Arnold diffusion for convex nearly integrable systems V. Kaloshin - - PowerPoint PPT Presentation

arnold diffusion for convex nearly integrable systems
SMART_READER_LITE
LIVE PREVIEW

Arnold diffusion for convex nearly integrable systems V. Kaloshin - - PowerPoint PPT Presentation

Arnold diffusion for convex nearly integrable systems V. Kaloshin November 24, 2014 V. Kaloshin (University of Maryland) Arnold diffusion November 24, 2014 1 / 22 Plan of the talk Motivation: Ergodic and quasiergodic hypothesis. Nearly


slide-1
SLIDE 1

Arnold diffusion for convex nearly integrable systems

  • V. Kaloshin

November 24, 2014

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 1 / 22

slide-2
SLIDE 2

Plan of the talk

Motivation: Ergodic and quasiergodic hypothesis. Nearly integrable systems and the problem of Arnold diffusion Results in 3, 4, and more degrees of freedom Indication of Arnold diffusion in the Solar system Stochastic aspects of Arnold diffusion

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 2 / 22

slide-3
SLIDE 3

Plan of the talk

Motivation: Ergodic and quasiergodic hypothesis. Nearly integrable systems and the problem of Arnold diffusion Results in 3, 4, and more degrees of freedom Indication of Arnold diffusion in the Solar system Stochastic aspects of Arnold diffusion

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 2 / 22

slide-4
SLIDE 4

Plan of the talk

Motivation: Ergodic and quasiergodic hypothesis. Nearly integrable systems and the problem of Arnold diffusion Results in 3, 4, and more degrees of freedom Indication of Arnold diffusion in the Solar system Stochastic aspects of Arnold diffusion

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 2 / 22

slide-5
SLIDE 5

Plan of the talk

Motivation: Ergodic and quasiergodic hypothesis. Nearly integrable systems and the problem of Arnold diffusion Results in 3, 4, and more degrees of freedom Indication of Arnold diffusion in the Solar system Stochastic aspects of Arnold diffusion

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 2 / 22

slide-6
SLIDE 6

Plan of the talk

Motivation: Ergodic and quasiergodic hypothesis. Nearly integrable systems and the problem of Arnold diffusion Results in 3, 4, and more degrees of freedom Indication of Arnold diffusion in the Solar system Stochastic aspects of Arnold diffusion

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 2 / 22

slide-7
SLIDE 7

Motivation: Ergodic Hypothesis

Let H : R2n → R be a smooth function, (q, p) ∈ Rn × Rn. Let XH be the Hamiltonian flow associated to H.

  • ˙

q = ∂pH ˙ p = −∂qH (1) Let SE = {(q, p) ∈ T ∗M : H(q, p) = E} be an energy surface. Ergodic Hypothesis (Boltzmann, Maxwell) Is a generic Hamiltonian flow XH on a generic energy surface SE ergodic? Numerical doubts (Fermi-Pasta-Ulam) Chains of nonlinear springs

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 3 / 22

slide-8
SLIDE 8

Motivation: Ergodic Hypothesis

Let H : R2n → R be a smooth function, (q, p) ∈ Rn × Rn. Let XH be the Hamiltonian flow associated to H.

  • ˙

q = ∂pH ˙ p = −∂qH (1) Let SE = {(q, p) ∈ T ∗M : H(q, p) = E} be an energy surface. Ergodic Hypothesis (Boltzmann, Maxwell) Is a generic Hamiltonian flow XH on a generic energy surface SE ergodic? Numerical doubts (Fermi-Pasta-Ulam) Chains of nonlinear springs

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 3 / 22

slide-9
SLIDE 9

Motivation: Ergodic Hypothesis

Let H : R2n → R be a smooth function, (q, p) ∈ Rn × Rn. Let XH be the Hamiltonian flow associated to H.

  • ˙

q = ∂pH ˙ p = −∂qH (1) Let SE = {(q, p) ∈ T ∗M : H(q, p) = E} be an energy surface. Ergodic Hypothesis (Boltzmann, Maxwell) Is a generic Hamiltonian flow XH on a generic energy surface SE ergodic? Numerical doubts (Fermi-Pasta-Ulam) Chains of nonlinear springs

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 3 / 22

slide-10
SLIDE 10

Motivation: Ergodic Hypothesis

Let H : R2n → R be a smooth function, (q, p) ∈ Rn × Rn. Let XH be the Hamiltonian flow associated to H.

  • ˙

q = ∂pH ˙ p = −∂qH (1) Let SE = {(q, p) ∈ T ∗M : H(q, p) = E} be an energy surface. Ergodic Hypothesis (Boltzmann, Maxwell) Is a generic Hamiltonian flow XH on a generic energy surface SE ergodic? Numerical doubts (Fermi-Pasta-Ulam) Chains of nonlinear springs

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 3 / 22

slide-11
SLIDE 11

Motivation: Ergodic Hypothesis

Let H : R2n → R be a smooth function, (q, p) ∈ Rn × Rn. Let XH be the Hamiltonian flow associated to H.

