What error bounds exist for physics-informed neural network approximations?

Physics-informed neural networks approximate solutions of partial differential equations by minimizing a loss that combines PDE residuals and data misfit. The foundational formulation by Maziar Raissi, Paris Perdikaris University of Pennsylvania, and George Em Karniadakis Brown University in Journal of Computational Physics established the empirical success and prompted rigorous follow-up work on error characterization. Contemporary analyses frame error control in terms of error decomposition into distinct, quantifiable pieces.

Sources of error and theoretical structure

The approximation error breaks down into approximation error, optimization error, and generalization error. Approximation error expresses how well the chosen neural network class can represent the true solution in relevant norms such as L2 or Sobolev H1. Optimization error measures the gap between the minimized loss and the global minimum; nonconvex training can leave a nonzero residual. Generalization error captures the difference between empirical residuals computed at collocation points and the continuous-domain residual. Rigorous results show that, under standard PDE well-posedness assumptions, an upper bound on the solution error can be written as a constant times the sum of the PDE residual norm and boundary/data residuals, provided the network approximates derivatives accurately. The constant reflects PDE stability or coercivity and therefore depends on the equation type and coefficients.

Relevance, causes, and consequences

The practical consequence is that small PINN training residuals do not universally guarantee small solution error. For elliptic and coercive problems the stability constant is moderate, so residual control yields reliable error bounds. For hyperbolic or advection-dominated equations the stability constant can be large and small residuals may be amplified, producing poor numerical accuracy. Heterogeneous coefficients or complex territorial domains typical in geophysics and environmental modeling increase sensitivity and require tailored collocation strategies and stronger approximation spaces. Human and cultural factors enter through model choice and data quality: sparse or biased observational data used in the loss can degrade generalization, affecting trustworthiness in engineering or policy contexts.

Mathematical research continues to refine these bounds by specifying function-space assumptions, showing explicit dependence on network width and depth, and quantifying sampling error from collocation. Nuance matters: theoretical guarantees require assumptions often stricter than those in applied settings, so practitioners should combine analytical bounds, adaptive sampling, and validation against independent measurements to assess PINN accuracy.