Stochastically perturbed geodesic °ows on Lie...

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Stochastically perturbed geodesic flows on Lie groups. Wenqing Hu. 1 1 School of Mathematics, University of Minnesota, Twin Cities.

Transcript of Stochastically perturbed geodesic °ows on Lie...

Page 1: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Stochastically perturbed geodesic flows onLie groups.

Wenqing Hu. 1

1School of Mathematics, University of Minnesota, Twin Cities.

Page 2: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

The classical Langevin equation.

I Random movement of a particle in a fluid due to collisionswith the molecules of the fluid. 1

Fig. 1: P. Langevin (1872–1946).

1Langevin, P. (1908). “Sur la theorie du mouvement brownien”. C. R. Acad.Sci. (Paris) 146 : pp. 530–533.

Page 3: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

The classical Langevin equation.

I Motion of a free particle :

qt = 0 .

I Hamiltonian equation :

{qt = pt ,pt = 0 .

I q0 = q0 ∈ Rn, q0 = p0 ∈ Rn.

Page 4: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 2: Motion of a free particle in Rn.

Page 5: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

The classical Langevin equation.

I Motion of a damped free particle :

qt = −λqt .

I Hamiltonian equation :

{qt = pt ,pt = −λpt .

I λ > 0, q0 = q0 ∈ Rn, q0 = p0 ∈ Rn.

Page 6: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 3: Motion of a damped free particle in Rn.

Page 7: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

The classical Langevin equation.

I Motion of a damped free particle subject to randomfluctuation :

qt = −λqt+εWt .

I Hamiltonian equation :

{qt = pt ,

pt = −λpt+εWt .

I λ > 0, ε > 0, q0 = q0 ∈ Rn, q0 = p0 ∈ Rn.

I Wt is a standard Brownian motion in Rn.

Page 8: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 4: Motion of a damped free particle subject to random fluctuationsin Rn.

Page 9: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

The classical Langevin equation.

I Random fluctuation : pt = −λpt+εWt .

I The process pt is an Ornstein–Uhlenbeck process.

I What is Wt ?

I Stochastic differential equation

dpt = −λptdt+εdWt

can be understood as an integral equation

pt2 − pt1 = −λ

∫ t2

t1

psds+ε(Wt2 −Wt1)

for 0 ≤ t1 < t2 ≤ t.

Page 10: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

The classical Langevin equation.

I Wt is a standard Brownian motion (Wiener process).

Page 11: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 5: A.Einstein (1879–1955).

Page 12: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 6: N.Wiener (1894–1964).

Page 13: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

The classical Langevin equation.

I Einstein–Wiener definition :(a) For any t ≥ 0 and s > 0, Wt+s −Wt ∼ N (0, s) ;(b) For any 0 < t1 < ... < tn, Wt1 , Wt2 −Wt1 ,...,Wtn −Wtn−1 are independent ;(c) With probability 1 the process Wt has continuoustrajectories.

Page 14: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 7: A sample path of Wt in dimension 2.

Page 15: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

The classical Langevin equation.

I The Brownian component is only in the momentum variable :

{qt = pt ,

pt = −λpt+εWt .

I “physical Brownian motion” 2.

2Einstein, A., Uber die von der molekularkinetischen Theorie der Warmegeforderte Bewegung von in ruhenden Flussigkeiten suspendierten Teilchen,Annalen der Physik, 322(8), pp.549–560.

Page 16: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

The classical Langevin equation.

I

Fig. 8: Motion of a damped free particle subject to randomfluctuations in Rn.

Page 17: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Equation of a “free” rigid body with fixed overhangingpoint.

I Motion of a free particle :

qt = 0 .

I Configuration space G = Rn.

I Hamiltonian equation :

{qt = pt ,pt = 0 .

I Phase space (qt , pt) ∈ Rn × Rn.

Page 18: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 9: Motion of a free particle in Rn.

Page 19: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Equation of a “free” rigid body with fixed overhangingpoint.

I Motion of a rigid body with a fixed overhanging point.

I Configuration space G = SO(3).

I “kinematic equation” : a(t) ∈ SO(3) such that

a−1a = z .