  • ˙

q = ∂pH ˙ p = −∂qH Let SE = {(q, p) ∈ T ∗M : H(q, p) = E} be an energy surface. Ergodic Hypothesis (Boltzmann, Maxwell) Is a generic Hamiltonian flow XH on a generic energy surface SE ergodic? Numerical doubts (Fermi-Pasta-Ulam) Chains of nonlinear springs ¨ un = k(un+1 − un) − k(un − un−1) + α(un+1 − un)2 + α(un − un−1)2 the α-term — nonlinearity. Most “small” solutions are almost periodic!

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 4 / 22

slide-12
SLIDE 12

Motivation: Ergodic Hypothesis

Let H : R2n → R be a smooth function, (q, p) ∈ Rn × Rn. Let XH be the Hamiltonian flow associated to H.

  • ˙

q = ∂pH ˙ p = −∂qH Let SE = {(q, p) ∈ T ∗M : H(q, p) = E} be an energy surface. Ergodic Hypothesis (Boltzmann, Maxwell) Is a generic Hamiltonian flow XH on a generic energy surface SE ergodic? Numerical doubts (Fermi-Pasta-Ulam) Chains of nonlinear springs ¨ un = k(un+1 − un) − k(un − un−1) + α(un+1 − un)2 + α(un − un−1)2 the α-term — nonlinearity. Most “small” solutions are almost periodic!

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 4 / 22

slide-13
SLIDE 13

Motivation: Ergodic Hypothesis

Let H : R2n → R be a smooth function, (q, p) ∈ Rn × Rn. Let XH be the Hamiltonian flow associated to H.

  • ˙

q = ∂pH ˙ p = −∂qH Let SE = {(q, p) ∈ T ∗M : H(q, p) = E} be an energy surface. Ergodic Hypothesis (Boltzmann, Maxwell) Is a generic Hamiltonian flow XH on a generic energy surface SE ergodic? Numerical doubts (Fermi-Pasta-Ulam) Chains of nonlinear springs ¨ un = k(un+1 − un) − k(un − un−1) + α(un+1 − un)2 + α(un − un−1)2 the α-term — nonlinearity. Most “small” solutions are almost periodic!

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 4 / 22

slide-14
SLIDE 14

Quasiergodic Hypothesis

KAM theory Each nearly integrable systems has collections of invariant tori of positive measure = ⇒ no ergodicity! Quasiergodic Hypothesis (Birkhoff, Ehrenfest) Does a generic Hamiltonian flow on a generic energy surface SE have a dense orbit?

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 5 / 22

slide-15
SLIDE 15

Quasiergodic Hypothesis

KAM theory Each nearly integrable systems has collections of invariant tori of positive measure = ⇒ no ergodicity! Quasiergodic Hypothesis (Birkhoff, Ehrenfest) Does a generic Hamiltonian flow on a generic energy surface SE have a dense orbit?

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 5 / 22

slide-16
SLIDE 16

Quasiergodic Hypothesis

KAM theory Each nearly integrable systems has collections of invariant tori of positive measure = ⇒ no ergodicity! Quasiergodic Hypothesis (Birkhoff, Ehrenfest) Does a generic Hamiltonian flow on a generic energy surface SE have a dense orbit?

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 6 / 22

slide-17
SLIDE 17

Integrable systems & action-angles coordinates

Let H : R2n → R be a Hamiltonian, ϕ ∈ Tn be angle, I ∈ Rn be action. A Hamiltonian system is Arnold-Liouville integrable if for an open set U ⊂ Rn there exists a symplectic map Φ : Tn × U → R 2n s. t. H ◦ Φ(ϕ, I) depends only on I and

  • ˙

ϕ = ∂I(H ◦ Φ)(I) = ω(I), ˙ I = 0. (ϕ, I)–action-angle coordinates In particular, Φ(Tn × U) is foliated by invariant n-dim’l tori & on each torus Tn the flow is linear.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 7 / 22

slide-18
SLIDE 18

Integrable systems & action-angles coordinates

Let H : R2n → R be a Hamiltonian, ϕ ∈ Tn be angle, I ∈ Rn be action. A Hamiltonian system is Arnold-Liouville integrable if for an open set U ⊂ Rn there exists a symplectic map Φ : Tn × U → R 2n s. t. H ◦ Φ(ϕ, I) depends only on I and

  • ˙

ϕ = ∂I(H ◦ Φ)(I) = ω(I), ˙ I = 0. (ϕ, I)–action-angle coordinates In particular, Φ(Tn × U) is foliated by invariant n-dim’l tori & on each torus Tn the flow is linear.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 7 / 22

slide-19
SLIDE 19

Integrable systems & action-angles coordinates

Let H : R2n → R be a Hamiltonian, ϕ ∈ Tn be angle, I ∈ Rn be action. A Hamiltonian system is Arnold-Liouville integrable if for an open set U ⊂ Rn there exists a symplectic map Φ : Tn × U → R 2n s. t. H ◦ Φ(ϕ, I) depends only on I and

  • ˙

ϕ = ∂I(H ◦ Φ)(I) = ω(I), ˙ I = 0. (ϕ, I)–action-angle coordinates In particular, Φ(Tn × U) is foliated by invariant n-dimensional tori and

  • n each torus Tn the flow is linear.
  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 8 / 22

slide-20
SLIDE 20

Integrable systems

Newtonial two body problem. Pendulum H = I2

2 − cos 2πϕ, (ϕ, I) ∈ T ∗T = T × R.

