Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In...

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Cold planar horizons are floppy Cold planar horizons are floppy Jorge E. Santos New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1 / 15

Transcript of Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In...

Page 1: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Cold planar horizons are floppy

Jorge E. SantosNew frontiers in dynamical gravity

In collaboration withSean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612

1 / 15

Page 2: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Motivation

The AdS/CFT correspondence maps asymptotically AdS solutions ofEinsteins’ equations to states of a dual conformal field theory.

Near horizon geometries of AdS black holes describe the low energydissipative dynamics of strongly interacting QFTs.

Near horizon geometries of extremal planar black holes capture thedissipative dynamics of novel phases of T = 0 quantum matter.

Extensive classification exists for translational invariant systems.

A more realistic model needs to account for a ubiquitous property ofCMT systems:

What this talk is not:

∂x is broken explicitly in all matter sectors.

For other setups recall Jerome’s talk.

What I am going to describe doesn’t happen in such setups.

2 / 15

Page 3: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Motivation

The AdS/CFT correspondence maps asymptotically AdS solutions ofEinsteins’ equations to states of a dual conformal field theory.

Near horizon geometries of AdS black holes describe the low energydissipative dynamics of strongly interacting QFTs.

Near horizon geometries of extremal planar black holes capture thedissipative dynamics of novel phases of T = 0 quantum matter.

Extensive classification exists for translational invariant systems.

A more realistic model needs to account for a ubiquitous property ofCMT systems: breaking translational invariance.

What this talk is not:

∂x is broken explicitly in all matter sectors.

For other setups recall Jerome’s talk.

What I am going to describe doesn’t happen in such setups.

2 / 15

Page 4: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Motivation

The AdS/CFT correspondence maps asymptotically AdS solutions ofEinsteins’ equations to states of a dual conformal field theory.

Near horizon geometries of AdS black holes describe the low energydissipative dynamics of strongly interacting QFTs.

Near horizon geometries of extremal planar black holes capture thedissipative dynamics of novel phases of T = 0 quantum matter.

Extensive classification exists for translational invariant systems.

A more realistic model needs to account for a ubiquitous property ofCMT systems: breaking translational invariance.

What this talk is not:

∂x is broken explicitly in all matter sectors.

For other setups recall Jerome’s talk.

What I am going to describe doesn’t happen in such setups.

2 / 15

Page 5: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Motivation

The AdS/CFT correspondence maps asymptotically AdS solutions ofEinsteins’ equations to states of a dual conformal field theory.

Near horizon geometries of AdS black holes describe the low energydissipative dynamics of strongly interacting QFTs.

Near horizon geometries of extremal planar black holes capture thedissipative dynamics of novel phases of T = 0 quantum matter.

Extensive classification exists for translational invariant systems.

A more realistic model needs to account for a ubiquitous property ofCMT systems: breaking translational invariance.

What this talk is not:

∂x is broken explicitly in all matter sectors.

For other setups recall Jerome’s talk.

What I am going to describe doesn’t happen in such setups.

2 / 15

Page 6: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Motivation

The AdS/CFT correspondence maps asymptotically AdS solutions ofEinsteins’ equations to states of a dual conformal field theory.

Near horizon geometries of AdS black holes describe the low energydissipative dynamics of strongly interacting QFTs.

Near horizon geometries of extremal planar black holes capture thedissipative dynamics of novel phases of T = 0 quantum matter.

Extensive classification exists for translational invariant systems.

A more realistic model needs to account for a ubiquitous property ofCMT systems: breaking translational invariance.

What this talk is not:

∂x is broken explicitly in all matter sectors.

For other setups recall Jerome’s talk.

What I am going to describe doesn’t happen in such setups.

2 / 15

Page 7: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Motivation

The AdS/CFT correspondence maps asymptotically AdS solutions ofEinsteins’ equations to states of a dual conformal field theory.

Near horizon geometries of AdS black holes describe the low energydissipative dynamics of strongly interacting QFTs.

Near horizon geometries of extremal planar black holes capture thedissipative dynamics of novel phases of T = 0 quantum matter.

Extensive classification exists for translational invariant systems.

A more realistic model needs to account for a ubiquitous property ofCMT systems: breaking translational invariance.

What this talk is not:

∂x is broken explicitly in all matter sectors.

For other setups recall Jerome’s talk.

What I am going to describe doesn’t happen in such setups.

2 / 15

Page 8: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Motivation

The AdS/CFT correspondence maps asymptotically AdS solutions ofEinsteins’ equations to states of a dual conformal field theory.

Near horizon geometries of AdS black holes describe the low energydissipative dynamics of strongly interacting QFTs.

Near horizon geometries of extremal planar black holes capture thedissipative dynamics of novel phases of T = 0 quantum matter.

Extensive classification exists for translational invariant systems.

A more realistic model needs to account for a ubiquitous property ofCMT systems: breaking translational invariance.

What this talk is not:

∂x is broken explicitly in all matter sectors.

For other setups recall Jerome’s talk.

What I am going to describe doesn’t happen in such setups.

2 / 15

Page 9: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Motivation

The AdS/CFT correspondence maps asymptotically AdS solutions ofEinsteins’ equations to states of a dual conformal field theory.

Near horizon geometries of AdS black holes describe the low energydissipative dynamics of strongly interacting QFTs.

Near horizon geometries of extremal planar black holes capture thedissipative dynamics of novel phases of T = 0 quantum matter.

Extensive classification exists for translational invariant systems.

A more realistic model needs to account for a ubiquitous property ofCMT systems: breaking translational invariance.

What this talk is not:

∂x is broken explicitly in all matter sectors.

For other setups recall Jerome’s talk.

What I am going to describe doesn’t happen in such setups.

2 / 15

Page 10: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Motivation

The AdS/CFT correspondence maps asymptotically AdS solutions ofEinsteins’ equations to states of a dual conformal field theory.

Near horizon geometries of AdS black holes describe the low energydissipative dynamics of strongly interacting QFTs.

Near horizon geometries of extremal planar black holes capture thedissipative dynamics of novel phases of T = 0 quantum matter.

Extensive classification exists for translational invariant systems.

A more realistic model needs to account for a ubiquitous property ofCMT systems: breaking translational invariance.

What this talk is not:

∂x is broken explicitly in all matter sectors.

For other setups recall Jerome’s talk.

