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Islands in JT Gravity

The island formula is most transparent in two-dimensional dilaton gravity. The reason is not that the black hole information problem is really two-dimensional. The reason is that two-dimensional gravity lets us separate the essential ingredients from the technical clutter of higher-dimensional black holes.

Jackiw-Teitelboim gravity, usually called JT gravity, is especially useful because its metric is locally fixed to be AdS2_2, while its dilaton keeps track of the transverse area that would have appeared in a higher-dimensional near-extremal black hole. In this model the island mechanism can be explained with actual formulas rather than just slogans.

The central result of this page is the JT version of the island rule:

S(R)=minIextI[pIΦ0+Φ(p)4GN+Smatter(RI)].\boxed{ S(R) = \min_I\operatorname{ext}_I \left[ \sum_{p\in\partial I} \frac{\Phi_0+\Phi(p)}{4G_N} + S_{\rm matter}(R\cup I) \right]. }

Here RR is a nongravitating radiation region in an external bath, II is a possible island inside the gravitating region, I\partial I is the set of quantum extremal-surface points bounding the island, Φ\Phi is the JT dilaton, and Smatter(RI)S_{\rm matter}(R\cup I) is an ordinary matter entropy computed in a fixed semiclassical background.

The formula says something wonderfully weird but precise: after the Page time, the fine-grained entropy of Hawking radiation is computed as though a region behind the horizon belongs to the radiation system.

A near-extremal charged black hole in higher dimensions has a long throat whose geometry is approximately AdS2_2 times a compact transverse space:

near-horizon regionAdS2×K.\text{near-horizon region} \approx \text{AdS}_2\times \mathcal K.

The transverse area is not constant once we move along the throat. After reducing on K\mathcal K, this area becomes a two-dimensional scalar field, the dilaton Φ\Phi. The two-dimensional metric describes the AdS2_2 throat, while Φ\Phi remembers the higher-dimensional area.

This is the conceptual reason the entropy term in JT gravity is

Sarea(p)=Φ0+Φ(p)4GN,S_{\rm area}(p)=\frac{\Phi_0+\Phi(p)}{4G_N},

where pp is a codimension-two surface. In two spacetime dimensions a codimension-two surface is just a point, so the “area of a surface” becomes the value of a scalar at a point.

JT gravity is simple in a very specific sense. It has no local graviton. The metric equation fixes the curvature, and the remaining gravitational dynamics are mostly boundary dynamics and dilaton dynamics. But this simplicity is a feature, not a bug: the island transition is an entropy saddle transition, and JT gravity keeps that transition visible.

A convenient Lorentzian convention is

IJT=116πGN[Φ0(Md2xgR+2MduhK)+Md2xgΦ(R+2L2)+2MduhΦ(K1L)]+Imatter.I_{\rm JT} = \frac{1}{16\pi G_N} \left[ \Phi_0 \left( \int_{\mathcal M}d^2x\sqrt{-g}\,R +2\int_{\partial\mathcal M}du\sqrt{|h|}\,K \right) + \int_{\mathcal M}d^2x\sqrt{-g}\,\Phi\left(R+\frac{2}{L^2}\right) +2\int_{\partial\mathcal M}du\sqrt{|h|}\,\Phi\left(K-\frac{1}{L}\right) \right] +I_{\rm matter}.

Different papers use different signs and normalizations. What matters for us is the structure:

topological term Φ0+dynamical dilaton Φ+matter CFT.\text{topological term }\Phi_0 \quad+ \quad \text{dynamical dilaton }\Phi \quad+ \quad \text{matter CFT}.

Varying with respect to Φ\Phi gives

R=2L2.R=-\frac{2}{L^2}.

So the spacetime is locally AdS2_2. The metric itself has no propagating local degrees of freedom. The nontrivial physics sits in the boundary trajectory, the dilaton profile, the matter fields, and the choice of saddle in the gravitational entropy calculation.

The constant Φ0\Phi_0 multiplies the Euler characteristic. It gives an extremal entropy

S0=Φ04GN.S_0=\frac{\Phi_0}{4G_N}.

The dynamical part of the entropy is controlled by Φ\Phi. For a point pp, the generalized entropy contribution is

Sgeom(p)=Φ0+Φ(p)4GN.S_{\rm geom}(p)=\frac{\Phi_0+\Phi(p)}{4G_N}.

In higher-dimensional language, Φ0+Φ\Phi_0+\Phi is the effective transverse area.