Harmonic oscillator ¨ q = −kq or H = p2

2 + kq2 2 .

Motion in a central force field ¨ q = F(q)q. Newtonian two center problem. Lagrange’s top, Kovaleskaya’s top, Euler top. Toda lattice: chain · · · < x0 < x1 < . . . with the neighbor interaction

i exp(xi − xi+1)

Calogero-Moser system: chain of harmonic oscillators with a neighbor repulsive interaction. A geodesic flow on an n-dim’l ellipsoid with different main axes. A geodesic flow on a surface of revolution.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 9 / 22

slide-21
SLIDE 21

Integrable systems

Newtonial two body problem. Pendulum H = I2

2 − cos 2πϕ, (ϕ, I) ∈ T ∗T = T × R.

Harmonic oscillator ¨ q = −kq or H = p2

2 + kq2 2 .

Motion in a central force field ¨ q = F(q)q. Newtonian two center problem. Lagrange’s top, Kovaleskaya’s top, Euler top. Toda lattice: chain · · · < x0 < x1 < . . . with the neighbor interaction

i exp(xi − xi+1)

Calogero-Moser system: chain of harmonic oscillators with a neighbor repulsive interaction. A geodesic flow on an n-dim’l ellipsoid with different main axes. A geodesic flow on a surface of revolution.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 9 / 22

slide-22
SLIDE 22

Integrable systems

Newtonial two body problem. Pendulum H = I2

2 − cos 2πϕ, (ϕ, I) ∈ T ∗T = T × R.

Harmonic oscillator ¨ q = −kq or H = p2

2 + kq2 2 .

Motion in a central force field ¨ q = F(q)q. Newtonian two center problem. Lagrange’s top, Kovaleskaya’s top, Euler top. Toda lattice: chain · · · < x0 < x1 < . . . with the neighbor interaction

i exp(xi − xi+1)

Calogero-Moser system: chain of harmonic oscillators with a neighbor repulsive interaction. A geodesic flow on an n-dim’l ellipsoid with different main axes. A geodesic flow on a surface of revolution.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 9 / 22

slide-23
SLIDE 23

Integrable systems

Newtonial two body problem. Pendulum H = I2

2 − cos 2πϕ, (ϕ, I) ∈ T ∗T = T × R.

Harmonic oscillator ¨ q = −kq or H = p2

2 + kq2 2 .

Motion in a central force field ¨ q = F(q)q. Newtonian two center problem. Lagrange’s top, Kovaleskaya’s top, Euler top. Toda lattice: chain · · · < x0 < x1 < . . . with the neighbor interaction

i exp(xi − xi+1)

Calogero-Moser system: chain of harmonic oscillators with a neighbor repulsive interaction. A geodesic flow on an n-dim’l ellipsoid with different main axes. A geodesic flow on a surface of revolution.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 9 / 22

slide-24
SLIDE 24

Integrable systems

Newtonial two body problem. Pendulum H = I2

2 − cos 2πϕ, (ϕ, I) ∈ T ∗T = T × R.

Harmonic oscillator ¨ q = −kq or H = p2

2 + kq2 2 .

Motion in a central force field ¨ q = F(q)q. Newtonian two center problem. Lagrange’s top, Kovaleskaya’s top, Euler top. Toda lattice: chain · · · < x0 < x1 < . . . with the neighbor interaction

i exp(xi − xi+1)

Calogero-Moser system: chain of harmonic oscillators with a neighbor repulsive interaction. A geodesic flow on an n-dim’l ellipsoid with different main axes. A geodesic flow on a surface of revolution.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 9 / 22

slide-25
SLIDE 25

Integrable systems

Newtonial two body problem. Pendulum H = I2

2 − cos 2πϕ, (ϕ, I) ∈ T ∗T = T × R.

Harmonic oscillator ¨ q = −kq or H = p2

2 + kq2 2 .

Motion in a central force field ¨ q = F(q)q. Newtonian two center problem. Lagrange’s top, Kovaleskaya’s top, Euler top. Toda lattice: chain · · · < x0 < x1 < . . . with the neighbor interaction

i exp(xi − xi+1)

Calogero-Moser system: chain of harmonic oscillators with a neighbor repulsive interaction. A geodesic flow on an n-dim’l ellipsoid with different main axes. A geodesic flow on a surface of revolution.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 9 / 22

slide-26
SLIDE 26

Integrable systems

Newtonial two body problem. Pendulum H = I2

2 − cos 2πϕ, (ϕ, I) ∈ T ∗T = T × R.

Harmonic oscillator ¨ q = −kq or H = p2

2 + kq2 2 .