I “dynamic equation” : for z = z1e1 + z2e2 + z3e3 we have

z1 =I2 − I3

I1z2z3 ,

z2 =I3 − I1

I2z3z1 ,

z3 =I1 − I2

I3z1z2 .

I z ∈ TeG = g.

I Euler’s equation for a rigid body.

Page 20: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 10: Motion of a rigid body.

Page 21: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Equation of a “free” rigid body with fixed overhangingpoint.

I Configuration space G = SO(3).

I Phase space (a, z) ∈ G × TeG = G × g. 3

3Remark : In fact the phase space is the (co)tangent bundle T ∗G ∼= TG ,but since G = SO(3) is a Lie group, the bundle T ∗G ∼= TG is parallizable, andcan be viewed as G × g.

Page 22: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 11: Phase space : G × g.

Page 23: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Langevin equation of a rigid body.

I Configuration space G = SO(3).

I Phase space (a, z) ∈ G × TeG = G × g.

I “kinematic equation” :

a−1a = z .

I “dynamic equation” : for z = z1e1 + z2e2 + z3e3 we have

z1 =I2 − I3

I1z2z3−λz1+εW 1

t ,

z2 =I3 − I1

I2z3z1−λz2+εW 2

t ,

z3 =I1 − I2

I3z1z2−λz3+εW 3

t .

Page 24: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Langevin equation of a rigid body.

I In short form{

a−1a = z ,

z = q(z , z)− λz + εW .

I q(z1, z2) is a quadratic, bilinear form.

I Process (at , zt) lives in G × g, G = SO(3).

Page 25: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 12: Phase space : G × g.

Page 26: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Motion of ideal and viscous incompressible fluid.

I Let the group G be the volume–preserving diffeomorphismgroup of a certain domain M.

I This group G models the motion of ideal incompressible fluidwithin that domain M. The original picture is from Arnold’sclassical work in 1966 4.

I The equation of the “free particle” is now an Euler’s equation

ut + (u · ∇)u +∇p = 0 , divu = 0 ,

and the “Langevin equation” is now a stochasticNavier–Stokes equation

ut + (u · ∇)u +∇p = ∆u + εW , divu = 0 .

4Arnold, V.I., Sur la geometrie differentielle des groupes de Lie dedimension infinie et ses applications a l’hydrodynamique des fluides parfaits,Ann. Inst. Fourier (Grenoble), 16, 1966 fasc. 1, pp. 319–361.

Page 27: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Classical mechanics from group theoretic point of view.

I G : n–dimensional Lie group ; g = TeG : Lie algebra.

I On g we introduce an inner product 〈•, •〉, and a basise1, ..., en.

5

I Left–invariant frame : carry the basis e1, ..., en to any TaG byleft–translation b → ab : ek(a) = aek .

I Left–invariant metrics on G is given by 〈•, •〉 :〈ξ, η〉a = 〈ξkek , ηkek〉 for ξ = ξkek(a), η = ηkek(a) ∈ TaG .

I Kinetic energy : T (a, a) =1

2〈a, a〉a.

5Remark : Actually the dual space g∗ and dual basis e1, ..., en are involvedin the Hamiltonian formalism, but for simplicity and easy understanding we willidentify g∗ with g via 〈•, •〉.

Page 28: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 13: Configuration space : Left–invariant frame on G .

Page 29: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Classical mechanics from group theoretic point of view.

I Hamiltonian H(a, a) = T (a, a).

I Hamiltonian equation

{a−1a = zz = q(z , z) .

where (a, z) ∈ G × g.

I The solution a(t) gives a geodesic flow on the group G withrespect to its left–invariant metric.

I q(z1, z2) is a quadratic, bilinear form that can be calculatedfrom the structure constants of the Lie algebra g.

I z = q(z , z) is the so called Euler–Arnold equation. 6

6Tao, T., The Euler–Arnold equation. available online athttps ://terrytao.wordpress.com/2010/06/07/the-euler-arnold-equation/

Page 30: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Langevin equation on finite–dimensional group G .