What I am going to describe doesn’t happen in such setups.2 / 15

Page 11: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Outline

1 The Einstein-Maxwell system

2 Breakdown of Perturbation theory

3 Zero Temperature Numerics

4 Results

5 What about AdS4?

6 Conclusion & Outlook

3 / 15

Page 12: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

The Einstein-Maxwell system

The bulk theory we study is governed by the Lagrangian

S =1

16πGd

∫ddx√−g[R+

(d− 1)(d− 2)

L2− 1

2F abFab

],

where F = dA and L is the AdSd length scale.

Comments:

Field content: gravity and Maxwell field

Consider solutions in the Poincare patch with fixed boundarymetric

ds2∂ = −dt2 + dx2 + dw2

Translational invariance is explicitly broken via the boundarybehaviour of At:

At(x,w, y) = µ(x,w) + 〈ρ(x,w)〉 y + . . .

Focus on d = 4, with µ(x) = µ [1 +A0 cos(kLx)].

Moduli space space of solutions is 2D: A0 and k0 ≡ kL/µ.

4 / 15

Page 13: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

The Einstein-Maxwell system

The bulk theory we study is governed by the Lagrangian

S =1

16πGd

∫ddx√−g[R+

(d− 1)(d− 2)

L2− 1

2F abFab

],

where F = dA and L is the AdSd length scale.

Comments:

Field content: gravity and Maxwell field

Consider solutions in the Poincare patch with fixed boundarymetric

ds2∂ = −dt2 + dx2 + dw2

Translational invariance is explicitly broken via the boundarybehaviour of At:

At(x,w, y) = µ(x,w) + 〈ρ(x,w)〉 y + . . .

Focus on d = 4, with µ(x) = µ [1 +A0 cos(kLx)].

Moduli space space of solutions is 2D: A0 and k0 ≡ kL/µ.

4 / 15

Page 14: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

The Einstein-Maxwell system

The bulk theory we study is governed by the Lagrangian

S =1

16πGd

∫ddx√−g[R+

(d− 1)(d− 2)

L2− 1

2F abFab

],

where F = dA and L is the AdSd length scale.

Comments:

Field content: gravity and Maxwell field

Consider solutions in the Poincare patch with fixed boundarymetric

ds2∂ = −dt2 + dx2 + dw2

Translational invariance is explicitly broken via the boundarybehaviour of At:

At(x,w, y) = µ(x,w) + 〈ρ(x,w)〉 y + . . .

Focus on d = 4, with µ(x) = µ [1 +A0 cos(kLx)].

Moduli space space of solutions is 2D: A0 and k0 ≡ kL/µ.

4 / 15

Page 15: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

The Einstein-Maxwell system

The bulk theory we study is governed by the Lagrangian

S =1

16πGd

∫ddx√−g[R+

(d− 1)(d− 2)

L2− 1

2F abFab

],

where F = dA and L is the AdSd length scale.

Comments:

Field content: gravity and Maxwell field

Consider solutions in the Poincare patch with fixed boundarymetric

ds2∂ = −dt2 + dx2 + dw2

Translational invariance is explicitly broken via the boundarybehaviour of At:

At(x,w, y) = µ(x,w) + 〈ρ(x,w)〉 y + . . .

Focus on d = 4, with µ(x) = µ [1 +A0 cos(kLx)].

Moduli space space of solutions is 2D: A0 and k0 ≡ kL/µ.

4 / 15

Page 16: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

The Einstein-Maxwell system

The bulk theory we study is governed by the Lagrangian

S =1

16πGd

∫ddx√−g[R+

(d− 1)(d− 2)

L2− 1

2F abFab

],

where F = dA and L is the AdSd length scale.

Comments:

Field content: gravity and Maxwell field

Consider solutions in the Poincare patch with fixed boundarymetric

ds2∂ = −dt2 + dx2 + dw2

Translational invariance is explicitly broken via the boundarybehaviour of At:

At(x,w, y) = µ(x,w) + 〈ρ(x,w)〉 y + . . .

Focus on d = 4, with µ(x) = µ [1 +A0 cos(kLx)].

Moduli space space of solutions is 2D: A0 and k0 ≡ kL/µ.

4 / 15

Page 17: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

The Einstein-Maxwell system

The bulk theory we study is governed by the Lagrangian

S =1

16πGd

∫ddx√−g[R+

(d− 1)(d− 2)

L2− 1

2F abFab

],

where F = dA and L is the AdSd length scale.

Comments:

Field content: gravity and Maxwell field

Consider solutions in the Poincare patch with fixed boundarymetric

ds2∂ = −dt2 + dx2 + dw2

Translational invariance is explicitly broken via the boundarybehaviour of At:

At(x,w, y) = µ(x,w) + 〈ρ(x,w)〉 y + . . .

Focus on d = 4, with µ(x) = µ [1 +A0 cos(kLx)].

Moduli space space of solutions is 2D: A0 and k0 ≡ kL/µ.

4 / 15

Page 18: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

The Einstein-Maxwell system

The bulk theory we study is governed by the Lagrangian

S =1

16πGd

∫ddx√−g[R+

(d− 1)(d− 2)

L2− 1

2F abFab

],

where F = dA and L is the AdSd length scale.

Comments:

Field content: gravity and Maxwell field

Consider solutions in the Poincare patch with fixed boundarymetric

ds2∂ = −dt2 + dx2 + dw2

Translational invariance is explicitly broken via the boundarybehaviour of At:

At(x,w, y) = µ(x,w) + 〈ρ(x,w)〉 y + . . .

Focus on d = 4, with µ(x) = µ [1 +A0 cos(kLx)].

Moduli space space of solutions is 2D: A0 and k0 ≡ kL/µ.

4 / 15

Page 19: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

An infamous solution:

Study time independent perturbations of extremal RN:

ds2 =L2

y2

[−G(y)(1− y)2dt2 +

dy2

G(y)(1− y)2+ dx2 + dw2

],

A = L√

6 (1− y)dt ,(1)

with G(y) = 1 + 2y + 3y2 and δAt(0, x) = L√

6A0 cos(kLx).

Possible to do analytically, but not illuminating.

Instead, take near horizon limit:

t = τ/ε , y = 1− ερ/6 with ε→ 0.

Brings line element (1) to

ds2 = L2

[1

6

(−ρ2dτ2 +

dρ2

ρ2

)+ dx2 + dw2

],

A =Lρ√

6dτ .