Motion in a central force field ¨ q = F(q)q. Newtonian two center problem. Lagrange’s top, Kovaleskaya’s top, Euler top. Toda lattice: chain · · · < x0 < x1 < . . . with the neighbor interaction

i exp(xi − xi+1)

Calogero-Moser system: chain of harmonic oscillators with a neighbor repulsive interaction. A geodesic flow on an n-dim’l ellipsoid with different main axes. A geodesic flow on a surface of revolution.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 9 / 22

slide-27
SLIDE 27

Integrable systems

Newtonial two body problem. Pendulum H = I2

2 − cos 2πϕ, (ϕ, I) ∈ T ∗T = T × R.

Harmonic oscillator ¨ q = −kq or H = p2

2 + kq2 2 .

Motion in a central force field ¨ q = F(q)q. Newtonian two center problem. Lagrange’s top, Kovaleskaya’s top, Euler top. Toda lattice: chain · · · < x0 < x1 < . . . with the neighbor interaction

i exp(xi − xi+1)

Calogero-Moser system: chain of harmonic oscillators with a neighbor repulsive interaction. A geodesic flow on an n-dim’l ellipsoid with different main axes. A geodesic flow on a surface of revolution.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 9 / 22

slide-28
SLIDE 28

Integrable systems

Newtonial two body problem. Pendulum H = I2

2 − cos 2πϕ, (ϕ, I) ∈ T ∗T = T × R.

Harmonic oscillator ¨ q = −kq or H = p2

2 + kq2 2 .

Motion in a central force field ¨ q = F(q)q. Newtonian two center problem. Lagrange’s top, Kovaleskaya’s top, Euler top. Toda lattice: chain · · · < x0 < x1 < . . . with the neighbor interaction

i exp(xi − xi+1)

Calogero-Moser system: chain of harmonic oscillators with a neighbor repulsive interaction. A geodesic flow on an n-dim’l ellipsoid with different main axes. A geodesic flow on a surface of revolution.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 9 / 22

slide-29
SLIDE 29

Integrable systems

Newtonial two body problem. Pendulum H = I2

2 − cos 2πϕ, (ϕ, I) ∈ T ∗T = T × R.

Harmonic oscillator ¨ q = −kq or H = p2

2 + kq2 2 .

Motion in a central force field ¨ q = F(q)q. Newtonian two center problem. Lagrange’s top, Kovaleskaya’s top, Euler top. Toda lattice: chain · · · < x0 < x1 < . . . with the neighbor interaction

i exp(xi − xi+1)

Calogero-Moser system: chain of harmonic oscillators with a neighbor repulsive interaction. A geodesic flow on an n-dim’l ellipsoid with different main axes. A geodesic flow on a surface of revolution.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 9 / 22

slide-30
SLIDE 30

Integrable systems

Newtonial two body problem. Pendulum H = I2

2 − cos 2πϕ, (ϕ, I) ∈ T ∗T = T × R.

Harmonic oscillator ¨ q = −kq or H = p2

2 + kq2 2 .

Motion in a central force field ¨ q = F(q)q. Newtonian two center problem. Lagrange’s top, Kovaleskaya’s top, Euler top. Toda lattice: chain · · · < x0 < x1 < . . . with the neighbor interaction

i exp(xi − xi+1)

Calogero-Moser system: chain of harmonic oscillators with a neighbor repulsive interaction. A geodesic flow on an n-dim’l ellipsoid with different main axes. A geodesic flow on a surface of revolution.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 9 / 22

slide-31
SLIDE 31

Arnold diffusion

Arnold, 63: Let (ϕ, I) ∈ T ∗Tn = Tn × Rn, t ∈ T. (weak form) Does there exist a real instability in many-dimensional problems of perturbation theory when the invariant tori do not divide the phase space? More precisely, for a generic perturbation εH1(ϕ, I, t) the Hamiltonian Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) has an orbit whose action component “travels” in action space, in particular, maxt I(t) − I(0) = O(1). (strong form) For any two open sets U, U′ ⊂ Bn the Hamiltonian Hε(ϕ, I, t) has an orbit whose action component “travels” from U to U ′, i.e. I(0) ∈ U and I(T) ∈ U ′ for some T > 0.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 10 / 22

slide-32
SLIDE 32

Arnold diffusion

Arnold, 63: Let (ϕ, I) ∈ T ∗Tn = Tn × Rn, t ∈ T. (weak form) Does there exist a real instability in many-dimensional problems of perturbation theory when the invariant tori do not divide the phase space? More precisely, for a generic perturbation εH1(ϕ, I, t) the Hamiltonian Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) has an orbit whose action component “travels” in action space, in particular, maxt I(t) − I(0) = O(1). (strong form) For any two open sets U, U′ ⊂ Bn the Hamiltonian Hε(ϕ, I, t) has an orbit whose action component “travels” from U to U ′, i.e. I(0) ∈ U and I(T) ∈ U ′ for some T > 0.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 10 / 22