I Langevin equation for the dynamics of geodesic flow onfinite–dimensional group G can be written as

{a−1a = z ,

z = q(z , z)− λz + εσW .

I (a, z) ∈ G × g, ε > 0 and σ = (σ1, ..., σr ) is an n × r matrix,σk ∈ Rn, k = 1, ..., r , Wt = (W 1

t , ...,W rt )T is the standard

Brownian motion in Rr .

I We want degenerate noise so we usually pick r < n :stochastic forcing through a few degrees of freedom given bythe vectors σ1,...,σr .

Page 31: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Stochastic mechanical models : ergodic theory.

I What type of problems are people usually interested in thesestochastic mechanical models ?

I Long time evolution, ergodicity, invariant measure ...

I For example, in the classical work of Hairer–Mattingly 7, theyestablished the ergodicity for a stochastically forced 2–dNavier–Stokes equation. The stochastic forcing is degenerate.

I Another example : problems about turbulent mixing 8.

7Hairer, M., Mattingly, J.C., Ergodicity of the 2D Navier–Stokes equationswith degenerate stochastic forcing, Annals of Mathematics, (2) 164 (2006), no.3, 993–1032.

8Komorowski, T., Papanicolaou, G., Motion in a Gaussian incompressibleflow, Annals of Applied Probability, 7, 1, 1997, pp. 229–264.

Page 32: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Stochastic mechanical models : ergodic theory.

I Our major interest is the ergodic theory of the equation

{a−1a = z ,

z = q(z , z)− λz + εσW .

I Existence and uniqueness of invariant measure ? Long–timeconvergence to the invariant measure ? Structure of invariantmeasure ?

I The classical Langevin equation

{qt = pt

pt = −λpt + εWt

has an invariant measure with density ∝ exp(− λε2 |p|2Rn), that

is the Boltzmann distribution.

Page 33: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Ergodic theory : deterministic vs. stochastic.

I Ergodic theory for the classical Hamiltonian equation

{a−1a = zz = q(z , z) .

is usually very hard.

I It is much easier for the stochastic equation

{a−1a = z ,

z = q(z , z)− λz + εσW .

Page 34: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 14: Ergodic theory.

Page 35: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Markov process associated with Langevin equation onfinite–dimensional group G .

I Think of the Langevin equation as a stochastic dynamicalsystem on G × g :

(az

)=

(az

q(z , z)− λz

)+ ε

(0

σW

). (∗)

I Even if σ is non–degenerate, the noise is degenerate for theLangevin dynamics on G × g.

I (∗) gives a Markov process (at , zt) on G × g.

Page 36: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Ergodic theory for Markov processes.

I Ergodic theory for Markov processes ≈ irreducibility +smoothing .

I Smoothing = “loss of memory” = “essentially stochastic” = “locally spread stochasticity to all directions” = “ aperiodicity” (for Markov chains) = “Hypoellipticity” (for diffusions).

I Roughly speaking, the process spreads stochasticity to alldirections via the interaction of the injection of noise in a fewdirections and the deterministic drift term, so that the processlocally will reach an open set around the solution of thedeterministic system 9.

9Hairer, M., On Malliavin’s proof of Hormander’s theorem. Bulletin dessciences mathematiques, 135(6), August 2011.

Page 37: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 15: Ergodic theory for Markov processes.

Page 38: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Hypoellipticity for the classical Langevin equation.

I Let us look at the system of stochastic differential equationssatisfied by the process (qt , pt) starting from (q0, p0) ∈ R2n :

{qt = pt ,

pt = −λpt+εWt .

Page 39: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 16: A.N.Kolmogorov (1903–1987).

Page 40: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Hypoellipticity for the classical Langevin equation.

I Suppose (q0, p0) ∈ R2n and

P((qt , pt) ∈ dqdp) = g(t; q, p)dqdp .

I Basic principle proposed by Kolmogorov : The probabilitydensity g(t; q, p) is a fundamental solution to theFokker–Planck equation (forward Kolmogorov equation)10 :

∂g

∂t= −

n∑i=1

pi∂g

∂qi+ λ

n∑i=1

∂pi(pig) +

ε2

2

n∑i=1

∂2g

∂p2i

;

g(0; q, p) = δ(q0, p0) .