5 / 15

Page 20: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

An infamous solution:

Study time independent perturbations of extremal RN:

ds2 =L2

y2

[−G(y)(1− y)2dt2 +

dy2

G(y)(1− y)2+ dx2 + dw2

],

A = L√

6 (1− y)dt ,

with G(y) = 1 + 2y + 3y2 and δAt(0, x) = L√

6A0 cos(kLx).

Possible to do analytically, but not illuminating.

Instead, take near horizon limit:

t = τ/ε , y = 1− ερ/6 with ε→ 0.

Brings line element (1) to

ds2 = L2

[1

6

(−ρ2dτ2 +

dρ2

ρ2

)+ dx2 + dw2

],

A =Lρ√

6dτ .

5 / 15

Page 21: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

An infamous solution:

Study time independent perturbations of extremal RN:

ds2 =L2

y2

[−G(y)(1− y)2dt2 +

dy2

G(y)(1− y)2+ dx2 + dw2

],

A = L√

6 (1− y)dt ,

with G(y) = 1 + 2y + 3y2 and δAt(0, x) = L√

6A0 cos(kLx).

Possible to do analytically, but not illuminating.

Instead, take near horizon limit:

t = τ/ε , y = 1− ερ/6 with ε→ 0.

Brings line element (1) to

ds2 = L2

[1

6

(−ρ2dτ2 +

dρ2

ρ2

)+ dx2 + dw2

],

A =Lρ√

6dτ .

5 / 15

Page 22: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

An infamous solution:

Study time independent perturbations of extremal RN:

ds2 =L2

y2

[−G(y)(1− y)2dt2 +

dy2

G(y)(1− y)2+ dx2 + dw2

],

A = L√

6 (1− y)dt ,

with G(y) = 1 + 2y + 3y2 and δAt(0, x) = L√

6A0 cos(kLx).

Possible to do analytically, but not illuminating.

Instead, take near horizon limit:

t = τ/ε , y = 1− ερ/6 with ε→ 0.

Brings line element (1) to

ds2 = L2

[1

6

(−ρ2dτ2 +

dρ2

ρ2

)+ dx2 + dw2

],

A =Lρ√

6dτ .

5 / 15

Page 23: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

An infamous solution:

Study time independent perturbations of extremal RN:

ds2 =L2

y2

[−G(y)(1− y)2dt2 +

dy2

G(y)(1− y)2+ dx2 + dw2

],

A = L√

6 (1− y)dt ,(1)

with G(y) = 1 + 2y + 3y2 and δAt(0, x) = L√

6A0 cos(kLx).

Possible to do analytically, but not illuminating.

Instead, take near horizon limit:

t = τ/ε , y = 1− ερ/6 with ε→ 0.

Brings line element (1) to

ds2 = L2

[1

6

(−ρ2dτ2 +

dρ2

ρ2

)+ dx2 + dw2

],

A =Lρ√

6dτ .

5 / 15

Page 24: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

Dream:

Study finite size time independent perturbations about pureAdS2 × R2 - if a breakdown occurs, likely to be universal, since it

only depends on near horizon geometry.

Start with AdS2 × R2 written in Poincare-like coordinates

ds2 =

(−2dτ2 +

d2

2

)+ L2dx2 + L2dw2 and A = dτ

where L2 ≡ L/√

6, and ρ = 0 is the horizon location.

Solve for the Kodama-Ishibashi variable:

Third order Kodama-Ishibashi variable grows faster than first order:

Φ(3)− (ρ, x) = . . .+ β(ν−) δL2 ρ

ν−(kL) log ρ cos(kLx) + . . .

Breakdown of perturbation theory - resumm perturbation theory.

6 / 15

Page 25: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

Dream:

Study finite size time independent perturbations about pureAdS2 × R2 - if a breakdown occurs, likely to be universal, since it

only depends on near horizon geometry.

Start with AdS2 × R2 written in Poincare-like coordinates

ds2 = L22

(−ρ2dτ2 +

dρ2

ρ2

)+L2dx2 +L2dw2 and A = L2 ρ dτ .

where L2 ≡ L/√

6, and ρ = 0 is the horizon location.

Solve for the Kodama-Ishibashi variable:

Third order Kodama-Ishibashi variable grows faster than first order:

Φ(3)− (ρ, x) = . . .+ β(ν−) δL2 ρ

ν−(kL) log ρ cos(kLx) + . . .

Breakdown of perturbation theory - resumm perturbation theory.

6 / 15

Page 26: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

Dream:

Study finite size time independent perturbations about pureAdS2 × R2 - if a breakdown occurs, likely to be universal, since it

only depends on near horizon geometry.

Start with AdS2 × R2 written in Poincare-like coordinates

ds2 = L22

(−ρ2dτ2 +

dρ2

ρ2

)+L2dx2 +L2dw2 and A = L2 ρ dτ ,

where L2 ≡ L/√

6, and ρ = 0 is the horizon location.

Solve for the Kodama-Ishibashi variable:

Third order Kodama-Ishibashi variable grows faster than first order:

Φ(3)− (ρ, x) = . . .+ β(ν−) δL2 ρ

ν−(kL) log ρ cos(kLx) + . . .

Breakdown of perturbation theory - resumm perturbation theory.

6 / 15

Page 27: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

Dream:

Study finite size time independent perturbations about pureAdS2 × R2 - if a breakdown occurs, likely to be universal, since it

only depends on near horizon geometry.

Start with AdS2 × R2 written in Poincare-like coordinates

ds2 = L22

(−ρ2dτ2 +

dρ2

ρ2

)+L2dx2 +L2dw2 and A = L2 ρ dτ ,

where L2 ≡ L/√

6, and ρ = 0 is the horizon location.Solve for the Kodama-Ishibashi variable:

Φ(1)− (ρ, x) = γ cos(kLx)ρν−(kL) where

ν−(kL) =

√√√√(1

2−√k2L3

+ 1

)2

−k2L6− 1

2> 0 .

Third order Kodama-Ishibashi variable grows faster than first order:

Φ(3)− (ρ, x) = . . .+ β(ν−) δL2 ρ

ν−(kL) log ρ cos(kLx) + . . .

Breakdown of perturbation theory - resumm perturbation theory.

6 / 15

Page 28: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

Dream:

Study finite size time independent perturbations about pureAdS2 × R2 - if a breakdown occurs, likely to be universal, since it

only depends on near horizon geometry.

