Geodesics and generalized geodesics: Difference between revisions

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== Introduction ==
== Introduction ==


There are many ways that we can describe [https://en.wikipedia.org/wiki/ Wasserstein metric]. One of them is to characterize absolutely continuos curves (AC)(p.188<ref name=Santambrogio />) and provide a dynamic formulation of the special case <math> W_{2}^{2} </math> Namely, it is possible to see <math> W_{2}^{2}(\mu, \nu) </math> as an infimum of the lengts of curves that satisfy [https://en.wikipedia.org/wiki/ Continuity equation] (<math> \partial_{t}\mu+\nabla(v\mu)=0 </math>).
There are many ways that we can describe [https://en.wikipedia.org/wiki/ Wasserstein metric]. One of them is to characterize absolutely continuos curves (AC)(p.188<ref name=Santambrogio />) and provide a dynamic formulation of the special case <math> W_{2}^{2} </math> Namely, it is possible to see <math> W_{2}^{2}(\mu, \nu) </math> as an infimum of the lengts of curves that satisfy [https://en.wikipedia.org/wiki/ Continuity equation] <br> (<math> \partial_{t}\mu+\nabla(v\mu)=0 </math>).


== Statement of Theorem==
== Statement of Theorem==

Revision as of 12:55, 8 June 2020

Introduction

There are many ways that we can describe Wasserstein metric. One of them is to characterize absolutely continuos curves (AC)(p.188[1]) and provide a dynamic formulation of the special case Namely, it is possible to see as an infimum of the lengts of curves that satisfy Continuity equation
().

Statement of Theorem

Theorem.(Benamow-Brenier)[1] Let ,

Generalization

References