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Discretization of Stochastic Differential Systems With Singular Coefficients Part I Denis Talay INRIA Sophia Antipolis, France TOSCA Project-team ICERM - Brown November 2012 Outline Introduction Monte Carlo Methods For Linear PDEs


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SLIDE 1

Discretization of Stochastic Differential Systems With Singular Coefficients Part I

Denis Talay

INRIA Sophia Antipolis, France TOSCA Project-team

ICERM - Brown – November 2012

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SLIDE 2

Outline

Introduction Monte Carlo Methods For Linear PDEs Discretization of Stochastic Hamiltonian Dissipative Systems Stochastic Lagrangian Models for Turbulent Flows Conclusion

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SLIDE 3

Outline

Introduction Monte Carlo Methods For Linear PDEs Discretization of Stochastic Hamiltonian Dissipative Systems Stochastic Lagrangian Models for Turbulent Flows Conclusion

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SLIDE 4

Why is Probability useful?

THE WORLD IS COMPLEX

◮ The physical model is badly calibrated (e.g., MEG or electrical

neuronal activity: few sensors),

◮ The physical law is not completely known (e.g., turbulence,

meteorology,. . . ),

◮ There is no physical law (e.g., finance).

THE PARTIAL DIFFERENTIAL EQUATIONS ARE COMPLEX

◮ Mathematical analysis (existence, uniqueness, smoothness), ◮ Probabilistic analysis of deterministic numerical methods (cf.

Kushner, or domain decompositions, or artificial boundary conditions),

◮ Probabilistic numerical methods for high dimensional problems

and/or equations in domains with possibly complex geometries and/or small viscosities (high Reynolds numbers),. . . ).

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SLIDE 5

SUMMARY:

◮ Probability theory (in particuler, stochastic integration theory) is

used to solve problems which, by nature, are deterministic or ’stochastic’,

◮ Probabilistic models and numerical methods are used when

deterministic ones are unefficient.

◮ In all cases, one seeks a statistical information on the model:

classical numerical analysis needs to be deeply adapted. Remarks:

◮ For physicists, Stochastic PDEs often are PDEs with random

coefficients,

◮ Stochastic collocation methods are not stochastic.

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SLIDE 6

Outline

Introduction Monte Carlo Methods For Linear PDEs Discretization of Stochastic Hamiltonian Dissipative Systems Stochastic Lagrangian Models for Turbulent Flows Conclusion

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SLIDE 7

General parabolic PDEs

Let b : Rd → Rd and σj : Rd → Rd, (1 ≤ j ≤ r). Consider the elliptic

  • perator

Lψ(x) :=

d

  • i=1

bi(x) ∂iψ(x) + 1 2

d

  • i,j=1

ai

j(x) ∂ijψ(x),

where a(x) := σ(x) σ(x)t, and the evolution problem    ∂u ∂t (t, x) = Lu(t, x), t > 0, x ∈ Rd, u(0, x) = f(x), x ∈ Rd.

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SLIDE 8

The Euler scheme for SDEs

Let (Gj

p) be i.i.d. N(0, 1) and h > 0 be the discretization step.

       ¯ X h

0 (x)

= x, ¯ X h

(p+1)h(x)

= ¯ X h

ph(x) + b

  • ¯

X h

ph(x)

  • h

+ r

j=1 σj

  • ¯

X h

ph(x)

√ h Gj

p+1. ◮ Easy to simulate (even for Lévy driven SDEs). ◮ Discretizes the stochastic differential equation

Xt(x) = x + t b(Xs(x)) ds + t σ(Xs(x)) dWs.

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SLIDE 9

Moments of the Euler scheme

E {¯ X h

(p+1)h(x) − ¯

X h

ph} = E b

¯ X h

ph(x)

  • h,

E {(¯ X h

(p+1)h(x) − ¯

X h

ph) · (¯

X h

(p+1)h(x) − ¯

X h

ph)t} = E a(¯

X h

ph) h + O

  • h2

.

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SLIDE 10

Moments of the Euler scheme

E {¯ X h

(p+1)h(x) − ¯

X h

ph} = E b

¯ X h

ph(x)

  • h,

E {(¯ X h

(p+1)h(x) − ¯

X h

ph) · (¯

X h

(p+1)h(x) − ¯

X h

ph)t} = E a(¯

X h

ph) h + O

  • h2

.