Start with AdS2 × R2 written in Poincare-like coordinates

ds2 = L22

(−ρ2dτ2 +

dρ2

ρ2

)+L2dx2 +L2dw2 and A = L2 ρ dτ ,

where L2 ≡ L/√

6, and ρ = 0 is the horizon location.Solve for the Kodama-Ishibashi variable:

Φ(1)− (ρ, x) = γ cos(kLx)ρν−(kL) .

Third order Kodama-Ishibashi variable grows faster than first order:

Φ(3)− (ρ, x) = . . .+ β(ν−) δL2 ρ

ν−(kL) log ρ cos(kLx) + . . .

Breakdown of perturbation theory - resumm perturbation theory.

6 / 15

Page 29: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

Dream:

Study finite size time independent perturbations about pureAdS2 × R2 - if a breakdown occurs, likely to be universal, since it

only depends on near horizon geometry.

Start with AdS2 × R2 written in Poincare-like coordinates

ds2 = L22

(−ρ2dτ2 +

dρ2

ρ2

)+L2dx2 +L2dw2 and A = L2 ρ dτ ,

where L2 ≡ L/√

6, and ρ = 0 is the horizon location.Solve for the Kodama-Ishibashi variable:

Φ(1)− (ρ, x) = γ cos(kLx)ρν−(kL) .

Third order Kodama-Ishibashi variable grows faster than first order:

Φ(3)− (ρ, x) = . . .+ β(ν−) δL2 ρ

ν−(kL) log ρ cos(kLx) + . . .

Breakdown of perturbation theory - resumm perturbation theory.

6 / 15

Page 30: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

A tale of two resummations:

Preserving AdS2 × R2:

Promote ν− to be a function of γ2, in such a way that theexpansion cancels the log.

Similar to the construction of Geons where ω is promoted tobe a function of ε.

For kL � 1, ν− dangerously approaches 0 as k4L - exponentmight become negative ⇒ lattice relevant in IR.

Destroying AdS2 × R2:

Add the following third order term:

ρν− sin(kL)

Close to x = 0, perturbation theory is saved, however awayfrom x = 0 perturbation theory breaks down!

7 / 15

Page 31: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

A tale of two resummations:

Preserving AdS2 × R2:

Promote ν− to be a function of γ2, in such a way that theexpansion cancels the log.

Similar to the construction of Geons where ω is promoted tobe a function of ε.

For kL � 1, ν− dangerously approaches 0 as k4L - exponentmight become negative ⇒ lattice relevant in IR.

Destroying AdS2 × R2:

Add the following third order term:

ρν− sin(kL)

Close to x = 0, perturbation theory is saved, however awayfrom x = 0 perturbation theory breaks down!

7 / 15

Page 32: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

A tale of two resummations:

Preserving AdS2 × R2:

Promote ν− to be a function of γ2, in such a way that theexpansion cancels the log.

Similar to the construction of Geons where ω is promoted tobe a function of ε.

For kL � 1, ν− dangerously approaches 0 as k4L - exponentmight become negative ⇒ lattice relevant in IR.

Destroying AdS2 × R2:

Add the following third order term:

ρν− sin(kL)

Close to x = 0, perturbation theory is saved, however awayfrom x = 0 perturbation theory breaks down!

7 / 15

Page 33: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

A tale of two resummations:

Preserving AdS2 × R2:

Promote ν− to be a function of γ2, in such a way that theexpansion cancels the log.

Similar to the construction of Geons where ω is promoted tobe a function of ε.

For kL � 1, ν− dangerously approaches 0 as k4L - exponentmight become negative ⇒ lattice relevant in IR.

Destroying AdS2 × R2:

Add the following third order term:

ρν− sin(kL)

Close to x = 0, perturbation theory is saved, however awayfrom x = 0 perturbation theory breaks down!

7 / 15

Page 34: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

A tale of two resummations:

Preserving AdS2 × R2:

Promote ν− to be a function of γ2, in such a way that theexpansion cancels the log.

Similar to the construction of Geons where ω is promoted tobe a function of ε.

For kL � 1, ν− dangerously approaches 0 as k4L - exponentmight become negative ⇒ lattice relevant in IR.

Destroying AdS2 × R2:

Add the following third order term:

ρν− sin(kL)

Close to x = 0, perturbation theory is saved, however awayfrom x = 0 perturbation theory breaks down!

7 / 15

Page 35: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

A tale of two resummations:

Preserving AdS2 × R2:

Promote ν− to be a function of γ2, in such a way that theexpansion cancels the log.

Similar to the construction of Geons where ω is promoted tobe a function of ε.

For kL � 1, ν− dangerously approaches 0 as k4L - exponentmight become negative ⇒ lattice relevant in IR.

Destroying AdS2 × R2:

Add the following third order term:

η(ν−)ρν−x sin(kLx) .

Close to x = 0, perturbation theory is saved, however awayfrom x = 0 perturbation theory breaks down!

7 / 15

Page 36: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

A tale of two resummations:

Preserving AdS2 × R2:

Promote ν− to be a function of γ2, in such a way that theexpansion cancels the log.

Similar to the construction of Geons where ω is promoted tobe a function of ε.

For kL � 1, ν− dangerously approaches 0 as k4L - exponentmight become negative ⇒ lattice relevant in IR.

Destroying AdS2 × R2:

Add the following third order term:

η(ν−)ρν−x sin(kLx) ,

where η(ν−) can be chosen to cancel the diverging log.

Close to x = 0, perturbation theory is saved, however awayfrom x = 0 perturbation theory breaks down!

7 / 15

Page 37: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

A tale of two resummations:

Preserving AdS2 × R2:

Promote ν− to be a function of γ2, in such a way that theexpansion cancels the log.

Similar to the construction of Geons where ω is promoted tobe a function of ε.

For kL � 1, ν− dangerously approaches 0 as k4L - exponentmight become negative ⇒ lattice relevant in IR.

Destroying AdS2 × R2:

Add the following third order term:

η(ν−)ρν−x sin(kLx) .

Close to x = 0, perturbation theory is saved, however awayfrom x = 0 perturbation theory breaks down!

7 / 15

Page 38: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Breakdown of Perturbation theory

How to decide which is which?

Proceed without any approximation - Numerics.

8 / 15

Page 39: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Zero Temperature Numerics

Ansetzen & Numerics

Most general line element, without any gauge choice, and compatiblewith our symmetries takes the following form

ds2 =L2

y2

[−(1− y)2 G(y)Adt2 +

B

(1− y)2 G(y)(dy + F dx)2 + S1dx2 + S2dw2

]A = L

√6 (1− y)P dt .

where G(y) = 1 + 2y + 3y2. For A = B = S1 = S2 = P = 1 and F = 0 it

reduces to extreme RN black hole.

