

FOLLOWUS
1.School of Atmospheric Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China
2.School of Marine Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China
3.Southern Ocean Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519000, China
4.School of Artificial Intelligence, Nanjing University of Information Science and Technology, Nanjing 210044, China
cmdong@nuist.edu.cn
Received:18 December 2024,
Accepted:24 January 2025,
Online First:21 March 2025,
Published:01 January 2026
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HAN Lei,DONG Changming,LIU Yuli,et al.Application of physics-informed neural networks in solving temperature diffusion equation of seawater[J].Journal of Oceanology and Limnology,2026,44(01):1-18.
HAN Lei,DONG Changming,LIU Yuli,et al.Application of physics-informed neural networks in solving temperature diffusion equation of seawater[J].Journal of Oceanology and Limnology,2026,44(01):1-18. DOI: 10.1007/s00343-025-4348-1.
Physics-informed neural networks (PINNs)
as a novel artificial intelligence method for solving partial differential equations
are applicable to solve both forward and inverse problems. This study evaluates the performance of PINNs in solving the temperature diffusion equation of the seawater across six scenarios
including forward and inverse problems under three different boundary conditions. Results demonstrate that PINNs achieved consistently higher accuracy with the Dirichlet and Neumann boundary conditions compared to the Robin boundary condition for both forward and inverse problems. Inaccurate weighting of terms in the loss function can reduce model accuracy. Additionally
the sensitivity of model performance to the positioning of sampling points varied between different boundary conditions. In particular
the model under the Dirichlet boundary condition exhibited superior robustness to variations in point positions during the solutions of inverse problems. In contrast
for the Neumann and Robin boundary conditions
accuracy declines when points were sampled from identical positions or at the same time. Subsequently
the Argo observations were used to reconstruct the vertical diffusion of seawater temperature in the north-central Pacific for the applicability of PINNs in the real ocean. The PINNs successfully captured the vertical diffusion characteristics of seawater temperature
reflected the seasonal changes of vertical temperature under different topographic conditions
and revealed the influence of topography on the temperature diffusion coefficient. The PINNs were proved effective in solving the temperature diffusion equation of seawater with limited data
providing a promising technique for simulating or predicting ocean phenomena using sparse observations.
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