slide-33
SLIDE 33

Arnold diffusion

Arnold, 63: Let (ϕ, I) ∈ T ∗Tn = Tn × Rn, t ∈ T. (weak form) Does there exist a real instability in many-dimensional problems of perturbation theory when the invariant tori do not divide the phase space? More precisely, for a generic perturbation εH1(ϕ, I, t) the Hamiltonian Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) has an orbit whose action component “travels” in action space, in particular, maxt I(t) − I(0) = O(1). (strong form) For any two open sets U, U′ ⊂ Bn the Hamiltonian Hε(ϕ, I, t) has an orbit whose action component “travels” from U to U ′, i.e. I(0) ∈ U and I(T) ∈ U ′ for some T > 0.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 10 / 22

slide-34
SLIDE 34

Nearly integrable systems in dimension 2

Let H0(I) = I 2

2 . Time one map (ϕ, I) → (ϕ + I, I) (mod 1).

Let Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t). The model time one map fε : (ϕ, I) → (ϕ′, I′) = (ϕ + I′, I + ε sin 2πϕ) (mod 1).

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 11 / 22

slide-35
SLIDE 35

Nearly integrable systems in dimension 2

Let H0(I) = I 2

2 . Time one map (ϕ, I) → (ϕ + I, I) (mod 1).

Let Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t). The model time one map fε : (ϕ, I) → (ϕ′, I′) = (ϕ + I′, I + ε sin 2πϕ) (mod 1).

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 11 / 22

slide-36
SLIDE 36

Nearly integrable systems in dimension 2

Let H0(I) = I 2

2 . Time one map (ϕ, I) → (ϕ + I, I) (mod 1).

Let Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t). The model time one map fε : (ϕ, I) → (ϕ′, I′) = (ϕ + I′, I + ε sin 2πϕ) (mod 1).

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 12 / 22

slide-37
SLIDE 37

KAM Theorem, obstacles to instability

Let H0(I) have non-degenerate Hessian, e.g. H0(I) = I2

j /2.

KAM Theorem Let Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) be a smooth

  • perturbation. Then with probability 1 − O(√ε) has an initial condition in

Tn × Bn × T having a quasiperiodic orbit. Moreover, Tn × Bn × T with certain neighborhood of rational lines deleted is laminated by invariant (n + 1)-dimensional tori, one for each diophantine ω.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 13 / 22

slide-38
SLIDE 38

KAM Theorem, obstacles to instability

Let H0(I) have non-degenerate Hessian, e.g. H0(I) = I2

j /2.

KAM Theorem Let Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) be a smooth

  • perturbation. Then with probability 1 − O(√ε) has an initial condition in

Tn × Bn × T having a quasiperiodic orbit. Moreover, Tn × Bn × T with certain neighborhood of rational lines deleted is laminated by invariant (n + 1)-dimensional tori, one for each diophantine ω.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 13 / 22

slide-39
SLIDE 39

KAM Theorem, obstacles to instability

Let H0(I) have non-degenerate Hessian, e.g. H0(I) = I2

j /2.

KAM Theorem Let Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) be a smooth

  • perturbation. Then with probability 1 − O(√ε) has an initial condition in

Tn × Bn × T having a quasiperiodic orbit. Moreover, Tn × Bn × T with certain neighborhood of rational lines deleted is laminated by invariant (n + 1)-dimensional tori, one for each diophantine ω.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 13 / 22

slide-40
SLIDE 40

The heuristic picture

In (2n + 1)-dimensional space there are (n + 1)-dimensional tori. For n = 1 they confine orbits! For n > 1 they do not!

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 14 / 22

slide-41
SLIDE 41

The heuristic picture

In (2n + 1)-dimensional space there are (n + 1)-dimensional tori. For n = 1 they confine orbits! For n > 1 they do not!

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 14 / 22

slide-42
SLIDE 42

The heuristic picture

In (2n + 1)-dimensional space there are (n + 1)-dimensional tori. For n = 1 they confine orbits! For n > 1 they do not!

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 14 / 22

slide-43
SLIDE 43

A strong from of Arnold diffusion

Let H0(I) be smooth and strictly convex, I ∈ Bn. The First Main Result For any γ > 0 & a generic smooth perturbation εH1(φ, I, t) the Hamiltonian Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) has an orbit (ϕε, Iε, t)(t) which is γ-dense in Tn × Bn × T. Namely, γ-neighbourhood of ∪t (ϕε, Iε, t)(t) contains Tn × Bn × T. [K-Zhang, 12] n=2 (arxiv) In 2002 a version of this result was announced by Mather. There is an annoucement of Cheng. [K-Zhang, 14] n=3 (my webpage) [K-Zhang, 14] n > 3, progress (arxiv)

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 15 / 22

slide-44
SLIDE 44

A strong from of Arnold diffusion

Let H0(I) be smooth and strictly convex, I ∈ Bn. The First Main Result For any γ > 0 & a generic smooth perturbation εH1(φ, I, t) the Hamiltonian Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) has an orbit (ϕε, Iε, t)(t) which is γ-dense in Tn × Bn × T. Namely, γ-neighbourhood of ∪t (ϕε, Iε, t)(t) contains Tn × Bn × T. [K-Zhang, 12] n=2 (arxiv) In 2002 a version of this result was announced by Mather. There is an annoucement of Cheng. [K-Zhang, 14] n=3 (my webpage) [K-Zhang, 14] n > 3, progress (arxiv)