Comments:

Small irrational powers - (1− y)ν−(kL) - ν−(1) ≈ 0.012.

Use finite difference patch near H and spectral collocation.

Very steep gradients - need to use adaptive mesh refinementin finite difference patch.

Use De-Turck method - thank you Toby!

Alternatively, use very, very small T/µ.

9 / 15

Page 40: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Zero Temperature Numerics

Ansetzen & Numerics

Most general line element, without any gauge choice, and compatiblewith our symmetries takes the following form

ds2 =L2

y2

[−(1− y)2 G(y)Adt2 +

B

(1− y)2 G(y)(dy + F dx)2 + S1dx2 + S2dw2

]A = L

√6 (1− y)P dt .

where G(y) = 1 + 2y + 3y2. For A = B = S1 = S2 = P = 1 and F = 0 it

reduces to extreme RN black hole.

Comments:

Small irrational powers - (1− y)ν−(kL) - ν−(1) ≈ 0.012.

Use finite difference patch near H and spectral collocation.

Very steep gradients - need to use adaptive mesh refinementin finite difference patch.

Use De-Turck method - thank you Toby!

Alternatively, use very, very small T/µ.

9 / 15

Page 41: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Zero Temperature Numerics

Ansetzen & Numerics

Most general line element, without any gauge choice, and compatiblewith our symmetries takes the following form

ds2 =L2

y2

[−(1− y)2 G(y)Adt2 +

B

(1− y)2 G(y)(dy + F dx)2 + S1dx2 + S2dw2

]A = L

√6 (1− y)P dt .

where G(y) = 1 + 2y + 3y2. For A = B = S1 = S2 = P = 1 and F = 0 it

reduces to extreme RN black hole.

Comments:

Small irrational powers - (1− y)ν−(kL) - ν−(1) ≈ 0.012.

Use finite difference patch near H and spectral collocation.

Very steep gradients - need to use adaptive mesh refinementin finite difference patch.

Use De-Turck method - thank you Toby!

Alternatively, use very, very small T/µ.

9 / 15

Page 42: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Zero Temperature Numerics

Ansetzen & Numerics

Most general line element, without any gauge choice, and compatiblewith our symmetries takes the following form

ds2 =L2

y2

[−(1− y)2 G(y)Adt2 +

B

(1− y)2 G(y)(dy + F dx)2 + S1dx2 + S2dw2

]A = L

√6 (1− y)P dt .

where G(y) = 1 + 2y + 3y2. For A = B = S1 = S2 = P = 1 and F = 0 it

reduces to extreme RN black hole.

Comments:

Small irrational powers - (1− y)ν−(kL) - ν−(1) ≈ 0.012.

Use finite difference patch near H and spectral collocation.

Very steep gradients - need to use adaptive mesh refinementin finite difference patch.

Use De-Turck method - thank you Toby!

Alternatively, use very, very small T/µ.

9 / 15

Page 43: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Zero Temperature Numerics

Ansetzen & Numerics

Most general line element, without any gauge choice, and compatiblewith our symmetries takes the following form

ds2 =L2

y2

[−(1− y)2 G(y)Adt2 +

B

(1− y)2 G(y)(dy + F dx)2 + S1dx2 + S2dw2

]A = L

√6 (1− y)P dt .

where G(y) = 1 + 2y + 3y2. For A = B = S1 = S2 = P = 1 and F = 0 it

reduces to extreme RN black hole.

Comments:

Small irrational powers - (1− y)ν−(kL) - ν−(1) ≈ 0.012.

Use finite difference patch near H and spectral collocation.

Very steep gradients - need to use adaptive mesh refinementin finite difference patch.

Use De-Turck method - thank you Toby!

Alternatively, use very, very small T/µ.

9 / 15

Page 44: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Zero Temperature Numerics

Ansetzen & Numerics

Most general line element, without any gauge choice, and compatiblewith our symmetries takes the following form

ds2 =L2

y2

[−(1− y)2 G(y)Adt2 +

B

(1− y)2 G(y)(dy + F dx)2 + S1dx2 + S2dw2

]A = L

√6 (1− y)P dt .

where G(y) = 1 + 2y + 3y2. For A = B = S1 = S2 = P = 1 and F = 0 it

reduces to extreme RN black hole.

Comments:

Small irrational powers - (1− y)ν−(kL) - ν−(1) ≈ 0.012.

Use finite difference patch near H and spectral collocation.

Very steep gradients - need to use adaptive mesh refinementin finite difference patch.

Use De-Turck method - thank you Toby!

Alternatively, use very, very small T/µ.

9 / 15

Page 45: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Zero Temperature Numerics

Ansetzen & Numerics

Most general line element, without any gauge choice, and compatiblewith our symmetries takes the following form

ds2 =L2

y2

[−(1− y)2 G(y)Adt2 +

B

(1− y)2 G(y)(dy + F dx)2 + S1dx2 + S2dw2

]A = L

√6 (1− y)P dt .

where G(y) = 1 + 2y + 3y2. For A = B = S1 = S2 = P = 1 and F = 0 it

reduces to extreme RN black hole.

Comments:

Small irrational powers - (1− y)ν−(kL) - ν−(1) ≈ 0.012.

Use finite difference patch near H and spectral collocation.

Very steep gradients - need to use adaptive mesh refinementin finite difference patch.

Use De-Turck method - thank you Toby!

Alternatively, use very, very small T/µ.9 / 15

Page 46: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Results

Results:

To measure deviations from AdS2 × R2:

$ ≡ Wmax

Wmin− 1 ,

where W = (∂w)a(∂w)a|H.

For small A0, $ ∝ A0 - brokentranslational invariance ∀A0 6=0!!!

We repeated this calculation for severalvalues of k0, and find similar results. 0.0 0.5 1.0 1.5 2.0

0

5

10

15

20

A0

v

Einstein’s equations chose a resummation that rendersthe IR floppy - broken translational invariance.

10 / 15

Page 47: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Results

Results:

To measure deviations from AdS2 × R2:

$ ≡ Wmax

Wmin− 1 ,

where W = (∂w)a(∂w)a|H.

For small A0, $ ∝ A0 - brokentranslational invariance ∀A0 6=0!!!