A standard two-dimensional black-hole solution is

ds2=r2rh2L2dt2+L2r2rh2dr2,ds^2 = -\frac{r^2-r_h^2}{L^2}\,dt^2 +\frac{L^2}{r^2-r_h^2}\,dr^2,

with dilaton

Φ(r)=ΦrrL.\Phi(r)=\Phi_r\frac{r}{L}.

The horizon is at r=rhr=r_h. The Hawking temperature is fixed by smoothness of the Euclidean cigar:

T=1β=rh2πL2.T=\frac{1}{\beta}=\frac{r_h}{2\pi L^2}.

The entropy is

SBH=Φ0+Φ(rh)4GN=S0+Φrrh4GNL.S_{\rm BH} = \frac{\Phi_0+\Phi(r_h)}{4G_N} = S_0+\frac{\Phi_r r_h}{4G_N L}.

The mass above extremality is, in this convention,

M=Φrrh216πGNL3.M = \frac{\Phi_r r_h^2}{16\pi G_N L^3}.

Indeed,

dM=TdSBH.dM=T\,dS_{\rm BH}.

This solution should be read as a controlled near-horizon model of near-extremal black-hole physics. The constant S0S_0 is the large extremal entropy. The temperature-dependent entropy is the part carried by the AdS2_2 throat.

Even though the bulk curvature is fixed, the AdS2_2 boundary can wiggle. A boundary trajectory can be described by a reparametrization t=f(u)t=f(u), where uu is the physical boundary time. The low-energy effective action for this mode is the Schwarzian action,

ISch=Cdu{f(u),u},I_{\rm Sch} = -C\int du\,\{f(u),u\},

where

{f,u}=f(u)f(u)32(f(u)f(u))2.\{f,u\} = \frac{f'''(u)}{f'(u)} -\frac{3}{2}\left(\frac{f''(u)}{f'(u)}\right)^2.

The coefficient CC is proportional to Φr/GN\Phi_r/G_N. The Schwarzian mode controls the thermodynamics and the gravitational response of nearly AdS2_2 systems. In the island calculation, however, we will mostly use a simpler fact: the dilaton gives a large entropy cost for placing a QES, and the matter fields give an entropy benefit.

To make an evaporating black hole, one attaches the AdS2_2 gravitating region to a nongravitating bath. The bath carries the same matter CFT, but gravity is turned off there. Transparent boundary conditions allow excitations to pass from the gravitating region into the bath.

A JT black hole coupled to a nongravitating bath

A JT black hole can be coupled to a nongravitating bath by transparent boundary conditions for the matter CFT. Radiation collected in the bath defines an ordinary quantum subsystem $R$, while gravity remains dynamical in the AdS$_2$ region.

This setup is conceptually important. In a gravitating region, defining “the Hilbert space of a subregion” is subtle because of diffeomorphism constraints. In the bath, by contrast, gravity is absent and RR is an ordinary nongravitating subsystem with an ordinary reduced density matrix ρR\rho_R.

So the question

S(R)=TrρRlogρRS(R)=-\operatorname{Tr}\rho_R\log\rho_R

is sharply defined. The surprise is that the gravitational formula for this entropy may include an island II that lies in the gravitating region.

For a bath region RR, the island prescription says to consider candidate regions II in the gravitating region and compute

Sgen(I;R)=pIΦ0+Φ(p)4GN+Smatter(RI).S_{\rm gen}(I;R) = \sum_{p\in\partial I} \frac{\Phi_0+\Phi(p)}{4G_N} + S_{\rm matter}(R\cup I).

Then one extremizes over the island endpoint locations and chooses the minimal saddle:

S(R)=minIextISgen(I;R).S(R) = \min_I\operatorname{ext}_I S_{\rm gen}(I;R).

The two most important candidate saddles are:

I=,I.I=\varnothing, \qquad I\neq\varnothing.

The first is the no-island saddle. It reproduces the Hawking answer. The second is the island saddle. It gives the Page-curve answer at late times.

No-island and island saddles in a JT bath setup

The no-island saddle computes the entropy of the bath radiation region $R$ alone. The island saddle computes the entropy of $R\cup I$ and pays a geometric cost at the QES point. At late times, the island saddle wins.

The notation can be dangerously simple. The island is not inserted by hand as a new physical rule about where the radiation lives. It is a saddle in a gravitational entropy calculation. The gravitational path integral decides whether the saddle contributes dominantly.

The technical advantage of JT gravity is that the matter entropy is often computable using two-dimensional CFT formulas.

For a single interval of length \ell in the vacuum of a CFT2_2,

SCFT([x1,x2])=c3logϵ,=x1x2.S_{\rm CFT}([x_1,x_2]) = \frac{c}{3}\log\frac{\ell}{\epsilon}, \qquad \ell=|x_1-x_2|.