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SLIDE 11

Probabilistic interpretation of parabolic PDEs

E f(¯ X h

T(x)) − u(T, x)

=

T/h−1

  • p=0

E

  • u
  • T − (p + 1)h, ¯

X h

(p+1)h(x)

  • − u
  • T − ph, ¯

X h

ph(x)

  • =

T/h−1

  • p=0

E

  • u
  • T − (p + 1)h, ¯

X h

ph(x)

  • − u
  • T − ph, ¯

X h

ph(x)

  • + h

T/h−1

  • p=0

E

  • Lu
  • T − (p + 1)h, ¯

X h

ph(x)

  • +

T/h−1

  • p=0

O

  • h2

= h

T/h−1

  • p=0

E

  • Lu
  • T − ph, ¯

X h

ph(x)

  • − ∂u

∂t

  • T − ph, ¯

X h

ph(x)

  • + O (h)

= O (h) , since ∂u ∂t (t, x) = Lu(t, x).

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SLIDE 12

Probabilistic interpretation of parabolic PDEs

E f(¯ X h

T(x)) − u(T, x)

=

T/h−1

  • p=0

E

  • u
  • T − (p + 1)h, ¯

X h

(p+1)h(x)

  • − u
  • T − ph, ¯

X h

ph(x)

  • =

T/h−1

  • p=0

E

  • u
  • T − (p + 1)h, ¯

X h

ph(x)

  • − u
  • T − ph, ¯

X h

ph(x)

  • + h

T/h−1

  • p=0

E

  • Lu
  • T − (p + 1)h, ¯

X h

ph(x)

  • +

T/h−1

  • p=0

O

  • h2

= h

T/h−1

  • p=0

E

  • Lu
  • T − ph, ¯

X h

ph(x)

  • − ∂u

∂t

  • T − ph, ¯

X h

ph(x)

  • + O (h)

= O (h) , since ∂u ∂t (t, x) = Lu(t, x).

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SLIDE 13

Probabilistic interpretation of parabolic PDEs

E f(¯ X h

T(x)) − u(T, x)

=

T/h−1

  • p=0

E

  • u
  • T − (p + 1)h, ¯

X h

(p+1)h(x)

  • − u
  • T − ph, ¯

X h

ph(x)

  • =

T/h−1

  • p=0

E

  • u
  • T − (p + 1)h, ¯

X h

ph(x)

  • − u
  • T − ph, ¯

X h

ph(x)

  • + h

T/h−1

  • p=0

E

  • Lu
  • T − (p + 1)h, ¯

X h

ph(x)

  • +

T/h−1

  • p=0

O

  • h2

= h

T/h−1

  • p=0

E

  • Lu
  • T − ph, ¯

X h

ph(x)

  • − ∂u

∂t

  • T − ph, ¯

X h

ph(x)

  • + O (h)

= O (h) , since ∂u ∂t (t, x) = Lu(t, x).

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SLIDE 14

Probabilistic interpretation of parabolic PDEs

E f(¯ X h

T(x)) − u(T, x)

=

T/h−1

  • p=0

E

  • u
  • T − (p + 1)h, ¯

X h

(p+1)h(x)

  • − u
  • T − ph, ¯

X h

ph(x)

  • =

T/h−1

  • p=0

E

  • u
  • T − (p + 1)h, ¯

X h

ph(x)

  • − u
  • T − ph, ¯

X h

ph(x)

  • + h

T/h−1

  • p=0

E

  • Lu
  • T − (p + 1)h, ¯

X h

ph(x)

  • +

T/h−1

  • p=0

O

  • h2

= h

T/h−1

  • p=0

E

  • Lu
  • T − ph, ¯

X h

ph(x)

  • − ∂u

∂t

  • T − ph, ¯

X h

ph(x)

  • + O (h)

= O (h) , since ∂u ∂t (t, x) = Lu(t, x).

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SLIDE 15

Probabilistic interpretation of parabolic PDEs

E f(¯ X h

T(x)) − u(T, x)

=

T/h−1

  • p=0

E

  • u
  • T − (p + 1)h, ¯

X h

(p+1)h(x)

  • − u
  • T − ph, ¯

X h

ph(x)

  • =

T/h−1

  • p=0

E

  • u
  • T − (p + 1)h, ¯

X h

ph(x)

  • − u
  • T − ph, ¯

X h

ph(x)

  • + h

T/h−1

  • p=0

E

  • Lu
  • T − (p + 1)h, ¯

X h

ph(x)

  • +

T/h−1

  • p=0

O

  • h2

= h

T/h−1

  • p=0

E

  • Lu
  • T − ph, ¯

X h

ph(x)

  • − ∂u

∂t

  • T − ph, ¯

X h

ph(x)

  • + O (h)

= O (h) , since ∂u ∂t (t, x) = Lu(t, x).

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SLIDE 16

Convergence rate

Let F(·) be a functional on the path space. The global error of a Monte Carlo method is E F(X·) − 1 N

N

  • k=1

E F ¯ X h,k

·

  • = E F(X·) − E F(¯

X h

· )

  • =:ǫd(h)

+ E F(¯ X h

· ) − 1

N

N

  • k=1

F ¯ X h,k

·

  • =:ǫs(h,N)

. The statistical error satisfies ∃C > 0, E |ǫs(h)| ≤ C √ N for all h.