We repeated this calculation for severalvalues of k0, and find similar results. 0.0 0.5 1.0 1.5 2.0

0

5

10

15

20

A0

v

Einstein’s equations chose a resummation that rendersthe IR floppy - broken translational invariance.

10 / 15

Page 48: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Results

Results:

To measure deviations from AdS2 × R2:

$ ≡ Wmax

Wmin− 1 ,

where W = (∂w)a(∂w)a|H.

For small A0, $ ∝ A0 - brokentranslational invariance ∀A0 6=0!!!

We repeated this calculation for severalvalues of k0, and find similar results.

0.0 0.5 1.0 1.5 2.00

5

10

15

20

A0

v

Einstein’s equations chose a resummation that rendersthe IR floppy - broken translational invariance.

10 / 15

Page 49: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Results

Results:

To measure deviations from AdS2 × R2:

$ ≡ Wmax

Wmin− 1 ,

where W = (∂w)a(∂w)a|H.

For small A0, $ ∝ A0 - brokentranslational invariance ∀A0 6=0!!!

We repeated this calculation for severalvalues of k0, and find similar results.

0.0 0.5 1.0 1.5 2.00

5

10

15

20

A0

v

Einstein’s equations chose a resummation that rendersthe IR floppy - broken translational invariance.

10 / 15

Page 50: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Results

Results:

To measure deviations from AdS2 × R2:

$ ≡ Wmax

Wmin− 1 ,

where W = (∂w)a(∂w)a|H.

For small A0, $ ∝ A0 - brokentranslational invariance ∀A0 6=0!!!

We repeated this calculation for severalvalues of k0, and find similar results. 0.0 0.5 1.0 1.5 2.0

0

5

10

15

20

A0

v

Einstein’s equations chose a resummation that rendersthe IR floppy - broken translational invariance.

10 / 15

Page 51: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Results

Results:

To measure deviations from AdS2 × R2:

$ ≡ Wmax

Wmin− 1 ,

where W = (∂w)a(∂w)a|H.

For small A0, $ ∝ A0 - brokentranslational invariance ∀A0 6=0!!!

We repeated this calculation for severalvalues of k0, and find similar results. 0.0 0.5 1.0 1.5 2.0

0

5

10

15

20

A0

v

Einstein’s equations chose a resummation that rendersthe IR floppy - broken translational invariance.

10 / 15

Page 52: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Results

Emergent picture:

AdS4 + μ + α cos (kLx)

AdS x R 22

Inhomogeneous IR

E

11 / 15

Page 53: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Periodic potentials in AdS4

Having seen the results in AdS2, one might wonder whether thesame happens in AdS4 for which µ = 0.

The T 6= 0 case was considered first by Chesler, Lucas and Sachdev.We will restrict to T = 0, which was not covered by their analysis.Can be done in an analytic perturbative expansion (valid for smalllattice amplitude) and numerically, for any lattice amplitude.

Results:

Recall At(x, 0) = α cos(kLx).

1D moduli space: α ≡ α/kL.

IR does not break ∂x.

Good agreement between numericsand analytic results: 10th order.

No phase transition up to α ∼ 6. 0 1 2 3 4 50.0

0.2

0.4

0.6

0.8

1.0

-»»∂t »»2»»∂w »»2

12 / 15

Page 54: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Periodic potentials in AdS4

Having seen the results in AdS2, one might wonder whether thesame happens in AdS4 for which µ = 0.The T 6= 0 case was considered first by Chesler, Lucas and Sachdev.

We will restrict to T = 0, which was not covered by their analysis.Can be done in an analytic perturbative expansion (valid for smalllattice amplitude) and numerically, for any lattice amplitude.

Results:

Recall At(x, 0) = α cos(kLx).

1D moduli space: α ≡ α/kL.

IR does not break ∂x.

Good agreement between numericsand analytic results: 10th order.

No phase transition up to α ∼ 6. 0 1 2 3 4 50.0

0.2

0.4

0.6

0.8

1.0

-»»∂t »»2»»∂w »»2

12 / 15

Page 55: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Periodic potentials in AdS4

Having seen the results in AdS2, one might wonder whether thesame happens in AdS4 for which µ = 0.The T 6= 0 case was considered first by Chesler, Lucas and Sachdev.We will restrict to T = 0, which was not covered by their analysis.

Can be done in an analytic perturbative expansion (valid for smalllattice amplitude) and numerically, for any lattice amplitude.

Results:

Recall At(x, 0) = α cos(kLx).

1D moduli space: α ≡ α/kL.

IR does not break ∂x.

Good agreement between numericsand analytic results: 10th order.

No phase transition up to α ∼ 6. 0 1 2 3 4 50.0

0.2

0.4

0.6

0.8

1.0

-»»∂t »»2»»∂w »»2

12 / 15

Page 56: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Periodic potentials in AdS4

Having seen the results in AdS2, one might wonder whether thesame happens in AdS4 for which µ = 0.The T 6= 0 case was considered first by Chesler, Lucas and Sachdev.We will restrict to T = 0, which was not covered by their analysis.Can be done in an analytic perturbative expansion (valid for smalllattice amplitude) and numerically, for any lattice amplitude.

Results:

Recall At(x, 0) = α cos(kLx).

1D moduli space: α ≡ α/kL.

IR does not break ∂x.

Good agreement between numericsand analytic results: 10th order.

No phase transition up to α ∼ 6. 0 1 2 3 4 50.0

0.2

0.4

0.6

0.8

1.0

-»»∂t »»2»»∂w »»2

12 / 15

Page 57: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Periodic potentials in AdS4

Having seen the results in AdS2, one might wonder whether thesame happens in AdS4 for which µ = 0.The T 6= 0 case was considered first by Chesler, Lucas and Sachdev.We will restrict to T = 0, which was not covered by their analysis.Can be done in an analytic perturbative expansion (valid for smalllattice amplitude) and numerically, for any lattice amplitude.

Results:

Recall At(x, 0) = α cos(kLx).

1D moduli space: α ≡ α/kL.

IR does not break ∂x.

Good agreement between numericsand analytic results: 10th order.

No phase transition up to α ∼ 6. 0 1 2 3 4 50.0

0.2

0.4

0.6

0.8

1.0

-»»∂t »»2»»∂w »»2

12 / 15

Page 58: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Periodic potentials in AdS4

Having seen the results in AdS2, one might wonder whether thesame happens in AdS4 for which µ = 0.The T 6= 0 case was considered first by Chesler, Lucas and Sachdev.We will restrict to T = 0, which was not covered by their analysis.Can be done in an analytic perturbative expansion (valid for smalllattice amplitude) and numerically, for any lattice amplitude.

