Geodesics and generalized geodesics: Difference between revisions

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Constant speed geodesic ...  
Constant speed geodesic ...  


: '''Definition.''' In a length space, a curve <math> l:[0,1]\rigtharrow X </math> is said to be constant speed geodesic between <math> \omega(0)</math> and <math> \omega(1)</math> in <math> X </math> if it satisfies <br>
: '''Definition.''' In a length space, a curve <math> l:[0,1]\rigtharrow X </math> is said to be constant speed geodesic between <math> \omega(0)</math> and <math> \omega(1)</math> in <math> X </math> if it satisfies  


<math> d(\omega(s),\omega(t))=|t-s|d(\omega(0),\omega(1)) </math> for all <math> t,s \in [0,1]</math>
<math> d(\omega(s),\omega(t))=|t-s|d(\omega(0),\omega(1)) </math> for all <math> t,s \in [0,1]</math>

Revision as of 12:22, 11 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
().

Geodesics

Constant speed geodesic ...

Definition. In a length space, a curve Failed to parse (unknown function "\rigtharrow"): {\displaystyle l:[0,1]\rigtharrow X } is said to be constant speed geodesic between and in if it satisfies

for all

Statement of Theorem

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

Generalization

It is possible to generalize the previous theorem and theory to metrics. More about that could be seen in the book [2].

However, it is possible to generalize theorem for a different kind of geodesics [3].

References