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Surface geodesic flow, index form, and transport primitive

Statement

Let (M,g) be a compact, connected, nonempty, oriented smooth Riemannian surface with smooth strictly convex boundary, no conjugate points, and nontrapping geodesic flow. Let SM={(x,v):x∈M, v∈TxM, gx(v,v)=1}, and let φt denote its unit-speed geodesic flow up to boundary exit. For w∈C∞(SM) define the geodesic vector field by Xw=ddt∣0w(φt(x,v)). Define the vertical vector field by Vw(x,v)=ddθ∣0w(x,cos⁡θ v+sin⁡θ v⊥), where v⊥ is the positive 90-degree rotation of v, and put X⊥=[X,V]. The Liouville measure is dΣ=dVg(x) dSx(v), with induced boundary measure dΣ∂=dS∂M(x) dSx(v); write μ(x,v)=gx(v,νin(x)) on ∂+SM.

In a positive orthonormal frame e1,e2, define K(x)=g(R(e1,e2)e2,e1); this scalar is independent of the frame. For a positive-length unit-speed geodesic γ:[0,L]→M and a smooth normal field Y with Y(0)=Y(L)=0, define the index form

Iγ(Y,Y)=∫0L(∣DtY∣g2−g(R(Y,γ˙)γ˙,Y))dt.

Then dΣ is preserved by φt, and the commutators are [X,V]=X⊥, [V,X⊥]=X, and [X,X⊥]=−KV. If a,b∈C∞(SM) and ab=0 on ∂SM, then each Y∈{X,V,X⊥} satisfies ∫SM(Ya)b dΣ=−∫SMa(Yb) dΣ. For every h∈C(SM), Santaló's formula is

∫SMh dΣ=∫∂+SMμ(x,v)∫0τ+(x,v)h(φt(x,v)) dt dΣ∂.

The index form is positive definite: Iγ(Y,Y)>0 whenever Y≢0. Finally, if f∈Cc∞(M∘) and I0f=0, then

uf(x,v)=∫0τ+(x,v)f(γx,v(t)) dt

extends to a smooth function compactly supported in SM∘, satisfies Xuf=−f, and vanishes on ∂SM. For smooth a,b with ab=0 on ∂SM, integration by parts holds for X and X⊥; for V, which is tangent to ∂SM, it holds for all smooth a,b.

Facts & Assumptions

Given: A compact, connected, nonempty oriented smooth Riemannian surface with smooth strictly convex boundary, no conjugate points, and nontrapping geodesic flow; a scalar f∈Cc∞(M∘) with I0f=0; and a smooth function h on SM.

[F1]

Simple surface and geodesic X-ray transform: simple means strict convexity, absence of Jacobi fields vanishing at two distinct parameters, and finite forward and backward exit times; I0f integrates the scalar pullback along unit-speed boundary-to-boundary geodesics.

[F2]

Riemannian volume density: in coordinates with metric matrix Gx, the base density is dVg=det⁡Gx ∣dx1⋯dxn∣.

[F3]

Fundamental theorem of riemannian geometry: a supplied smooth Riemannian metric, including one up to a smooth boundary, has a unique Levi-Civita connection; Levi civita connection states that this connection is metric-compatible and torsion-free.

[F4]

Local existence, uniqueness, and smooth dependence for manifold integral curves: every smooth local vector field has unique local integral curves depending smoothly on initial data.

[F5]

Jacobi field: along a geodesic, a Jacobi field satisfies Dt2J+R(J,γ˙)γ˙=0.

[F6]

Curvature of an affine connection: R(X,Y)Z=∇X∇YZ−∇Y∇XZ−∇[X,Y]Z; Riemann curvature four-tensor defines Rm⁡(X,Y,Z,W)=g(R(X,Y)Z,W), positive on the unit round sphere.