Results:

Recall At(x, 0) = α cos(kLx).

1D moduli space: α ≡ α/kL.

IR does not break ∂x.

Good agreement between numericsand analytic results: 10th order.

No phase transition up to α ∼ 6. 0 1 2 3 4 50.0

0.2

0.4

0.6

0.8

1.0

-»»∂t »»2»»∂w »»2

12 / 15

Page 59: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Periodic potentials in AdS4

Having seen the results in AdS2, one might wonder whether thesame happens in AdS4 for which µ = 0.The T 6= 0 case was considered first by Chesler, Lucas and Sachdev.We will restrict to T = 0, which was not covered by their analysis.Can be done in an analytic perturbative expansion (valid for smalllattice amplitude) and numerically, for any lattice amplitude.

Results:

Recall At(x, 0) = α cos(kLx).

1D moduli space: α ≡ α/kL.

IR does not break ∂x.

Good agreement between numericsand analytic results: 10th order.

No phase transition up to α ∼ 6. 0 1 2 3 4 50.0

0.2

0.4

0.6

0.8

1.0

-»»∂t »»2»»∂w »»2

12 / 15

Page 60: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Periodic potentials in AdS4

Having seen the results in AdS2, one might wonder whether thesame happens in AdS4 for which µ = 0.The T 6= 0 case was considered first by Chesler, Lucas and Sachdev.We will restrict to T = 0, which was not covered by their analysis.Can be done in an analytic perturbative expansion (valid for smalllattice amplitude) and numerically, for any lattice amplitude.

Results:

Recall At(x, 0) = α cos(kLx).

1D moduli space: α ≡ α/kL.

IR does not break ∂x.

Good agreement between numericsand analytic results: 10th order.

No phase transition up to α ∼ 6.

0 1 2 3 4 50.0

0.2

0.4

0.6

0.8

1.0

-»»∂t »»2»»∂w »»2

12 / 15

Page 61: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Periodic potentials in AdS4

Having seen the results in AdS2, one might wonder whether thesame happens in AdS4 for which µ = 0.The T 6= 0 case was considered first by Chesler, Lucas and Sachdev.We will restrict to T = 0, which was not covered by their analysis.Can be done in an analytic perturbative expansion (valid for smalllattice amplitude) and numerically, for any lattice amplitude.

Results:

Recall At(x, 0) = α cos(kLx).

1D moduli space: α ≡ α/kL.

IR does not break ∂x.

Good agreement between numericsand analytic results: 10th order.

No phase transition up to α ∼ 6. 0 1 2 3 4 50.0

0.2

0.4

0.6

0.8

1.0

-»»∂t »»2»»∂w »»2

12 / 15

Page 62: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Disorder in AdS4:

One periodic source does not do, what about many?

Φs(x,w, 0) = 2V

Nx−1∑i=1

Nw−1∑j=1

AiBj cos[k(i)x+ ] cos[q(j)w + ] .

where γi and λj are random phases, and Φs is the source foroperator of ∆+ = 2.

Averaged quantities are defined as:

〈f〉R ≡ limNw→+∞

limNx→+∞

Nx−1∏i=1

∫ 2π

0

dγi2π

Nw−1∏j=1

∫ 2π

0

dδj2π

f .

If we are interested in isotropic local Gaussian disorder:

N = Nx = Nw , Ai = Bj =

√k0

Nand k(ξ) = q(ξ) = ξ

π k0

N

in which case:

〈Φ〉R = 0 , and 〈Φs(x,w, 0)Φs(s, h, 0)〉R = V 2δ(x− s)δ(w − h) .

13 / 15

Page 63: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Disorder in AdS4:

One periodic source does not do, what about many?

Φs(x,w, 0) = 2V

Nx−1∑i=1

Nw−1∑j=1

AiBj cos[k(i)x+ γi] cos[q(j)w + λj ] ,

where γi and λj are random phases, and Φs is the source foroperator of ∆+ = 2.Averaged quantities are defined as:

〈f〉R ≡ limNw→+∞

limNx→+∞

Nx−1∏i=1

∫ 2π

0

dγi2π

Nw−1∏j=1

∫ 2π

0

dδj2π

f .

If we are interested in isotropic local Gaussian disorder:

N = Nx = Nw , Ai = Bj =

√k0

Nand k(ξ) = q(ξ) = ξ

π k0

N

in which case:

〈Φ〉R = 0 , and 〈Φs(x,w, 0)Φs(s, h, 0)〉R = V 2δ(x− s)δ(w − h) .

13 / 15

Page 64: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Disorder in AdS4:

One periodic source does not do, what about many?

Φs(x,w, 0) = 2V

Nx−1∑i=1

Nw−1∑j=1

AiBj cos[k(i)x+ γi] cos[q(j)w + λj ] ,

where γi and λj are random phases, and Φs is the source foroperator of ∆+ = 2.

Averaged quantities are defined as:

〈f〉R ≡ limNw→+∞

limNx→+∞

Nx−1∏i=1

∫ 2π

0

dγi2π

Nw−1∏j=1

∫ 2π

0

dδj2π

f .

If we are interested in isotropic local Gaussian disorder:

N = Nx = Nw , Ai = Bj =

√k0

Nand k(ξ) = q(ξ) = ξ

π k0

N

in which case:

〈Φ〉R = 0 , and 〈Φs(x,w, 0)Φs(s, h, 0)〉R = V 2δ(x− s)δ(w − h) .

13 / 15

Page 65: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Disorder in AdS4:

One periodic source does not do, what about many?

Φs(x,w, 0) = 2V

Nx−1∑i=1

Nw−1∑j=1

AiBj cos[k(i)x+ γi] cos[q(j)w + λj ] ,

where γi and λj are random phases, and Φs is the source foroperator of ∆+ = 2.Averaged quantities are defined as:

〈f〉R ≡ limNw→+∞

limNx→+∞

Nx−1∏i=1

∫ 2π

0

dγi2π

Nw−1∏j=1

∫ 2π

0

dδj2π

f .

If we are interested in isotropic local Gaussian disorder:

N = Nx = Nw , Ai = Bj =

√k0

Nand k(ξ) = q(ξ) = ξ

π k0

N

in which case:

〈Φ〉R = 0 , and 〈Φs(x,w, 0)Φs(s, h, 0)〉R = V 2δ(x− s)δ(w − h) .