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SLIDE 17

Concerning the discretization error : Suppose that f has a polynomial growth at infinity. Under hypoellipticity conditions, or when all the functions of the problem are smooth, one has (T.-Tubaro, Bally-T. etc.) ed(h) = Cf(T, x) h + Qh(f, T, x) h2, where |Cf(T, x)| + suph|Qh(f, T, x)| ≤ C (1 + xQ)1 + K(T) T q Thus, Romberg extrapolation techniques can be used: E

  • 2

N

N

  • k=1

f

  • ¯

X h/2,k

T

  • − 1

N

N

  • k=1

f

  • ¯

X h,k

T

  • = O
  • h2

. Remark: The technique used in the proofs is purely probabilistic (stochastic flows of diffeomorphisms, Malliavin variations calculus).

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SLIDE 18

Dirichlet boundary conditions

For        ∂u ∂t (t, x) = Lu(t, x), t > 0, x ∈ D, u(0, x) = f(x), x ∈ D, u(t, x) = g(x), x ∈ ∂D,

  • ne has

u(t, x) = E f(Xt(x)) It<τ + E g(Xτ(x)) It≥τ, where τ:= ‘first boundary hitting time of (Xt)’. The stopped Euler scheme is defined as ¯ X h

ph∧τ h(x),

where τ h:= ‘first boundary hitting time of the Euler scheme’. For a convergence rate analysis, see Gobet, Menozzi, etc.

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SLIDE 19

Neumann boundary conditions

For        ∂u ∂t (t, x) = Lu(t, x), t > 0, x ∈ D, u(0, x) = f(x), x ∈ D, ∇u(t, x) · n(x) = 0, x ∈ ∂D,

  • ne has

u(t, x) = E f(Xt(x)) where X:= ‘reflected diffusion process’: Xt(x) = x + t b(Xs(x)) ds + t σ(Xs(x)) dWs + t n(Xs)dLs(X). Here, (Lt(X)) is an increasing process, namely the local time of X at the boundary . The reflected Euler scheme is defined in such a way that the simulation of the local time is avoided.

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Consider a domain D ⊂ Rd, with smooth boundary. Let n(s) denote the unit inward normal vector at s ∈ D. Suppose that the vector field γ defining the reflection direction is uniformly non tangent to the boundary. Consider the reflected S.D.E. with smooth coefficients and strictly uniformly elliptic generator Xt = x + t b(Xs)ds + t σ(Xs)dWs + t γ(Xs) dks, where kt = t IXs∈D dks. To discretize the above reflected SDE , start at x ∈ D at time 0, and assume that one has obtained ˜ X h

ph ∈ D. Then observe that for all x in

a neighborhood of D, there exist a unique pair of functions πγ

∂D taking

values in ∂D and F γ taking values in R such that x = πγ

∂D(x) + F γ(x)γ(πγ ∂D(x)).

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SLIDE 21

Then,

◮ For t ∈ [tn i , tn i+1], set

˜ Y i

t := ˜

X h

ph + b(˜

X h

ph)(t − tn i ) + σ(˜

X h

ph)(Wt − Wtn

i ).

i) If ˜ Y i

(p+1)h /

∈ D, set ˜ X h

(p+1)h = πγ ∂D(˜

Y i

(p+1)h) − F γ(˜

Y i

(p+1)h)γ(˜

Y i

(p+1)h).

ii) If ˜ Y i

(p+1)h ∈ D, ˜

X h

(p+1)h = ˜

Y i

(p+1)h.

Let f be a function of class C5

b(D, R) which satisfies the compatibility

condition ∀z ∈ ∂D, [∇f γ](z) = [∇(Lf) γ](z) = 0.

  • Theorem. (Bossy–Gobet–T.) One has

|E (f(˜ X h

T)) − E (f(XT))| ≤ K(T)

n

  • α:|α|≤5

∂α

x f∞

for some constant K(T) uniform w.r.t. x and f.

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SLIDE 22

Outline

Introduction Monte Carlo Methods For Linear PDEs Discretization of Stochastic Hamiltonian Dissipative Systems Stochastic Lagrangian Models for Turbulent Flows Conclusion

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SLIDE 23

Stochastic Hamiltonian dynamics

  • dQt = ∂pH(Qt, Pt)dt,

dPt = −∂qH(Qt, Pt)dt − F1(H(Pt, Qt))∂pH(Qt, Pt)dt + F2(H(Pt, Qt))dWt, where H : Rd × Rd → R, and F1, F2 : R → R. Problems to solve:

◮ Existence, uniqueness of an invariant probability measure µ; ◮ The measure µ has a continuous and strictly positivite density; ◮ Construction of an approximate ergodic process ( ¯

Qn, ¯ Pn);

◮ Precise estimate on the global error

  • f(q, p)dµ − 1

K

K

  • k=1

f( ¯ Qn

k/n, ¯

Pn

k/n)

  • In,K

.