[F7]

Riemannian metric and riemannian manifold: g is positive definite; Riemannian speed and length: the length of a unit-speed curve on a time interval is the length of that interval; Riemannian distance on a connected manifold: dg is the infimum of lengths of piecewise C1 curves; Riemannian distance is a metric: dg is a finite metric; The riemannian distance topology is the manifold topology: its metric topology is the manifold topology; Length dominates endpoint distance: endpoint distance is at most curve length.

[F8]

The parametrized implicit function theorem with Ck regularity: if a Ck map F(z,t) vanishes at (z0,t0) and ∂tF(z0,t0)≠0, then near z0 its zero set near t0 is the graph of a unique Ck function t=T(z). If F is smooth, applying this for every finite k shows that T is smooth.

Proof

1.1F3F4given

In a boundary chart the metric coefficients are smooth up to the boundary, so its Levi-Civita Christoffel coefficients extend locally to smooth coefficients on an open chart. The geodesic equation is the smooth first-order system (x˙i,v˙k)=(vi,−Γijk(x)vivj) on the chart tangent coordinates.

1.2F2F3given

On an oriented coordinate patch choose a positive orthonormal frame e1,e2 and write ∇e1=ωe2, ∇e2=−ωe1. With v=cos⁡θ e1+sin⁡θ e2 and v⊥=−sin⁡θ e1+cos⁡θ e2, the fibre density is dθ and dΣ=dVg dθ. A change of positive orthonormal frame changes θ by a smooth rotation angle depending on x; its coordinate Jacobian is triangular with fibre derivative 1, so this density is independent of the frame.

2.1F3F4step 1.1

The local ODE result in [F4] gives unique geodesic arcs with smooth dependence on initial state. The coordinate equations agree on overlaps because they are the covariant equation Dtγ˙=0; metric compatibility gives ddtg(γ˙,γ˙)=2g(Dtγ˙,γ˙)=0. Thus the local arcs patch uniquely on their common intervals and unit-speed initial states remain in SM until exit.

2.2F2F3step 1.2algebra

The horizontal lifts are Hi=ei−ω(ei)V and X=cos⁡θ H1+sin⁡θ H2. At fixed θ, the base divergence of v is div⁡gv=ω(v⊥), while the vertical coefficient of X is −ω(v) and its θ-derivative is −ω(v⊥). Hence div⁡dΣX=0. Also div⁡dΣV=0 because V=∂θ, and div⁡dΣX⊥=0 because X⊥=[X,V] and div⁡[X,V]=X(div⁡V)−V(div⁡X). The local flow equation for the density is ddtφt∗dΣ=φt∗(div⁡dΣX dΣ)=0, so the geodesic flow preserves dΣ until boundary exit.

2.3F3F6step 1.2algebra

Write ωi=ω(ei). The curvature definition gives R(e1,e2)e1=dω(e1,e2)e2 and R(e1,e2)e2=−dω(e1,e2)e1, so dω=−K dVg for K=g(R(e1,e2)e2,e1). First-slot skewness follows from [F6]; last-slot skewness follows by applying metric compatibility in [F3] to g(R(A,B)C,D)+g(C,R(A,B)D). Under a positive rotation of (e1,e2), each alternating pair in g(R(e1,e2)e2,e1) is multiplied by the determinant 1, so K is frame-independent. Torsion-freeness gives [e1,e2]=−ω1e1−ω2e2 and direct expansion of Hi=ei−ωiV gives [H1,H2]=−ω1H1−ω2H2+KV. Put c=cos⁡θ, s=sin⁡θ, X=cH1+sH2, and X⊥=sH1−cH2. Since V(c)=−s and V(s)=c, the definitions give [X,V]=X⊥ and [V,X⊥]=X. In [X,X⊥], the horizontal-frame bracket contributes −[H1,H2]=ω1H1+ω2H2−KV; differentiating the coefficients c,s along Hi contributes −ω1H1−ω2H2, leaving [X,X⊥]=−KV.