At temperature T=1/βT=1/\beta,

SCFTβ([0,])=c3log[βπϵsinh(πβ)].S_{\rm CFT}^{\beta}([0,\ell]) = \frac{c}{3} \log\left[ \frac{\beta}{\pi\epsilon} \sinh\left(\frac{\pi\ell}{\beta}\right) \right].

For large \ell,

SCFTβ([0,])=πc3β+O(1).S_{\rm CFT}^{\beta}([0,\ell]) = \frac{\pi c}{3\beta}\ell +O(1).

The coefficient

sth=πc3βs_{\rm th}=\frac{\pi c}{3\beta}

is the thermal entropy density of a two-dimensional CFT. This is why the no-island entropy grows linearly with time in simple evaporating setups: as time passes, the radiation region contains a longer and longer thermal segment of outgoing Hawking radiation.

For multiple intervals, the entropy is a twist-operator correlation function. In general it depends on the full CFT data. In many island calculations one works in limits where the relevant conformal block or free-field approximation makes the answer simple enough to see the saddle transition explicitly.

Set I=I=\varnothing. Then

Sno(R)=Smatter(R).S_{\rm no}(R)=S_{\rm matter}(R).

The radiation region contains outgoing Hawking modes. In a simple thermal approximation,

Sno(t)πc3βt+Sconst.S_{\rm no}(t) \simeq \frac{\pi c}{3\beta}t+S_{\rm const}.

The precise coefficient depends on whether one studies a one-sided or two-sided setup, and on the precise definition of RR. The essential feature does not depend on these details:

Sno(t) grows without knowing about the finite black-hole entropy.\boxed{ S_{\rm no}(t)\text{ grows without knowing about the finite black-hole entropy.} }

This is Hawking’s answer in island language. It is a perfectly legitimate saddle. It is just not always the dominant saddle.

The island saddle: the partners are included

Section titled “The island saddle: the partners are included”

Now allow a nonempty island II behind the horizon. The generalized entropy has two competing pieces:

Sgen(I;R)=geometric cost+matter entropy benefit.S_{\rm gen}(I;R) = \text{geometric cost} + \text{matter entropy benefit}.

The geometric cost is large:

Φ0+Φ(I)4GNO(1GN).\frac{\Phi_0+\Phi(\partial I)}{4G_N} \sim O\left(\frac{1}{G_N}\right).

But the matter entropy can drop dramatically. The outgoing Hawking quanta in RR are entangled with interior partners. If the island contains those partners, then the matter entropy of RIR\cup I is much smaller than the entropy of RR alone.

At late times the island saddle has the schematic form

Sisland(t)SBH(t)+O(c),S_{\rm island}(t) \simeq S_{\rm BH}(t)+O(c),

for a one-sided setup, or twice this value for a symmetric two-sided setup. The O(c)O(c) term is the residual CFT entropy after including the island. The leading behavior is controlled by the black-hole entropy rather than by the growing Hawking entropy.

Thus the late-time entropy is not

Srad(t)=SHawking(t),S_{\rm rad}(t)=S_{\rm Hawking}(t),

but rather

Srad(t)min{SHawking(t),SBH(t)+O(c)}.S_{\rm rad}(t) \simeq \min\{S_{\rm Hawking}(t),S_{\rm BH}(t)+O(c)\}.

This is the Page curve in its simplest semiclassical disguise.

The QES condition is the extremality condition for SgenS_{\rm gen}. Near the horizon, let σ\sigma be a small coordinate distance from the horizon along a spatial slice. A useful schematic model is

Sgen(σ)=Φh+Φhσ4GN+Smatter(0)c6logσϵ.S_{\rm gen}(\sigma) = \frac{\Phi_h+\Phi'_h\sigma}{4G_N} +S_{\rm matter}^{(0)} -\frac{c}{6}\log\frac{\sigma}{\epsilon}.

The first term grows as the endpoint moves away from the horizon. The logarithmic term models the matter-entropy advantage of moving the endpoint. Extremizing gives

0=Sgenσ=Φh4GNc6σ,0 = \frac{\partial S_{\rm gen}}{\partial\sigma} = \frac{\Phi'_h}{4G_N}-\frac{c}{6\sigma_*},

so

σ=2cGN3Φh.\boxed{ \sigma_* = \frac{2cG_N}{3\Phi'_h}. }

Do not overinterpret the exact coefficient. It depends on the coordinate choice and the simplified matter entropy. The robust lesson is that the QES is parametrically close to the horizon when cGN/ΦhcG_N/\Phi'_h is small.