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 15 / 22

slide-45
SLIDE 45

A strong from of Arnold diffusion

Let H0(I) be smooth and strictly convex, I ∈ Bn. The First Main Result For any γ > 0 & a generic smooth perturbation εH1(φ, I, t) the Hamiltonian Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) has an orbit (ϕε, Iε, t)(t) which is γ-dense in Tn × Bn × T. Namely, γ-neighbourhood of ∪t (ϕε, Iε, t)(t) contains Tn × Bn × T. [K-Zhang, 12] n=2 (arxiv) In 2002 a version of this result was announced by Mather. There is an annoucement of Cheng. [K-Zhang, 14] n=3 (my webpage) [K-Zhang, 14] n > 3, progress (arxiv)

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 15 / 22

slide-46
SLIDE 46

A strong from of Arnold diffusion

Let H0(I) be smooth and strictly convex, I ∈ Bn. The First Main Result For any γ > 0 & a generic smooth perturbation εH1(φ, I, t) the Hamiltonian Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) has an orbit (ϕε, Iε, t)(t) which is γ-dense in Tn × Bn × T. Namely, γ-neighbourhood of ∪t (ϕε, Iε, t)(t) contains Tn × Bn × T. [K-Zhang, 12] n=2 (arxiv) In 2002 a version of this result was announced by Mather. There is an annoucement of Cheng. [K-Zhang, 14] n=3 (my webpage) [K-Zhang, 14] n > 3, progress (arxiv)

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 15 / 22

slide-47
SLIDE 47

A strong from of Arnold diffusion

Let H0(I) be smooth and strictly convex, I ∈ Bn. The First Main Result For any γ > 0 & a generic smooth perturbation εH1(φ, I, t) the Hamiltonian Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) has an orbit (ϕε, Iε, t)(t) which is γ-dense in Tn × Bn × T. Namely, γ-neighbourhood of ∪t (ϕε, Iε, t)(t) contains Tn × Bn × T. [K-Zhang, 12] n=2 (arxiv) In 2002 a version of this result was announced by Mather. There is an annoucement of Cheng. [K-Zhang, 14] n=3 (my webpage) [K-Zhang, 14] n > 3, progress (arxiv)

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 15 / 22

slide-48
SLIDE 48

A strong from of Arnold diffusion

Let H0(I) be smooth and strictly convex, I ∈ Bn. The First Main Result For any γ > 0 & a generic smooth perturbation εH1(φ, I, t) the Hamiltonian Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) has an orbit (ϕε, Iε, t)(t) which is γ-dense in Tn × Bn × T. Namely, γ-neighbourhood of ∪t (ϕε, Iε, t)(t) contains Tn × Bn × T. [K-Zhang, 12] n=2 (arxiv) In 2002 a version of this result was announced by Mather. There is an annoucement of Cheng. [K-Zhang, 14] n=3 (my webpage) [K-Zhang, 14] n > 3, progress (arxiv)

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 15 / 22

slide-49
SLIDE 49

A weak form of quasiergodic hypothesis

Let H0(I) be smooth and strictly convex, I ∈ B2. The Second Main Result [Guardia-K] For any γ > 0 & a dense set of perturbations εH1 the Hamiltonian Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) has an orbit (ϕε, Iε, t)(t) accumulating to all KAM tori and, therefore, Leb

  • ∪t(ϕε, Iε, t)(t)
  • Leb{T2 × B2 × T}

> 1 − γ. A weak form of Quasiergodict hypothesis: there exists an orbit dense in a set of almost maximal measure. Byproduct: KAM tori are Lyapunov unstable!

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 16 / 22

slide-50
SLIDE 50

A weak form of quasiergodic hypothesis

Let H0(I) be smooth and strictly convex, I ∈ B2. The Second Main Result [Guardia-K] For any γ > 0 & a dense set of perturbations εH1 the Hamiltonian Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) has an orbit (ϕε, Iε, t)(t) accumulating to all KAM tori and, therefore, Leb

  • ∪t(ϕε, Iε, t)(t)
  • Leb{T2 × B2 × T}

> 1 − γ. A weak form of Quasiergodict hypothesis: there exists an orbit dense in a set of almost maximal measure. Byproduct: KAM tori are Lyapunov unstable!

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 16 / 22

slide-51
SLIDE 51

A weak form of quasiergodic hypothesis

Let H0(I) be smooth and strictly convex, I ∈ B2. The Second Main Result [Guardia-K] For any γ > 0 & a dense set of perturbations εH1 the Hamiltonian Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) has an orbit (ϕε, Iε, t)(t) accumulating to all KAM tori and, therefore, Leb

  • ∪t(ϕε, Iε, t)(t)
  • Leb{T2 × B2 × T}

> 1 − γ. A weak form of Quasiergodict hypothesis: there exists an orbit dense in a set of almost maximal measure. Byproduct: KAM tori are Lyapunov unstable!