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SLIDE 24

Our main assumptions

◮ H, F1, F2 are smooth functions; ◮ A convexity type assumption on D2H; ◮ ∂ppH is bounded; ◮ ∃R > 0, ∃C0 > 0, F1(x) ≥ C0 for x ≥ R; ◮ ∃C0 > 0, F2(x) ≥ C0; ◮ Boundedness conditions on the derivatives of F 2.

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The implicit Euler scheme

The explicit Euler scheme may have moments not uniformly bounded in time (counterexamples. . . ). The implicit Euler scheme:

Choose an arbitrary 0 < ρ < 1.

       ¯ Qn

k+1 = ¯

Qn

k + ∂pH( ¯

Qn

k+1, ¯

Pn

k+1)ρ

n, ¯ Pn

k+1 = ¯

Pn

k − ∂qH( ¯

Qn

k+1, ¯

Pn

k+1)ρ

n − F1 ◦ H( ¯ Qn

k+1, ¯

Pn

k+1)ρ

n + F2 ◦ H( ¯ Qn

k, ¯

Pn

k )

  • W(k+1)ρ/n − Wkρ/n
  • .

Remark: using H + 1 as a Lyapunov function, one can prove that the implicit Euler scheme has moments uniformly bounded in time.

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Ergodicity of the implicit Euler scheme

Uniform in time upper bounds for the moments = ⇒ existence of an invariant probability measure ¯ µn for the implicit Euler scheme. To get uniqueness, prove that the chain is positive Harris recurrentowing to sufficient conditions found in Meyn and Tweedie:

◮ Prove that the chain is forward accessible and 0 is a globalling

attracting state, which provides the irreducibilityof the chain;

◮ Check that the chain is a T-chain; for an irreductible T-chain,

every compact set is a petite set; thus, there obviously exists a petite set K such that E

  • H( ¯

Qn

1, ¯

Pn

1)

  • ( ¯

Qn

0, ¯

Ph

0) = (q, p)

  • − H(q, p)

≤ −1 + b IK(q, p), ∀(q, p) ∈ R2d. For similar results: see Shardlow & Stuart (1999), Higham & Mattingly & Stuart (1999).

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SLIDE 27

Ergodicity of the Hamiltonian process

Uniform in time upper bounds for the moments = ⇒ existence of an invariant probability measure µ for (Qt, Pt). To get uniqueness, prove:

◮ The law of (Qt, Pt) has a smooth density π(t, q, p) for all t > 0:

this results, e.g., from hypoellipticityand a localization technique (the latter argument is used because of the possible unboundedness of ∂pqH, ∂qqH);

◮ The density π(t, q, p) is strictly positive everywhere: this results

from Michel & Pardoux’s controllability argument, since the reachibility set of the system

  • dQu

t = ∂pH(Qu t , Pu t )dt,

dPu

t = −∂qH(Qu t , Pu t )dt − F1(H(Pu t , Qu t ))∂pH(Qu t , Pu t )dt + F2(H(Pu t , Qu t

is the whole space. Remark: the measure µ has finite moments of all order.

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SLIDE 28

Exponential decay of moments of (Qt, Pt): the statement

Set u(t, x, v) := E

  • f(Xt, Vt)
  • (X0, V0) = (x, v)
  • R2d f dµ.

Theorem 1 Suppose that f is a smooth function, and that all its derivatives have a growth at most polynomial at infinity. Let Dmu(t) denote the vector of the derivatives of order m of the mapping (q, p) → u(t, q, p). For all integer m there exist an integer sm and Cm > 0, γm > 0 such that |Dmu(t)| ≤ Cm(1 + |q|sm + |p|sm) exp(−γmt), ∀t > 0, ∀(q, p) ∈ R2d.

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SLIDE 29

Sketch of the proof of Theorem 1

  • 1. Prove that, for any ball B in R2d, there exist C > 0 and

λ > 0 such that

  • B

|u(t)|2dµ ≤ C exp(−γt), ∀t > 0.

  • 2. Show that the preceding inequality also holds for any

spatial derivative of u(t) (possibly with different real numbers C and γ). As µ has a smooth and strictly positive density w.r.t. Lebesgue’s measure, deduce from the Sobolev imbedding Theorem that, for any ball B in R2d, there exist C > 0 and γ > 0 such that ∀(x, v) ∈ B, |u(t, q, p)| ≤ C exp(−γt), ∀t > 0.

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SLIDE 30

Sketch of the proof of Theorem 1 (cont.)

  • 3. Then show that there exist C > 0 and γ > 0 such that
  • |u(t)|2πs(q, p) dq dp ≤ C exp(−γt), ∀t > 0,

where πs(q, p) := 1 (H(q, p) + 1)s for some integer s.