13 / 15

Page 66: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Disorder in AdS4:

One periodic source does not do, what about many?

Φs(x,w, 0) = 2V

Nx−1∑i=1

Nw−1∑j=1

AiBj cos[k(i)x+ γi] cos[q(j)w + λj ] ,

where γi and λj are random phases, and Φs is the source foroperator of ∆+ = 2.Averaged quantities are defined as:

〈f〉R ≡ limNw→+∞

limNx→+∞

Nx−1∏i=1

∫ 2π

0

dγi2π

Nw−1∏j=1

∫ 2π

0

dδj2π

f .

If we are interested in isotropic local Gaussian disorder:

N = Nx = Nw , Ai = Bj =

√k0

Nand k(ξ) = q(ξ) = ξ

π k0

N.

in which case:

〈Φ〉R = 0 , and 〈Φs(x,w, 0)Φs(s, h, 0)〉R = V 2δ(x− s)δ(w − h) .

13 / 15

Page 67: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Disorder in AdS4:

One periodic source does not do, what about many?

Φs(x,w, 0) = 2V

Nx−1∑i=1

Nw−1∑j=1

AiBj cos[k(i)x+ γi] cos[q(j)w + λj ] ,

where γi and λj are random phases, and Φs is the source foroperator of ∆+ = 2.Averaged quantities are defined as:

〈f〉R ≡ limNw→+∞

limNx→+∞

Nx−1∏i=1

∫ 2π

0

dγi2π

Nw−1∏j=1

∫ 2π

0

dδj2π

f .

If we are interested in isotropic local Gaussian disorder:

N = Nx = Nw , Ai = Bj =

√k0

Nand k(ξ) = q(ξ) = ξ

π k0

N,

in which case:

〈Φ〉R = 0 , and 〈Φs(x,w, 0)Φs(s, h, 0)〉R = V 2δ(x− s)δ(w − h) .

13 / 15

Page 68: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Results:

Example of a fully 3D backreacted run.

Contour plot of Φ.

Common questions:

Since the pointwise value of |Φ|grows likes

√N , why don’t you

form black holes bound states?

Is the boundary data regularenough for this problem to be wellposed, as N → +∞?

〈gab〉R is accurately described by a Lifshitz geometry:

〈ds2〉R =L2

y2

[− dt2

y2(z−1)+ dx2 + dw2 + dy2

].

14 / 15

Page 69: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Results:

Example of a fully 3D backreacted run.

Contour plot of Φ.

Common questions:

Since the pointwise value of |Φ|grows likes

√N , why don’t you

form black holes bound states?

Is the boundary data regularenough for this problem to be wellposed, as N → +∞?

〈gab〉R is accurately described by a Lifshitz geometry:

〈ds2〉R =L2

y2

[− dt2

y2(z−1)+ dx2 + dw2 + dy2

].

14 / 15

Page 70: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Results:

Example of a fully 3D backreacted run.

Contour plot of Φ.

Common questions:

Since the pointwise value of |Φ|grows likes

√N , why don’t you

form black holes bound states?

Is the boundary data regularenough for this problem to be wellposed, as N → +∞?

〈gab〉R is accurately described by a Lifshitz geometry:

〈ds2〉R =L2

y2

[− dt2

y2(z−1)+ dx2 + dw2 + dy2

].

14 / 15

Page 71: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Results:

Example of a fully 3D backreacted run.

Contour plot of Φ.

Common questions:

Since the pointwise value of |Φ|grows likes

√N , why don’t you

form black holes bound states?

Is the boundary data regularenough for this problem to be wellposed, as N → +∞?

〈gab〉R is accurately described by a Lifshitz geometry:

〈ds2〉R =L2

y2

[− dt2

y2(z−1)+ dx2 + dw2 + dy2

].

14 / 15

Page 72: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Results:

Example of a fully 3D backreacted run.

Contour plot of Φ.

Common questions:

Since the pointwise value of |Φ|grows likes

√N , why don’t you

form black holes bound states?

Is the boundary data regularenough for this problem to be wellposed, as N → +∞?

〈gab〉R is accurately described by a Lifshitz geometry:

〈ds2〉R =L2

y2

[− dt2

y2(z−1)+ dx2 + dw2 + dy2

].

14 / 15

Page 73: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

What about AdS4?

Results:

Example of a fully 3D backreacted run.

Contour plot of Φ.

Common questions:

Since the pointwise value of |Φ|grows likes

√N , why don’t you

form black holes bound states?

Is the boundary data regularenough for this problem to be wellposed, as N → +∞?

0.00 0.05 0.10 0.15 0.201.000

1.005

1.010

1.015

1.020

1.025

1.030

V

z

〈gab〉R is accurately described by a Lifshitz geometry:

〈ds2〉R =L2

y2

[− dt2

y2(z−1)+ dx2 + dw2 + dy2

].

14 / 15

Page 74: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Conclusion & Outlook

Conclusions:

Numerical evidence that AdS2 × R2 is RG unstable.

Instability does not affect AdS4.

Disorder potentials affect AdS4.

What to ask me after the talk:

What about more general deformations?

Is there a full function of two variables worth ofdeformations?

What are the implications of this IR to transport?

Outlook:

Can these new IR geometries affect time dependence?

Can we make a connection with glassy physics?

. . .

15 / 15

Page 75: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Conclusion & Outlook

Conclusions:

Numerical evidence that AdS2 × R2 is RG unstable.

Instability does not affect AdS4.

Disorder potentials affect AdS4.

What to ask me after the talk:

What about more general deformations?

Is there a full function of two variables worth ofdeformations?

What are the implications of this IR to transport?

Outlook:

Can these new IR geometries affect time dependence?

Can we make a connection with glassy physics?

. . .

15 / 15

Page 76: Jorge E. Santos New frontiers in dynamical gravity · New frontiers in dynamical gravity In collaboration with Sean A. Hartnoll - arXiv:1402.0872 and arXiv:1403.4612 1/15. Cold planar

Cold planar horizons are floppy

Conclusion & Outlook

Conclusions:

Numerical evidence that AdS2 × R2 is RG unstable.

Instability does not affect AdS4.

Disorder potentials affect AdS4.

What to ask me after the talk:

What about more general deformations?

Is there a full function of two variables worth ofdeformations?

What are the implications of this IR to transport?

Outlook:

Can these new IR geometries affect time dependence?

Can we make a connection with glassy physics?

. . .

15 / 15