across-seed variability in the attained relative <InlineEquation ID="IEq1"> <EquationSource Format="TEX">\(\:{L}^{2}\)</EquationSource> </InlineEquation> error, consistent with known PINN optimization pathologies. We then demonstrate an event-based ocean application for internal solitary wave (ISW) variability near Dongsha Atoll using a reduced-order, one-dimensional fKdV representation. A spatiotemporal forcing proxy <InlineEquation ID="IEq2"> <EquationSource Format="TEX">\(\:F\left(x,\:t\right)\)</EquationSource> </InlineEquation> is constructed from TPXO <InlineEquation ID="IEq3"> <EquationSource Format="TEX">\(\:{M}_{2}\)</EquationSource> </InlineEquation> barotropic currents and the along-transect bathymetric slope; a ridge-based partitioning provides a consistent ridge-to-site linkage across events. A forced–free ablation of the propagation-stage forcing shows that West-Ridge corridor forcing primarily modulates site waveform morphology—systematically reducing peak magnitude while broadening the main pulse—without qualitatively altering the westward propagation pathway. These results suggest that PINNs provide a practical framework for investigating fKdV dynamics in both controlled benchmarks and mechanism-oriented ocean case studies.</p>

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Solving forced KdV equation using physics-informed neural networks

  • Lei Han,
  • Changming Dong,
  • Wanchen Cui,
  • Huarong Xie,
  • Weijun Zhu

摘要

Physics-informed neural networks (PINNs) are applied to solve forced-KdV (fKdV) equations and to assess their capability for nonlinear wave dynamics under external forcing. We first validate the solver in analytically tractable forced-KdV benchmarks with periodic and exponential time-dependent forcing, demonstrating accurate reproduction of two-soliton interactions. Robustness is sensitive to forcing characteristics and to the coupled choice of loss weights and sampling density: more rapidly varying forcing and imbalanced weighting increase across-seed variability in the attained relative \(\:{L}^{2}\) error, consistent with known PINN optimization pathologies. We then demonstrate an event-based ocean application for internal solitary wave (ISW) variability near Dongsha Atoll using a reduced-order, one-dimensional fKdV representation. A spatiotemporal forcing proxy \(\:F\left(x,\:t\right)\) is constructed from TPXO \(\:{M}_{2}\) barotropic currents and the along-transect bathymetric slope; a ridge-based partitioning provides a consistent ridge-to-site linkage across events. A forced–free ablation of the propagation-stage forcing shows that West-Ridge corridor forcing primarily modulates site waveform morphology—systematically reducing peak magnitude while broadening the main pulse—without qualitatively altering the westward propagation pathway. These results suggest that PINNs provide a practical framework for investigating fKdV dynamics in both controlled benchmarks and mechanism-oriented ocean case studies.