Geodesics and generalized geodesics

Introduction

There are many ways that we can describe Wasserstein metric. One of them is to characterize absolutely continuos curves (AC)(p.188) and provide a dynamic formulation of the special case $W_{2}^{2}$ Namely, it is possible to see $W_{2}^{2}(\mu ,\nu )$ as an infimum of the lengts of curves that satisfy Continuity equation
($\partial _{t}\mu +\nabla (v\mu )=0$).

Geodesics

Definition. A metric space $(X,d)$ is called a length space if it holds

                    $d(x,y)=\inf\{L(\omega )|\omega \in AC(X),\omega (0)=x\quad \omega (1)=y\}.$

Definition. In a length space, a curve $l:[0,1]\rightarrow X$ is said to be constant speed geodesic between $\omega (0)$ and $\omega (1)$ in $X$ if it satisfies

                    $d(\omega (s),\omega (t))=|t-s|d(\omega (0),\omega (1))$ for all $t,s\in [0,1]$

Statement of Theorem

Now, we can rephrase Wasserstein metrics in dynamic language. In special case:

Theorem.(Benamow-Brenier) Let $\mu ,\nu \in P_{2}(R^{d})$. Then we have

      $W_{2}^{2}(\mu ,\nu )=\inf _{(\mu (t).\nu (t))}\{\int _{0}^{1}|v(,t)|_{L^{2}(\mu (t))}^{2}dt,\quad \partial _{t}\mu +\nabla (v\mu )=0,\mu (0)=\mu ,\mu (1)=\nu \}$

Generalization

It is possible to generalize the previous theorem and theory to $W_{p}$ metrics. More about that could be seen in the book .

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