  • 4. Finally, prove that the prededing inequality also holds

for any spatial derivative of u(t) (possibly with different real numbers s, C and γ). Then conclude by using the Sobolev imbedding Theorem again.

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SLIDE 31

Sketch of the proof of Theorem 1 (end)

Main step:in spite of the degeneracy of the generator L of (Qt, Pt),

  • ne has

A.∃C > 0, ∃γ0 > 0,

  • |u(t)|2dµ ≤ C exp(−γ0t), ∀t ≥ 0,

B.∃Ckl > 0, ∃γkl > 0,

  • |u(t)|2(|q|k + |p|ℓ)dµ ≤ Ckℓ exp(−γkℓt), ∀t ≥ 0,
  • C. exp(γT)
  • |u(T)|2 dµ +

T exp(γt)

  • ∂u

∂p (t)

  • 2

dµ dt ≤ C, ∀T > 0,

  • D. −

T exp(γ1t) ∂u ∂q (t)∂u ∂p (t)|q|2dµ dt ≤ C, ∀T > 0, E.

  • ∂u

∂q (T)

  • 2

dµ ≤ C exp(−γ2T), ∀T > 0.

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SLIDE 32

Convergence rate of the implicit Euler scheme

Decomposition of the global error:

  • f(q, p)dµ − In,K =
  • f(q, p)dµ −
  • R2d f(q, p)¯

µn(dq, dp)

  • ed(n)

+

  • R2d f(q, p)¯

µn(dq, dp) − In,K

  • es(n,K)

.

◮ The term ed(n) is a discretization error: we expand it in terms of

1ρ/n, from which we justify Romberg-Richardson extrapolation techniques to accelerate the convergence rate.

◮ The term es(n, K) is a statistical error: we provide estimates by

using classical results on the weak convergence of normalized martingales.

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SLIDE 33

Convergence rate of the implicit Euler scheme (cont.)

Theorem 2 Suppose that f is a smooth function, and that all its derivatives have a growth at most polynomial at infinity. Then ed(n) = C1 n + . . . + Cm nm + O

  • 1

nm+1

  • , ∀m ∈ N − {0},

for some real numbers Cj uniform w.r.t. n, and es(n, K) − − − − − →

K→+∞ 0 a.s.

  • n

K es(n, K) = ⇒ N(0, Σn), with Σn uniformly bounded w.r.t. n.

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SLIDE 34

Sketch of the proof of Theorem 2

Set ¯ Y n

k := ( ¯

Qn

k, ¯

Pn

k ).

One has u(jρ/n, ¯ Y n

k+1) E

= u(jρ/n, ¯ Y n

k )+Lu(jρ/n, ¯

Y n

k )ρ

n+C0(jρ/n, ¯ Y n

k )ρ2

n2 +r n

j,k+1

1 n3 . As u(t, q, p) solves du/dt = Lu, one deduces u(jρ/n, ¯ Y n

k+1) E

= u((j + 1)ρ/n, ¯ Y n

kρ/n) + C(jρ/n, ¯

Y n

k )ρ2

n2 + Rn

j,k+1

1 n3 . The function C(t, y) is a sum of terms of the type φ(q, p)∂Ju(t, q, p). The remainder term Rn

j,k+1 is a sum of terms of the type

E

  • P( ¯

Y n

k )∂Ju

  • jρ/n, ¯

Y n

k + θ( ¯

Y n

(k+1)ρ/n − ¯

Y n

k )

  • , θ ∈ (0, 1).
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SLIDE 35

Sketch of the proof of Theorem 2 (cont.)

Observe that 1 K

K

  • k=1

f( ¯ Y n

k ) = 1

K

K

  • k=1

u(0, ¯ Y n

k ) +

  • R2d f dµ.

Thus 1 K

K

  • k=1

f( ¯ Y n

k ) E

=

  • R2d f dµ+ 1

K

K

  • k=1

u(jρ/n, ¯ Y0)+ 1 K

K

  • k=1

k−1

  • j=0

C(jρ/n, ¯ Y n

k )ρ2

n2 + 1 K

K

  • k=1

By ergodicity, lim

K→∞

1 K

K

  • k=1

E u(kρ/n, ¯ Y0) = 0 and lim

K→∞ E f( ¯

Y n

k ) =

  • R2 f d ¯

µn.

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SLIDE 36

Sketch of the proof of Theorem 2 (end)

In view of the estimates of Theorem 1,

+∞

  • j=0

|Rn

j,k+1| ≤

C0 1 − exp(−γρ/n)E (1 + | ¯ Y n

k |s + | ¯

Y n

k+1|s),

from which

+∞

  • j=0

|Rn

j,k+1| ≤ Cn(1 + E | ¯

Y n

0 |s).

