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A Physics-preserved Transfer Learning Method for Differential Equations

NeurIPS 2025 · Probabilistic and scientific modeling › Differential equations and PDEs · approach: Neural operators for general geometries · 0 citations (OpenAlex)

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Proposes Physics-preserved Optimal Tensor Transport (POTT), a min-max optimal-transport-based transfer learning method that maps source product distributions toward the target and adds a physics regularizer, to correct distribution and operator bias for neural operators on DEs.

Problem

Neural operators for differential equations suffer performance degradation under domain shift (distribution bias and operator bias) between source and target, and existing transfer learning methods either lack generality or fail to preserve physics when the target has few samples.

Approach

Model the ideal transfer map as a physics-regularized optimal tensor transport map between source and target product distributions; the pushforward of source data is used together with few target samples to fine-tune the neural operator, with a dual (Lagrangian) min-max training scheme and a physical regularizer (or marginal-relation regularizer when no physics prior is available).

Key results

Measured effects reported in the paper

What was changedWhereMeasuredEffect
use POTT instead of finetuningFNO transfer on Burgers' equation · Burgers' equation average, 50 target samplesrMSE: 0.1532 -> 0.1242Helped
use POTT instead of finetuningFNO transfer on Burgers' equation · Burgers' equation average, 100 target samplesrMSE: 0.0977 -> 0.0809Helped
use POTT instead of CODDeepONet transfer on Darcy flow · Darcy flow average, 50 target samplesrMSE: 0.2444 -> 0.2095Helped
use POTT instead of DARE-GRAMDeepONet transfer on Darcy flow · Darcy flow average, 100 target samplesrMSE: 0.1696 -> 0.1479Helped
use POTT instead of CODDeepONet transfer on Advection equation · Advection equation average, 50 target samplesrMSE: 0.1458 -> 0.1032Helped
use POTT instead of CODDeepONet transfer on Advection equation · Advection equation average, 100 target samplesrMSE: 0.0516 -> 0.0504Helped
use POTT instead of finetuningClimODE climate forecasting · ERA5 global forecasting, t2m, 6-hour leadlatitude-weighted RMSE: 3.43 ± 0.24 -> 2.65 ± 0.2Helped
use POTT instead of finetuningClimODE climate forecasting · ERA5 global forecasting, t2m, 36-hour leadlatitude-weighted RMSE: 3.86 ± 0.27 -> 3.13 ± 0.28Helped
add physical regularization to OTT (ablation)POTT on Darcy flow · D1→D2physics preservationHelped

Surprising findings

Limitations

Experimental setup

Datasets: Burgers' equation simulations Advection equation simulations Darcy flow simulations ERA5 (WeatherBench)

Benchmarks: Burgers' equation Advection equation Darcy flow ERA5 climate forecasting (WeatherBench)

Metrics: relative MSE (rMSE) latitude-weighted RMSE

Baselines: Src+Tgt Finetuning TL-DeepONet DARE-GRAM COD ClimaX

Builds on: Optimal transport (Monge/Kantorovich) neural optimal transport FNO DeepONet ClimODE

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