2020
DOI: 10.1007/s00211-020-01153-9
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A variational finite volume scheme for Wasserstein gradient flows

Abstract: We propose a variational finite volume scheme to approximate the solutions to Wasserstein gradient flows. The time discretization is based on an implicit linearization of the Wasserstein distance expressed thanks to Benamou-Brenier formula, whereas space discretization relies on upstream mobility two-point flux approximation finite volumes. The scheme is based on a first discretize then optimize approach in order to preserve the variational structure of the continuous model at the discrete level. It can be app… Show more

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Cited by 20 publications
(20 citation statements)
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“…where ν K i ,K j is the unit normal to K i pointing from K i to K j . We refer to the recent work [9] for a variational interpretation of the upwind scheme, which is close to that we propose for the more general equation (1.7). Earlier results in this direction are contained in [21,38].…”
Section: Relation To the Numerical Finite-volume Upwind Schemesupporting
confidence: 55%
“…where ν K i ,K j is the unit normal to K i pointing from K i to K j . We refer to the recent work [9] for a variational interpretation of the upwind scheme, which is close to that we propose for the more general equation (1.7). Earlier results in this direction are contained in [21,38].…”
Section: Relation To the Numerical Finite-volume Upwind Schemesupporting
confidence: 55%
“…In this case, the Monge-Kantorovich optimal transport cost T (µ, ν) is defined by (4) T (µ, ν) = inf π∈Π(µ,ν)…”
Section: Preliminaries and Motivationmentioning
confidence: 99%
“…The weighted negative homogeneous Sobolev norm has also been considered in connection to maximum mean discrepancy (MMD) which is a technique that can be used to compute a distance between point clouds, and has many applications in machine learning, see [1,19,20]. Authors have also considered this connection in papers focused on computing the W 2 metric, see [4,9,14]. Moreover, the negative homogeneous Sobolev norm has been considered in several applications to seismic image and image processing, see [8,10,31].…”
mentioning
confidence: 99%
“…In particular, the continuity equation is discretized on the fine grid whereas the Hamilton-Jacobi equation on the coarse one. Using a discretization that preserves the monotonocity of the discrete Hamilton-Jacobi operator it is possible to show that the value zero for λ is optimal (see [8] for a problem closely related to 2.6), i.e. the discrete Hamilton-Jacobi equation can be saturated.…”
Section: 2mentioning
confidence: 99%