10Kolmogorov, A.N., Uber die analytischen Methoden in derWahrscheinlichkeitsrechnung, Math. Ann., 104, 1931, pp. 415–458.

Page 41: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Hypoellipticity for the classical Langevin equation.

I The closed–form solution when n = 1, λ = 0 is also given byKolmogorov in a small paper on Brownian motion 11 :

g(t; q, p)

=8√

3

πε4t2exp

{− 1

ε2

[(p − p0)

2

2t+

6(q − q0 − p+p02 t)2

t3

]}.

I In general when λ > 0 the solution g(t; q, p) will again besmooth.

I “Smoothing”= full regularity !

I Why degenerate PDE yields smooth solution ?

11Kolmogorov, A.N., Zur Theorie Brownschen Bewegung, Annals ofMathematics, 35, 1934, pp. 116–117.

Page 42: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Hypoellipticity for the classical Langevin equation.

I Think of the classical Langevin equation as a stochasticdynamical system on R2n :

(qp

)=

(p−λp

)+

(0

εW

).

I Noise W is only injected in the p–direction.

I It is carried to the q–direction via interaction of the noise W

and the drift term p∂

∂q.

I Local smoothing.

Page 43: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 17: Hypoellipticity in Kolmogorov’s example.

Page 44: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 18: L.Hormander (1931–2012).

Page 45: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Hypoellipticity for general diffusion process.

I Consider the SDE

dx = X0(x)dt +r∑

k=1

Xk(x) ◦ dW k

on a manifold M.

I Let X0 = {Xk , k ≥ 1} and recursively defineXk+1 = Xk ∪ {[X ,Xj ],X ∈ Xk and j ≥ 0}.

I Lie bracket :[X1,X2] = ∇X1∇X2 −∇X2∇X1 = DX2X1 − DX1X2.

I Hormander’s parabolic hypoellipticity condition : ∪k≥1Xk

spans the whole tangent space TxM.

I This condition ensures the existence of a smooth density forthe corresponding Markov process xt , and for the solution tothe Fokker–Planck equation.

Page 46: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Ergodic theory for Langevin equation on finite–dimensionalgroup G .

I Back to the Langevin equation :

(az

)=

(az

q(z , z)− λz

)+ ε

(0

σW

).

I X0(a, z) =

(z

qk(z , z)∂

∂zk− λz

), Xk(a, z) =

(0σk

),

k = 1, 2, ..., r , σk ∈ g as constant vector fields.

I What is the bracket

[(AU

),

(BV

)]?

Page 47: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 19: Lie bracket of

(AU

)and

(BV

).

Page 48: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Ergodic theory for Langevin equation on finite–dimensionalgroup G .

I Let the vector field Q(z , z) = qk(z , z)∂

∂zk.

I Let Σ0 = {σj , j = 1, 2, ..., r}, and for k = 0, 1, 2, ... werecursively defineΣk+1 = Σk ∪ {Q(σj , σ), σ ∈ Σk , j = 1, 2, ..., r}. LetΣ = ∪∞k=1Σk .

I Theorem 1. (Hu–Sverak, 2015) The Langevin system

(az

)=

(az

q(z , z)− λz

)+ ε

(0

σW

)

satisfies the Hormander’s parabolic hypo–elliptic condition ifand only if Σ spans g. In this case if G is compact, theinvariant density for the a–process on G is constant withrespect to the Haar measure on G.

Page 49: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

More conservation laws.

I The Langevin equation

{a−1a = z ,

z = q(z , z)−λz+εσW

is incorporated with a dissipative structure : the friction term−λz dissipates the energy.

I This energy dissipation is compensated by the noise termεσW , and when a balance is reached we approach aninvariant measure.

I We cannot remove −λz unless we make use of a moreconservative noise.

Page 50: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

More conservation laws.

I What are the conservation laws of the “free” equation ? Recallthat when we remove the friction and the noise in theLangevin equation we come back to the Hamiltonian equation

{a−1a = z ,z = q(z , z) .