3.1F1F3F4F7F8step 2.1

Let ρ be a boundary defining function, positive in M∘. At a boundary point, νout=−∇ρ/∣dρ∣g. For tangent w, differentiation gives Hess⁡ρ(w,w)=−∣dρ∣g g(∇wνout,w)<0. Along a geodesic tangent to the boundary, d2dt2ρ(γ(t))=Hess⁡ρ(γ˙,γ˙)<0, so the geodesic lies outside M on both sides near tangency. Therefore a geodesic arriving from the interior exits transversely. For an interior initial state z0, nontrapping gives a finite first exit time t0=τ+(z0). In a local chart of SM near z0, choose a boundary defining function ρ near the exit and extend the geodesic ODE locally across the boundary in a boundary chart. A finite composition of the local flows from [F4] gives the smooth map F(z,t)=ρ(φt(z)) near (z0,t0). Transversality gives F(z0,t0)=0 and ∂tF(z0,t0)=dργz0(t0)(γ˙z0(t0))≠0. For each finite k≥1, [F8] gives a local Ck root t=T(z); applying this for every k makes T smooth. For each ϵ>0 with ϵ<t0, the compact arc γz0([0,t0−ϵ]) and compact boundary are disjoint, so their positive distance in the metric topology [F7] keeps nearby arcs interior on that interval. Transversality gives a unique crossing near t0; shrinking the neighborhood therefore makes the IFT root the first exit for nearby interior states. Thus the exit time is smooth near every interior initial state.

3.2F2step 2.2algebra

For Y∈{X,V,X⊥}, the local density formula for divergence gives div⁡dΣ(abY)=(Ya)b+a(Yb) because div⁡dΣY=0. Integrating in coordinate charts and applying one-variable integration by parts gives the boundary flux term ∫∂SMab ιYdΣ. It vanishes for X and X⊥ when ab=0 on ∂SM; for V it vanishes for arbitrary a,b because V rotates only the fibre and is tangent to ∂SM. A finite chart cover and a partition of unity sum these local identities to yield the asserted global formulas.

3.3F1F3F4F5step 2.3

Fix a unit-speed segment γ:[0,L]→M. Since M is oriented, let Q be positive rotation by 90 degrees on each tangent plane. In any local positive orthonormal frame e1,e2=Qe1, metric compatibility gives ∇Ae1=ω(A)e2 and ∇Ae2=−ω(A)e1; for e1, (∇AQ)e1=∇Ae2−Q(ω(A)e2)=−ω(A)e1+ω(A)e1=0, and for e2, (∇AQ)e2=∇A(−e1)−Q(−ω(A)e1)=−ω(A)e2+ω(A)e2=0. Thus ∇Q=0 and n(t)=Qγ˙(t) is a parallel unit normal along the whole segment. By [F5], the scalar coefficient j in the Jacobi field jn solves j′′+K(γ(t))j=0. Let j(0)=0, j′(0)=1. This solution is positive for 0<t≤L: it is positive near 0, and a later zero would give a nonzero Jacobi field vanishing at both endpoints of a positive-length subsegment, contradicting [F1].

3.4F1F4F7givenstep 2.1choose

If supp⁡f=∅, then f=0 and uf=0, so the transport claim is immediate; assume henceforth that the support is nonempty. The nontrapping hypothesis and existence of an interior unit geodesic from step 2.1 imply ∂M≠∅. The unit circle bundle SM is compact: cover compact M by finitely many smaller coordinate neighborhoods with closures inside charts carrying smooth orthonormal frames; each part of SM over such a closure is homeomorphic to the product of that compact closure with S1, so finitely many compact sets cover SM. Define D=min⁡{dg(x,y):x∈∂M, y∈supp⁡f}. These disjoint sets are compact in the metric topology by [F7], so the minimum is attained and is positive because dg is a metric. For a subset A, write dg(x,A)=inf⁡a∈Adg(x,a).

