NANAOCJul 21, 2017

Computation of Optimal Transport on Discrete Metric Measure Spaces

arXiv:1707.0685930 citations
AI Analysis

For researchers in optimal transport and graph-based machine learning, this provides a computationally tractable algorithm for discrete optimal transport with theoretical guarantees, though it is an incremental extension of existing continuous methods to graphs.

This paper develops a numerical algorithm for computing an analogue of the Wasserstein distance on graphs using a discrete Benamou-Brenier formulation with the logarithmic mean. The method achieves Γ-convergence of the time-discrete action functional and is validated on test cases, including a JKO scheme for entropy gradient flow that matches the Markov semigroup.

In this paper we investigate the numerical approximation of an analogue of the Wasserstein distance for optimal transport on graphs that is defined via a discrete modification of the Benamou--Brenier formula. This approach involves the logarithmic mean of measure densities on adjacent nodes of the graph. For this model a variational time discretization of the probability densities on graph nodes and the momenta on graph edges is proposed. A robust descent algorithm for the action functional is derived, which in particular uses a proximal splitting with an edgewise nonlinear projection on the convex subgraph of the logarithmic mean. Thereby, suitable chosen slack variables avoid a global coupling of probability densities on all graph nodes in the projection step. For the time discrete action functional $Γ$--convergence to the time continuous action is established. Numerical results for a selection of test cases show qualitative and quantitative properties of the optimal transport on graphs. Finally, we use our algorithm to implement a JKO scheme for the gradient flow of the entropy in the discrete transportation distance, which is known to coincide with the underlying Markov semigroup, and test our results against a classical backward Euler discretization of this discrete heat flow.

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