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Wasserstein Residuals: Learning Gradient Flows from Population Dynamics

About

Reconstructing population dynamics is a central problem in the physical and data sciences. Often, the dynamics are modeled as a Wasserstein gradient flow (WGF): a curve of distributions driven by an energy functional. Though there are multiple mathematical characterizations of a WGF, the dominant algorithmic approach relies on the Jordan--Kinderlehrer--Otto (JKO) scheme. JKO-based methods are inflexible to time discretisation and require solving costly optimal transport problems. We take a residual approach, enforcing the continuity equations via a non-negative loss function whose minimum is the WGF. Combined with a data-fitting divergence, this gives a single global objective. This perspective unifies several existing methods and leads to a new particle-based method, stitching, that is simulation-free and robust to large gaps between observations. We demonstrate that the stitching method achieves state-of-the-art performance across trajectory inference benchmarks. For code see github.com/BasisResearch/wasserstein-residuals.

Markus Heinonen, Yair Shenfeld, Ricardo Baptista, Daniel Waxman, Dmitry Batenkov, Tim Cooijmans, Eli Bingham• 2026

Related benchmarks

TaskDatasetResultRank
Single-cell trajectory inferenceEB (Embryoid Body) single-cell 5D (Full-data)
W1 Distance (t=1)0.44
14
Temporal interpolationEB single-cell dataset 5D (held-out t=1)
W20.84
10
Temporal interpolationEB single-cell dataset 5D (mean t=1 & t=3)
W2 Score0.88
10
Temporal interpolationEB single-cell dataset 5D (held-out t=3)
W20.92
10
Synthetic potential recoveryflowers potential unpaired regime
EMD0.31
3
Synthetic potential recoveryzigzag_ridge potential unpaired regime
EMD0.3
3
Synthetic potential recoverywatershed potential unpaired regime
EMD0.3
3
Synthetic potential recoveryishigami potential unpaired regime
EMD0.3
3
Synthetic potential recoveryfriedman potential unpaired regime
EMD0.31
3
Synthetic potential recoverywavy_plateau potential paired regime
EMD0.27
3
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