Riemannian geometry · Definition
Diffeomorphic flow
Before you start you need to know
A diffeomorphic flow describes a continuous deformation of space through a family of smooth, invertible transformations indexed by time. It is the basis of LDDMM, where the deformation is generated by integrating a velocity field.
Definition
A diffeomorphic flow \(\varphi_t\) is a family of deformations parametrized by time \(t\), where at each instant the transformation remains invertible and smooth.
The basic properties are that \(\varphi_0=\operatorname{id}\), that each \(\varphi_t\) is bijective and smooth, and that its inverse is also smooth. These conditions let each point be followed forward and backward in time without the space tearing or folding.
Guide example: on \(\mathbb{R}\) with constant field \(v_t(x)=1\), the flow is \(\varphi_t(x)=x+t\). Every point moves at the same speed, so \(\varphi_t\) is a translation, a diffeomorphism with inverse \(x-t\).
Typical error: confusing the field \(v_t\) with the total displacement \(\varphi_t(x)-x\). The field is an instantaneous velocity; the displacement comes from integrating \(v_t\) over the whole time interval.
Think about it
Why must a diffeomorphic flow have an inverse at each instant?
Because each point can be traced back, so the deformation neither tears nor folds the space.
Exercises 11
- For a point \(x\), the flow equation is read as \(\dot{\varphi}_t(x)=v_t(\varphi_t(x))\). What does it describe?
- What role does \(\varphi_0=\operatorname{id}\) play in a flow?
- If two flows have the same final map but travel different paths, what can vary?
- Which hypothesis on \(v_t\) helps the flow equation have a smooth, well-determined trajectory?
- Which description is compatible with a diffeomorphic flow \(\{\varphi_t\}\)?
- What does it mean for \(\varphi_t\) to be a diffeomorphism?
- What is the field \(v_t\) in LDDMM?
- What does it mean for the flow to be parametrized by \(t\in[0,1]\)?
- What does the final map \(\varphi_1\) do in LDDMM?
- If the field \(v_t\) is identically zero for all \(t\), what happens to the flow \(\varphi_t\)?
- Let \(v_t(x)=2x\) on \(\mathbb{R}\) with \(\varphi_0=\operatorname{id}\). What is \(\varphi_1\circ\varphi_{1/2}^{-1}(3)\)?
What comes next
References
- M. Faisal Beg, Michael I. Miller, Alain Trouvé, Laurent Younes, Computing Large Deformation Metric Mappings via Geodesic Flows of Diffeomorphisms, 2005.