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 16 / 22

slide-52
SLIDE 52

A weak form of quasiergodic hypothesis

Let H0(I) be smooth and strictly convex, I ∈ B2. The Second Main Result [Guardia-K] For any γ > 0 & a dense set of perturbations εH1 the Hamiltonian Hε(ϕ, I, t) = H0(I) + εH1(ϕ, I, t) has an orbit (ϕε, Iε, t)(t) accumulating to all KAM tori and, therefore, Leb

  • ∪t(ϕε, Iε, t)(t)
  • Leb{T2 × B2 × T}

> 1 − γ. A weak form of Quasiergodict hypothesis: there exists an orbit dense in a set of almost maximal measure. Byproduct: KAM tori are Lyapunov unstable!

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 16 / 22

slide-53
SLIDE 53

Instabilities in the Asteroid Belt

.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 17 / 22

slide-54
SLIDE 54

Instabilities in the Asteroid Belt

  • J. Wisdom,83, Chaotic Behavior & the Origin of the 3/1 Kirkwood Gaps

Fejoz-Guardia-K-Roldan (to appear in J of the EMS) Unstable orbits exist in the 3 : 1 Kirkwood gap.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 18 / 22

slide-55
SLIDE 55

Instabilities in the Asteroid Belt

  • J. Wisdom,83, Chaotic Behavior & the Origin of the 3/1 Kirkwood Gaps

Fejoz-Guardia-K-Roldan (to appear in J of the EMS) Unstable orbits exist in the 3 : 1 Kirkwood gap.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 18 / 22

slide-56
SLIDE 56

Instabilities in the Asteroid Belt

  • J. Wisdom,83, Chaotic Behavior & the Origin of the 3/1 Kirkwood Gaps

Fejoz-Guardia-K-Roldan (to appear in J of the EMS) Unstable orbits exist in the 3 : 1 Kirkwood gap.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 18 / 22

slide-57
SLIDE 57

Diffusion conjecture for Arnold’s example

Diffusion conjecture Let

Hε = I2 2

  • harm oscillator

+ p2 2 + cos q

  • pendulum

+εH1(ϕ, I, q, p, t), ϕ, q, t ∈ T, I, p ∈ R,

where H1 is a generic perturbation. Let Lebε be the norm Lebesgue measure on the √ε-ball around 0. Then I( −t·ln ε

ε2

) converges to a diffusion process wrt Leb√ε. Chirikov, ... , Guzzo

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 19 / 22

slide-58
SLIDE 58

Diffusion conjecture for Arnold’s example

Diffusion conjecture Let

Hε = I2 2

  • harm oscillator

+ p2 2 + cos q

  • pendulum

+εH1(ϕ, I, q, p, t), ϕ, q, t ∈ T, I, p ∈ R,

where H1 is a generic perturbation. Let Lebε be the norm Lebesgue measure on the √ε-ball around 0. Then I( −t·ln ε

ε2

) converges to a diffusion process wrt Leb√ε. Chirikov, ... , Guzzo

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 19 / 22

slide-59
SLIDE 59

Stochastic Aspects of Arnold diffusion

Model Problem Let f0 : (ϕ, I) → (ϕ + I + ε cos ϕ, I + ε cos ϕ), f1 : (ϕ, I) → (ϕ + I + ε sin ϕ, I + ε sin ϕ), be a pair of standard maps. Consider random composition of these maps fωn ◦ fωn−1 ◦ · · · ◦ fω1(ϕ0, I0) = (ϕn, In). Theorem (joint work with O. Castejon) For n ∼ ε−2 such compositions satisfy the Central Limit Theorem, i.e. In − I0 → N(0, σ), where N(0, σ) is a normal random variable with some variance σ > 0.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 20 / 22

slide-60
SLIDE 60

Stochastic Aspects of Arnold diffusion

Model Problem Let f0 : (ϕ, I) → (ϕ + I + ε cos ϕ, I + ε cos ϕ), f1 : (ϕ, I) → (ϕ + I + ε sin ϕ, I + ε sin ϕ), be a pair of standard maps. Consider random composition of these maps fωn ◦ fωn−1 ◦ · · · ◦ fω1(ϕ0, I0) = (ϕn, In). Theorem (joint work with O. Castejon) For n ∼ ε−2 such compositions satisfy the Central Limit Theorem, i.e. In − I0 → N(0, σ), where N(0, σ) is a normal random variable with some variance σ > 0.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 20 / 22

slide-61
SLIDE 61

Stochastic Aspects of Arnold diffusion

Model Problem Let f0 : (ϕ, I) → (ϕ + I + ε cos ϕ, I + ε cos ϕ), f1 : (ϕ, I) → (ϕ + I + ε sin ϕ, I + ε sin ϕ), be a pair of standard maps. Consider random composition of these maps fωn ◦ fωn−1 ◦ · · · ◦ fω1(ϕ0, I0) = (ϕn, In). Theorem (joint work with O. Castejon) For n ∼ ε−2 such compositions satisfy the Central Limit Theorem, i.e. In − I0 → N(0, σ), where N(0, σ) is a normal random variable with some variance σ > 0.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 20 / 22