The JT quantum extremal surface sits near the horizon because the area gradient balances the matter entropy gradient

The QES location is determined by a balance between the geometric area/dilaton gradient and the matter entropy gradient. In a semiclassical JT black hole, this balance places the QES close to the horizon.

This is the two-dimensional version of a very general intuition: the island endpoint appears near the horizon because the horizon is where the geometric entropy cost is just right for capturing the interior partners of Hawking radiation.

The fine-grained radiation entropy is obtained by comparing saddles:

Srad(t)=min{Sno(t),Sisland(t)}.S_{\rm rad}(t) = \min\{S_{\rm no}(t),S_{\rm island}(t)\}.

Before the Page time,

Sno(t)<Sisland(t),S_{\rm no}(t)<S_{\rm island}(t),

so the no-island saddle dominates and the entropy follows Hawking’s increasing answer.

After the Page time,

Sisland(t)<Sno(t),S_{\rm island}(t)<S_{\rm no}(t),

so the island saddle dominates and the entropy follows the black-hole entropy scale. For an evaporating black hole, SBH(t)S_{\rm BH}(t) decreases, so the radiation entropy decreases after the transition.

The Page transition in JT gravity arises from taking the minimum of no-island and island saddles

The no-island saddle gives Hawking growth. The island saddle has a larger initial cost but eventually dominates. The physical entropy is the lower envelope, giving the Page curve.

In the approximation where SBHS_{\rm BH} changes slowly compared with the radiation entropy growth, the Page time is estimated by

πc3βtPageSBH,\frac{\pi c}{3\beta}t_{\rm Page} \sim S_{\rm BH},

or

tPage3βπcSBH.t_{\rm Page} \sim \frac{3\beta}{\pi c}S_{\rm BH}.

Again, the coefficient depends on the setup. The parametric statement is the important one: the Page time is when the semiclassical Hawking entropy becomes comparable to the black-hole entropy.

Before the Page time, the radiation entanglement wedge is essentially the bath region RR. The interior partners are not reconstructible from the radiation alone.

After the Page time, the dominant QES changes. The radiation entanglement wedge includes RIR\cup I. Thus operators in the island are encoded in the radiation system, at least within the appropriate code subspace and with the usual caveats about reconstruction complexity and state dependence.

This gives a geometric explanation of Page’s information-theoretic expectation. The radiation entropy decreases not because local Hawking emission stops looking thermal, but because the fine-grained entropy prescription changes saddles.

A useful slogan is

the Page transition is an entanglement-wedge transition.\boxed{ \text{the Page transition is an entanglement-wedge transition.} }

The island is the bulk region that must be included so that the radiation has the correct fine-grained entropy.

The JT island calculation teaches several lessons that survive beyond two dimensions.

First, the Hawking calculation computes a real semiclassical saddle, but not always the dominant saddle for fine-grained entropy.

Second, the correction is nonperturbative from the viewpoint of the naive entropy answer. The island saddle can change S(R)S(R) by order 1/GN1/G_N, even though local effective field theory near the horizon remains an excellent approximation for simple observables.

Third, the generalized entropy is the correct object to extremize. The separation between the geometric term and matter entropy is regulator dependent, but the renormalized sum is meaningful.

Fourth, the island rule explains the Page curve but does not by itself give every microscopic matrix element of the black-hole SS-matrix. Entropy is a coarse functional of the density matrix. The full state is much more detailed.

Fifth, the calculation is powerful precisely because RR lives in a nongravitating bath. The bath gives a clean operational meaning to the radiation entropy.

Pitfall 1: “The island is manually added to purify the radiation.”

No. The island appears by extremizing and minimizing SgenS_{\rm gen}. At early times the island saddle is subdominant. At late times it dominates.

Pitfall 2: “The island means the Hawking calculation was locally wrong.”

Not in the usual sense. The local Hawking state can remain an excellent semiclassical approximation. The failure is in using the wrong global saddle for a fine-grained entropy.

Pitfall 3: “JT gravity solves the full four-dimensional problem.”

JT gravity is a controlled model, not a complete model of realistic black holes. It captures universal near-AdS2_2 and gravitational-entropy physics, but higher-dimensional evaporation has additional technical and conceptual issues.

Pitfall 4: “The area term and matter entropy are separately physical.”

Their split is cutoff dependent. The generalized entropy is the physical object after renormalization of gravitational couplings.

Pitfall 5: “The Page curve gives the final quantum state.”

No. The Page curve gives a fine-grained entropy. It strongly constrains the state, but it does not provide all amplitudes or a complete decoding protocol.