Moreover, in view of Theorem 1 again, ρ n lim

K→∞

1 K

K

  • k=1

k−1

  • j=0

E C(jρ/n, ¯ Y n

k ) =

  • R2d C(t, q, p)µ(dq, dp) dt+O

ρ n

  • .
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SLIDE 37

Outline

Introduction Monte Carlo Methods For Linear PDEs Discretization of Stochastic Hamiltonian Dissipative Systems Stochastic Lagrangian Models for Turbulent Flows Conclusion

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SLIDE 38

A simplified stochastic Lagrangian model

Consider a d-dimensional standard Brownian motion (Wt; t ∈ [0, T]), and ((Xt, Ut); t ∈ [0, T]) solution of              Xt = X0 + t Us ds, Ut = U0 + t B [Xs, Us; ρs] ds + t σ(s, Xs, Us) dWs, ρt is the density distribution of (Xt, Ut) for all t ∈ (0, T]. (1)

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SLIDE 39

Here, B is the mapping from Rd × Rd × L1(R2d) to Rd defined by B [x, u; γ] =           

  • Rd b(v, u)γ(x, v) dv
  • Rd γ(x, v) dv

if

  • Rd γ(x, v) dv = 0,

0 elsewhere, (2) where b : Rd × Rd → Rd is bounded .

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SLIDE 40

Formally, the drift component of (1) involves (x, u) → E

  • b (Ut, u)
  • Xt = x
  • .

(3) Such nonlinearity is typical of Lagrangian stochastic models for the position Xt and the velocity Ut of a generic fluid-particle in a turbulent flow: see the dramatically complex Probability Density Function (PDF) methods for turbulent flows and S. Pope’s models which aim to be alternative approaches to the Navier-Stokes equations for turbulent flows. Our objective is to show existence and uniqueness of a solution to

  • ur simplified Lagrangian model.
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SLIDE 41

Lagrangian stochastic models for monophasic turbulent flows

Statistical solutions to the Navier–Stokes equation: the Reynolds decomposition of the Eulerian velocity U of a turbulent flow is U(t, x, ω) = U(t, x) + u(t, x, ω), where U is the (ensemble) averaged part, and u is the fluctuating part. Reynolds Averaged Navier-Stokes (RANS) equations:        (∇x · U) = 0, ∂tU(i) +

  • U · ∇xU(i)
  • = −1

̺∇xP(i) + ν△xU(i) − ∂xju(i)u(j), U(0, x) = U0(x).

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SLIDE 42

The gradient pressure ∇xP solves the Poisson equation: − 1 ̺△xP = ∂2

xi,xjU(i)U(j) + ∂2 xixju(i)u(j).

The Reynolds stress tensor stands for the covariance of velocity components: u(i)u(j) = U(i)U(j) − U(i)U(j).

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SLIDE 43

The RANS equation is not closed. In Pope’s model, Lagrangian and Eulerian quantities are related as follows: for all suitable measurable function g : Rd → Rd, g(U)(t, x) = E [g(Ut)/Xt = x] . (4) The simplest model proposed by Pope (2003) is the simplified Langevin model            Xt = X0 + t

0 Us ds,

Ut = U0 − 1 ̺ t

0 ∇xP(s, Xs) ds + ν

t

0 △xU(s, Xs) ds

+C1 t E (s, Xs) k(s, Xs) (U(s, Xs) − Us) ds + t

  • C2E (s, Xs) dWs.
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SLIDE 44

Technical difficulties in the analysis

Difficulties come from the dependency of the drift coefficient on the conditional expectation. Related situations: Sznitman (1986): dζt = pt(ζt) dt + dWt, where pt is the Lebesgue density of ζt. Oelschlager (1985): dζt = F (ζt, pt(ζt)) dt + dWt, where F : Rd × R is a bounded function, and dζt = ∇pt(ζt) dt + dWt. Dermoune (2003): dζt = E (v(ζ0) / ζt) dt + dWt, where v : Rd → Rd is a bounded continuous function.

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SLIDE 45

Our situation drastically differs from the above:

◮ our drift coefficient depends on conditional distributions rather

than the density ρt itself;

◮ the infinitesimal generator of (Xt, U) is not strongly elliptic .

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SLIDE 46

A stochastic particle system

Consider                        X i,ǫ,N

t

= X i

0 +

t

0 Ui,ǫ,N s

ds, Ui,ǫ,N

t

= Ui

0 +

t

N

  • j=1

b(Uj,ǫ,N

s

, Ui,ǫ,N

s

)φǫ(X i,ǫ,N

s

− X j,ǫ,N

s

)

N

  • j=1
  • φǫ(X i,ǫ,N

s

− X j,ǫ,N

s

) + ǫ

  • ds

+ t

0 σ(s, Xs, Ui,ǫ,N s

) dW i

s, i = 1, · · · , N,

where {φǫ; ǫ > 0} is a family of mollifiers.

