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

NeurIPS 2026 · Label-efficient and robust learning › Recognition and long-tail · approach: Prototype and concept dictionary models · 0 citations (OpenAlex)

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Shows that input-noise perturbations displace (rather than amplitude-perturb) gradient attributions in autoregressive weather forecasters and proposes WassersteinGrad, which aggregates perturbed attribution maps via an entropic Wasserstein barycenter instead of SmoothGrad's pointwise average.

Problem

Gradient-smoothing attribution methods like SmoothGrad average pointwise over noisy inputs, which blurs spatially misaligned attributions when explaining predictions of dynamic physical fields such as autoregressive weather forecasts.

Approach

Treat each perturbed attribution map as a spatial probability measure and aggregate them via an entropic (Sinkhorn) Wasserstein barycenter, which preserves geometric structure, optionally used as a spatial mask on the base gradient (WG-Bary x Grad).

Key results

Surprising findings

Limitations

Experimental setup

Datasets: TITAN

Benchmarks: TITAN

Metrics: Gini sparsity ROAD faithfulness LLE l2 LLE cosine centroid displacement

Baselines: BaseGrad SmoothGrad VarGrad IntegratedGrad

Builds on: SmoothGrad Wasserstein barycenter Sinkhorn iterations ROAD UNetRPP

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