4.1F1step 3.1step 2.2step 3.2

Every interior state has a unique backward geodesic to its first boundary hit, and transversality in step 3.1 puts that state in ∂+SM. Thus (z,t)↦φt(z) maps z∈∂+SM, 0<t<τ+(z) bijectively onto SM∘. In a boundary coordinate and the fibre angle, adjoining the flow-time column to the two boundary-state tangent columns gives the volume determinant ∣g(v,νin)∣=μ(z) at t=0: the fibre column supplies dSx(v), the boundary column supplies dS∂M(x), and the component of the flow column normal to ∂M is g(v,νin). Since the flow preserves dΣ by step 2.2, that determinant is constant along each flow line. The change-of-variables formula therefore gives Santaló's identity; tangential boundary states form a measure-zero set and contribute nothing.

4.2F1F5step 3.3algebra

Write an endpoint-zero normal field as Y=yn and set q=y/j on (0,L]. Since y(0)=j(0)=0 and j′(0)=1, both functions factor smoothly as t times a smooth function and q extends smoothly to 0; also q(L)=0. Expanding y=jq and using j′′+Kj=0 gives (y′)2−Ky2=j2(q′)2+(jj′q2)′. The boundary term jj′q2 vanishes at 0 because j(0)=0 and at L because q(L)=0. Consequently Iγ(Y,Y)=∫0Lj2(q′)2dt≥0, with equality only if q is constant and hence zero from q(L)=0. Thus the index form is positive definite.

4.3F1F4F7step 3.1step 3.4choosealgebra

If dg(x,∂M)<D/4, the triangle inequality gives dg(x,supp⁡f)>3D/4; hence a unit-speed curve from x cannot reach the support before time D/2, since its length equals elapsed time and endpoint distance is at most length. Fix any z=(x,v)∈∂SM and a boundary chart with defining coordinate ρ positive inside. If v is transverse, choose the one of v,−v pointing outward; after shrinking a neighborhood, ρ′(t)<−c<0 up to some t0<D/2, and nearby interior states have ρ(0)<ct0, so this ray exits by t0. If v is tangent, step 3.1 gives ρ′′(0)<0. Choose t0<D/2 small enough to remain in the chart; after shrinking a neighborhood, ρ′′(t)<−c<0 for 0≤t≤t0, while ρ(0)<ct02/8 and ∣ρ′(0)∣<ct0/4. Taylor's formula yields ρ(t0)≤ρ(0)+t0ρ′(0)−ct02/2<0, so the geodesic has exited by t0. In either case there is a neighborhood of z and one fixed orientation whose forward ray exits before reaching supp⁡f. Shrink each such neighborhood so every state in it also has base point at distance less than D/4 from ∂M. Compactness of ∂SM from step 3.4 gives a finite subcover, whose union contains an open neighborhood of ∂SM with the same property.

5.1F1F4F7F8step 3.1step 3.4step 4.3algebra∎

At every non-tangent boundary state, the relevant first boundary hit is transverse: it is the time-zero hit for an outgoing state and the finite future exit for an incoming state. In local coordinates for the extension across the boundary, choose a boundary defining function near the hit and extend the geodesic ODE. The finite-time smooth dependence established in step 3.1 and [F8] give a smooth local root of F(z,t)=ρ(φt(z))=0. For an outgoing state the nonzero outward derivative makes this root the first exit for nearby interior states. For an incoming state the initial inward derivative gives a short interior segment; each compact middle segment before the final hit has positive distance from ∂M by [F7], and the final transverse crossing is the IFT root, so it remains the first exit for nearby states. Therefore the integration endpoint and integral defining uf depend smoothly on the initial state near every non-tangent boundary state. In the neighborhood from step 4.3, one of uf(x,v) and uf(x,−v) is zero by the support separation. Their sum is the full boundary-to-boundary integral of f along the same unoriented geodesic, which is I0f=0 by [F1]; therefore both vanish throughout that neighborhood. Thus uf is zero near ∂SM, removing the glancing singularity and making it smooth with compact support in SM∘, since SM is compact by step 3.4. Along the flow, uf(φs(x,v))=∫sτ+(x,v)f(φt(x,v))dt, so differentiation gives Xuf=−f. The incoming boundary value is I0f=0 and the outgoing value is zero because its future exit time is zero.

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