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SLIDE 47

We prove that the particles propagate chaos: as N tends to infinity, (X 1,ǫ,N, U1,ǫ,N) converges weakly to the solution of              X ǫ

t = X0 +

t Uǫ

s ds,

t = U0 +

t Bǫ [X ǫ

s , Uǫ s; ρǫ s] ds +

t σ(s, Xs, Us) dWs, ρǫ

t is the density of (X ǫ t , Uǫ t ) for all t ∈ (0, T],

(5)

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SLIDE 48

where the kernel Bǫ [x, u; γ] is defined by: for all nonnegative γ ∈ L1(R2d), (x, u) ∈ R2d, Bǫ [x, u; γ] =

  • Rd b(v, u)φǫ ∗ γ(x, v) dv
  • Rd φǫ ∗ γ(x, v) dv + ǫ

, (6) where φǫ ∗ γ(x, u) =

  • Rd φǫ(x − y)γ(y, u) dy.
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SLIDE 49

Our main theorem

Our assumptions.

◮ b is a bounded continuous function. ◮ The velocity diffusion coefficient σ is bounded and strongly

elliptic.

◮ For all 1 ≤ i, j ≤ d, σ(i,j) is Hölder continuous (in a reinforced

sense). Theorem. (i) For all ǫ > 0, the sequence {(X 1,ǫ,N, U1,ǫ,N); N ≥ 1} converges weakly to a weak solution (X ǫ, Uǫ) of (5). This solution is unique and, if Pǫ denotes the law by (X ǫ, Uǫ) (5), the interacting particle system is Pǫ-chaotic; that is, for every integer k ≥ 2 and every finite family {ψl; l = 1, · · · , k} of Cb(C([0, T] ; R2d)), Pǫ,N, ψ1 ⊗ ...ψk ⊗ . . . − →

k

  • l=1

Pǫ, ψl, when N − → +∞. (7) (ii) When ǫ tends to 0, (X ǫ, Uǫ) converges weakly to the unique solution (X, U) of (1).

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SLIDE 50

The non-linear martingale problems

  • Definition. A probability measure P on C([0, T] ; R2d) is said a weak

solutionto (1) or a solution to the martingale problem (MP) if (i) P ◦ (x0, u0)−1 = µ0. (ii) For all t ∈ (0, T], the time-marginal P ◦ (xt, ut)−1 has a positive density ρt w.r.t. Lebesgue measure on R2d. (iii) For all f ∈ C2

b(R2d), the process

f(xt, ut) − f(x0, u0) − t Aρs(f)(s, xs, us) ds (8) is a P-martingale, where, for each positive γ ∈ L1(R2d), Aγ is defined as Aγ(f)(t, x, u) = (u · ∇xf(x, u)) + (B [x, u; γ] · ∇uf(x, u)) + 1 2

d

  • i,j=1

(σσ∗)(i,j)(t, x, u)∂2

ui,ujf(x, u).

(9)

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SLIDE 51
  • Definition. A probability measure Pǫ on C([0, T]; R2d) is said a weak

solution to (5) or a solution to the martingale problem (MPǫ) if (i) Pǫ ◦ (x0, u0)−1 = µ0. (ii) For all t ∈ (0, T], the time–marginal Pǫ ◦ (xt, ut)−1 has a density ρǫ

t w.r.t. Lebesgue measure on R2d.

(iii) For all f ∈ C2

b(R2d), the process

f(xt, ut) − f(x0, u0) − t Aǫ

ρǫ

s (f)(s, xs, us) ds

is a Pǫ-martingale where, for all γ ∈ L1(R2d), Aǫ

γ is

defined as Aǫ

γ(f)(t, x, u) = (u · ∇xf(x, u)) + (Bǫ [x, u; γ] · ∇uf(x, u))

+ 1 2

d

  • i,j=1

(σσ∗)(i,j)(t, x, u)∂2

ui,ujf(x, u).

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SLIDE 52

A uniqueness result

  • Proposition. There is at most one weak solution to Equation (1) and
  • ne weak solution to Equation (5).

Sktech of the proof: One can easily prove existence and weak uniqueness for

  • Y s,y,v

t

= y + t

s V s,y,v θ

dθ, V s,y,v

t

= v + t

s σ(θ, Y s,y,v, V s,y,v θ

) dWθ. In addition, the transition density Γ(s, y, v; t, x, u) of the solution satisfies the following estimate (see Francesco and Pascucci (2006)): sup

(y,v)∈R2d

  • Rd |∇vΓ(s, y, v; t, x, u)| dx du ≤

C √ t − s, ∀ 0 ≤ s < t ≤ T.

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SLIDE 53

A uniqueness result

Set S∗

t,s(f)(x, u) =

  • R2d Γ(s, y, v; t, x, u)f(y, v) dy dv.

