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} </math> as an infimum of the lengts of curves that satisfy [https://en.wikipedia.org/wiki/ Continuity equation], <math> </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], <math> \partial_{t}\mu+\nabla(v\mu)=0 </math>. | ||
== Statement of Theorem== | == Statement of Theorem== |
Revision as of 12:51, 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 ,