Explanation of Dynamic Physical Field Predictions using WassersteinGrad: Application to Autoregressive Weather Forecasting

📅 2026-04-24
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🤖 AI Summary
Existing gradient-based attribution methods suffer from blurred attribution maps in dynamic physical fields—such as numerical weather prediction—due to geometric displacements, undermining their reliability for interpretation. This work proposes WassersteinGrad, an attribution aggregation framework grounded in entropy-regularized Wasserstein barycenters, which aligns attribution maps generated from multiple perturbations via optimal transport, thereby overcoming the limitations of conventional pointwise averaging. WassersteinGrad reveals, for the first time, that attribution discrepancies primarily stem from geometric shifts rather than amplitude noise, enabling the construction of geometrically consistent attribution consensus. Evaluated on regional meteorological data using an autoregressive neural weather forecasting model validated by meteorologists, WassersteinGrad consistently outperforms existing gradient-based baselines in both single-step and multi-step forecasts, yielding significantly sharper and more stable explanations.

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📝 Abstract
As the demand to integrate Artificial Intelligence into high-stakes environments continues to grow, explaining the reasoning behind neural-network predictions has shifted from a theoretical curiosity to a strict operational requirement. Our work is motivated by the explanations of autoregressive neural predictions on dynamic physical fields, as in weather forecasting. Gradient-based feature attribution methods are widely used to explain the predictions on such data, in particular due to their scalability to high-dimensional inputs. It is also interesting to remark that gradient-based techniques such as SmoothGrad are now standard on images to robustify the explanations using pointwise averages of the attribution maps obtained from several noised inputs. Our goal is to efficiently adapt this aggregation strategy to dynamic physical fields. To do so, our first contribution is to identify a fundamental failure mode when averaging perturbed attribution maps on dynamic physical fields: stochastic input perturbations do not induce stationary amplitude noise in attribution maps, but instead cause a geometric displacement of the attributions. Consequently, pointwise averaging blurs these spatially misaligned features. To tackle this issue, we introduce WassersteinGrad, which extracts a geometric consensus of perturbed attribution maps by computing their entropic Wasserstein barycenter. The results, obtained on regional weather data and a meteorologist-validated neural model, demonstrate promising explainability properties of WassersteinGrad over gradient-based baselines across both single-step and autoregressive forecasting settings.
Problem

Research questions and friction points this paper is trying to address.

dynamic physical fields
attribution maps
geometric displacement
feature attribution
autoregressive forecasting
Innovation

Methods, ideas, or system contributions that make the work stand out.

WassersteinGrad
attribution map alignment
dynamic physical fields
autoregressive forecasting
explainable AI
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