We then prove that the densities ρt and ρǫ

t are the unique solutions (in

appropriate spaces) to mild equations: for example, ∀ t ∈ (0, T], ρt = S∗

t,0(µ0) +

t S′

t,s (ρs(·)B [· ; ρs]) ds in L1(R2d).

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SLIDE 54

An existence result

  • Proposition. The martingale problem (MPǫ) has a unique solution Pǫ

and, when ǫ tends to 0, Pǫ converges to a solution of (MP). The proof proceeds in two steps:

◮ We show that {¯

Pǫ,N; N ≥ 1} is relatively compact and that any weakly convergent subsequence assigns full measure to the set

  • f the solutions to the martingale problem (MPǫ).

◮ The probability measure Pǫ, solution of the martingale problem

(MPǫ), converges to the solution of the martingale problem (MP).

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SLIDE 55

First step

Let ¯ µǫ,N be the empirical measure defined on M(C([0, T]; R2d)) by ¯ µǫ,N = 1 N

N

  • i=1

δ{X i,ǫ,N,Ui,ǫ,N}. Let ¯ Pǫ,N = Q ◦ (¯ µǫ,N)−1 be the probability law of ¯ µǫ,N. Easy: The sequence {¯ Pǫ,N; N ≥ 1} is tight on M(C([0, T]; R2d)). Let ¯ Pǫ,∞ be the limit of a weakly converging sequence.

  • Lemma. ¯

Pǫ,∞ assigns full measure to the set of the solutions to the martingale problem (MPǫ).

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SLIDE 56

Second step

The sequence

  • Pǫ := Pǫ ◦ ((xt, ut, ut − u0 −

t Bǫ[xs, us; ρǫ

s] ds); t ∈ [0, T])−1

is tight. The support of any accumulation point has full measure on the set of continuous functions ( x, u, D) of C([0, T]; R3d) satisfying

  • x(t) =

x(0) + t

  • u(s) ds, ∀ t ∈ [0, T],

and there exists a bounded function a such that sup

t∈[0,T]

  • a(t)
  • ≤ b∞,

and

  • u(t) −

u(0) − D(t) = t

  • a(s) ds, ∀ t ∈ [0, T].
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SLIDE 57

Consider the following marginal distribution P of P on C([0, T]; R2d): P = P ◦ ((xt, ut); t ∈ [0, T])−1.

  • Proposition. P solves the martingale problem (MP).

Sketch of the proof:

◮ Weak convergence (but we have to make fractions converge. . . ) ◮ Estimates by Francesco and Pascucci (2006) for ultraparabolic

PDEs .

◮ To overcome the difficulty due to the fact that Pǫ and Bǫ[· ; ρǫ]

depend on ǫ, we adapt a method designed by Stroock and Varadhan for the case of strongly elliptic diffusion processes:

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SLIDE 58

Key lemma. For all 0 < t ≤ T, ρǫ

t converges to ρt in L1(R2d) when

ǫ → 0+. Key result (Stroock & Varadhan (1979)). Let {fn; n ≥ 1} be a sequence of non–negative measurable functions such that

  • Rq fn(z) dz = 1, for all n ≥ 1. Suppose

◮ There exists a density function f such that, for all ψ ∈ Cc(Rq),

lim

n→+∞

  • Rq fn(z)ψ(z) dz =
  • Rq f(z)ψ(z) dz.

◮ For all h ∈ Rq,

lim

|h|→0 sup n∈N

  • Rq |fn(z + h) − fn(z)| dz = 0.

Then {fn} converges towards f in L1(Rq).

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SLIDE 59

Complements and perspectives

◮ Extensions to (simplified) stochastic Lagrangian models with

specular boundary conditions : see Bossy & Jabir (2008-2012).

◮ For numerical issues and an application to meteorology,

see Bossy et al. (2008-2012)).

◮ For the study of the Poisson equation, see Bossy and Fontbona

(in progress).

◮ For the full treatment of Pope’s model: a challenging problem!

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SLIDE 60

Outline

Introduction Monte Carlo Methods For Linear PDEs Discretization of Stochastic Hamiltonian Dissipative Systems Stochastic Lagrangian Models for Turbulent Flows Conclusion

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SLIDE 61

Many other problems:

◮ McKean–Vlasov systems for Navier–Stokes equations, ◮ Discretization of (reflected) backward SDEs for variational

inequalities (American options, Stefan problems),

◮ Stochastic PDEs (Gyöngy, Walsh, de Bouard–Debussche), ◮ Discretization of Hamilton–Jacobi–Belman equations for

stochastic control (Krtlov, Barles–Jakobsen),

◮ Bessel–type SDEs, ◮ Variance reduction methods (Arouna–Lapeyre,

Kebaier–Kohatsu-Higa,. . . ).