slide-62
SLIDE 62

Stochastic Aspects of Arnold diffusion

Model Problem Let f0 : (ϕ, I) → (ϕ + I + ε cos ϕ, I + ε cos ϕ), f1 : (ϕ, I) → (ϕ + I + ε sin ϕ, I + ε sin ϕ), be a pair of standard maps. Consider random composition of these maps fωn ◦ fωn−1 ◦ · · · ◦ fω1(ϕ0, I0) = (ϕn, In). Theorem (joint work with O. Castejon) For n ∼ ε−2 such compositions satisfy the Central Limit Theorem, i.e. In − I0 → N(0, σ), where N(0, σ) is a normal random variable with some variance σ > 0.

  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 20 / 22

slide-63
SLIDE 63

Diffusion mechanism

(Ma˜ n´ e 90s) periodic orbit1 periodic orbit2 periodic orbit3 . . . (Arnold, Gallavotti, Lochak, ... 60s-80s) whiskered KAM torus 1 whiskered KAM torus2 whiskered KAM torus3 . . . (Mather, Bernard, Cheng 90-00s) Cantor torus1 Cantor torus2 Cantor torus3 . . . Find invariant sets inside Normally Hyperbolic Invariant Cylinders

  • w. transverse invariant manifolds
  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 21 / 22

slide-64
SLIDE 64

Diffusion mechanism

(Ma˜ n´ e 90s) periodic orbit1 periodic orbit2 periodic orbit3 . . . (Arnold, Gallavotti, Lochak, ... 60s-80s) whiskered KAM torus 1 whiskered KAM torus2 whiskered KAM torus3 . . . (Mather, Bernard, Cheng 90-00s) Cantor torus1 Cantor torus2 Cantor torus3 . . . Find invariant sets inside Normally Hyperbolic Invariant Cylinders

  • w. transverse invariant manifolds
  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 21 / 22

slide-65
SLIDE 65

Diffusion mechanism

(Ma˜ n´ e 90s) periodic orbit1 periodic orbit2 periodic orbit3 . . . (Arnold, Gallavotti, Lochak, ... 60s-80s) whiskered KAM torus 1 whiskered KAM torus2 whiskered KAM torus3 . . . (Mather, Bernard, Cheng 90-00s) Cantor torus1 Cantor torus2 Cantor torus3 . . . Find invariant sets inside Normally Hyperbolic Invariant Cylinders

  • w. transverse invariant manifolds
  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 21 / 22

slide-66
SLIDE 66

Diffusion mechanism

(Ma˜ n´ e 90s) periodic orbit1 periodic orbit2 periodic orbit3 . . . (Arnold, Gallavotti, Lochak, ... 60s-80s) whiskered KAM torus 1 whiskered KAM torus2 whiskered KAM torus3 . . . (Mather, Bernard, Cheng 90-00s) Cantor torus1 Cantor torus2 Cantor torus3 . . . Find invariant sets inside Normally Hyperbolic Invariant Cylinders

  • w. transverse invariant manifolds
  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 21 / 22

slide-67
SLIDE 67

Diffusion mechanism

(Ma˜ n´ e 90s) periodic orbit1 periodic orbit2 periodic orbit3 . . . (Arnold, Gallavotti, Lochak, ... 60s-80s) whiskered KAM torus 1 whiskered KAM torus2 whiskered KAM torus3 . . . (Mather, Bernard, Cheng 90-00s) Cantor torus1 Cantor torus2 Cantor torus3 . . . Find invariant sets inside Normally Hyperbolic Invariant Cylinders

  • w. transverse invariant manifolds
  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 21 / 22

slide-68
SLIDE 68

Preprints contributing to the talk

P . Bernard., V. Kaloshin, K. Zhang, Arnold diffusion in arbitrary degrees of freedom and crumpled 3-dimensional normally hyperbolic invariant cylinders, arXiv:1112.2773v Dec 2011, 58pp.

  • V. Kaloshin, K. Zhang, A strong form of Arnold diffusion for two

and a half degrees of freedom, arXiv:1212.1150 [math.DS] Dec 2012, 208pp.;

  • J. Fejoz, M. Guardia, V. Kaloshin, P

. Roldan, Kirkwood gaps and diffusion along mean motion resonances in the restricted planar three-body problem, to appear in J of European Math Soc.

  • V. Kaloshin, K. Zhang, Arnold diffusion for three and a half

degrees of freedom, April 2014, 25pp.;

  • V. Kaloshin, K. Zhang, Dynamics of the dominant Hamiltonian,

with applications to Arnold diffusion, October 2014, 75pp.;

  • M. Guardia, V. Kaloshin, Orbits of nearly integrable systems

accumulating to KAM tori, preprint, 2014, 112pp. .

  • O. Castejon, V. Kaloshin, Random iteration of cylinder maps,
  • V. Kaloshin (University of Maryland)

Arnold diffusion November 24, 2014 22 / 22