I Conservation of energy (Hamiltonian) H(z) =1

2〈z , z〉.

I Conservation of angular momentum : the equation z = q(z , z)moves the variable z only on a submanifold O(η) ⊂ g.

I O∗(η) = {aηa−1, a ∈ G , η ∈ g∗} : co–adjoint orbit.

I Z = {H = const} ∩ O(η) is the manifold on which thez–variable moves.

Page 51: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 20: Phase space : G × Z .

Page 52: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Constrained Brownian motion compatible with theconservation law.

I Phase space is now G × Z .

I The Langevin equation

{a−1a = z ,

z = q(z , z)−λz+εσW .

I When we remove the dissipation −λz , we have to replace thenoise +εσW by a conservative noise εξ restricted to Z .

I {a−1a = z ,z = q(z , z)+εξ .

I Consideration from canonical ensemble : the new noise ξ hasto be adapted to the invariant measure of the Hamiltoniandynamics z = q(z , z).

Page 53: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Constrained Brownian motion compatible with theconservation law.

I Work with constrained Brownian motion 12.

12Freidlin, M., Wentzell, A., On the Neumann problem for PDE’s with asmall parameter and the corresponding diffusion processes, Probability Theoryand Related Fields, 152(1), pp. 101–140, January 2012.

Page 54: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 21: Constrained Brownian motion compatible with the canonicalensemble.

Page 55: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Ergodic theory for the conservative stochastic equation.

I Conservative stochastic perturbations of geodesic flow onfinite–dimensional group G :

{a−1a = z ,z = q(z , z) + εξ .

I Markov process on G × Z defined by the equation

(az

)=

(az

q(z , z)

)+ ε

(0ξ

).

I Apply Hormander’s parabolic hypoellipticity condition again.

Page 56: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Ergodic theory for the conservative stochastic equation.

I Theorem 2. (Hu–Sverak, 2015) The conservative stochasticsystem (

az

)=

(az

q(z , z)

)+ ε

(0ξ

)

satisfies the Hormander’s parabolic hypo–elliptic condition ifand only if the Lie algebra hull containing Z − Z and invariantunder the mapping z → [z0, z ] for all z ∈ Z coincides with g.In this case if G is compact, then the long–term dynamics forthe a–process will approach an invariant measure withconstant density with respect to the Haar measure on G.

Page 57: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Ergodic theory for the conservative stochastic equation.

I The Lie algebra hull containing Z − Z and invariant under themapping z → [z0, z ] for all z ∈ Z coincides with g is a purelyalgebraic property in terms of finite dimensional objectsrelated to the group’s Lie algebra.

I The original Hormander’s condition is related to iterated Liebrackets of vector fields on G × g. It is usually hard to check.

I We made use of algebraic as well as geometric observations tofind these optimal conditions.

I The conditions we found also shed some light in infinitedimensions. It can be thought of as a characterization of howthe non–linearity amplifies the effect of noise, which can onlyact in a few directions. This is exactly what we see in fluidflows.

Page 58: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Non–compact case.

I We also consider an example of a non–compact groupG = Rn and a one–dimensional submanifold γ : R→ Z ⊂ Rn.

I {a = γ(s) ;s = εw .

I Variable s is arc–length parameter on Z ; γ(s) is aparametrization of Z ; w(t) is Brownian motion on Z .

Page 59: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Non–compact case.

I Imagine the motion of a satellite in space.

I We interpret Z as a “control curve”.

I The motion of the satellite is only random along directionspointed out by Z .

Page 60: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Fig. 22: Controlled random motion of a satellite.

Page 61: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Non–compact case.

I Conclusion : The position a(t) of the satellite, after a longtime, satisfies a central limit theorem.

I It is non trivial because random forcing is “controlled”.

I A classical method of auxiliary functions using Ito’s formulawas used to obtain a central limit theorem for the a–process.

Page 62: Stochastically perturbed geodesic °ows on Lie groups.web.mst.edu/~huwen/...geodesic_flows_on_Lie_groups.pdf · Classical mechanics from group theoretic point of view. I Hamiltonian

Thank you for your attention !