Consider the dynamical part of the JT action,

IΦ=116πGNd2xgΦ(R+2L2).I_\Phi =\frac{1}{16\pi G_N} \int d^2x\sqrt{-g}\,\Phi\left(R+\frac{2}{L^2}\right).

Vary the action with respect to Φ\Phi. What equation does this impose on the metric?

Solution

The variation with respect to Φ\Phi is direct:

δΦIΦ=116πGNd2xgδΦ(R+2L2).\delta_\Phi I_\Phi =\frac{1}{16\pi G_N} \int d^2x\sqrt{-g}\,\delta\Phi \left(R+\frac{2}{L^2}\right).

Since δΦ\delta\Phi is arbitrary, the equation of motion is

R+2L2=0.R+\frac{2}{L^2}=0.

Therefore

R=2L2.R=-\frac{2}{L^2}.

The spacetime is locally AdS2_2.

Exercise 2: First law for the JT black hole

Section titled “Exercise 2: First law for the JT black hole”

For the JT black hole

T=rh2πL2,SBH=S0+Φrrh4GNL.T=\frac{r_h}{2\pi L^2}, \qquad S_{\rm BH}=S_0+\frac{\Phi_r r_h}{4G_N L}.

Show that the mass

M=Φrrh216πGNL3M=\frac{\Phi_r r_h^2}{16\pi G_N L^3}

satisfies dM=TdSBHdM=T\,dS_{\rm BH}.

Solution

Differentiate the entropy:

dSBH=Φr4GNLdrh.dS_{\rm BH}=\frac{\Phi_r}{4G_N L}\,dr_h.

Then

TdSBH=rh2πL2Φr4GNLdrh=Φrrh8πGNL3drh.T\,dS_{\rm BH} = \frac{r_h}{2\pi L^2} \frac{\Phi_r}{4G_N L}\,dr_h = \frac{\Phi_r r_h}{8\pi G_N L^3}\,dr_h.

Differentiating the mass gives

dM=Φr16πGNL32rhdrh=Φrrh8πGNL3drh.dM =\frac{\Phi_r}{16\pi G_N L^3}\,2r_h\,dr_h =\frac{\Phi_r r_h}{8\pi G_N L^3}\,dr_h.

Hence

dM=TdSBH.dM=T\,dS_{\rm BH}.

Exercise 3: Late-time growth of thermal CFT entropy

Section titled “Exercise 3: Late-time growth of thermal CFT entropy”

Use

SCFTβ([0,])=c3log[βπϵsinh(πβ)]S_{\rm CFT}^{\beta}([0,\ell]) = \frac{c}{3} \log\left[ \frac{\beta}{\pi\epsilon} \sinh\left(\frac{\pi\ell}{\beta}\right) \right]

to show that for β\ell\gg \beta,

SCFTβ([0,])=πc3β+O(1).S_{\rm CFT}^{\beta}([0,\ell]) =\frac{\pi c}{3\beta}\ell+O(1).
Solution

For x1x\gg1,

sinhx=exex2ex2.\sinh x=\frac{e^x-e^{-x}}{2}\simeq \frac{e^x}{2}.

Taking

x=πβ,x=\frac{\pi\ell}{\beta},

we find

log[βπϵsinh(πβ)]log[β2πϵ]+πβ.\log\left[ \frac{\beta}{\pi\epsilon} \sinh\left(\frac{\pi\ell}{\beta}\right) \right] \simeq \log\left[\frac{\beta}{2\pi\epsilon}\right] + \frac{\pi\ell}{\beta}.

Therefore

SCFTβ([0,])c3πβ+c3log[β2πϵ].S_{\rm CFT}^{\beta}([0,\ell]) \simeq \frac{c}{3}\frac{\pi\ell}{\beta} + \frac{c}{3}\log\left[\frac{\beta}{2\pi\epsilon}\right].

The second term is independent of \ell, so

SCFTβ([0,])=πc3β+O(1).S_{\rm CFT}^{\beta}([0,\ell]) =\frac{\pi c}{3\beta}\ell+O(1).

Consider the schematic generalized entropy

Sgen(σ)=Φh+Φhσ4GN+S0matterc6logσϵ.S_{\rm gen}(\sigma) = \frac{\Phi_h+\Phi'_h\sigma}{4G_N} +S_0^{\rm matter} -\frac{c}{6}\log\frac{\sigma}{\epsilon}.

Find the extremal value σ\sigma_* and determine whether it is a local minimum.

Solution

Differentiate:

dSgendσ=Φh4GNc6σ.\frac{dS_{\rm gen}}{d\sigma} = \frac{\Phi'_h}{4G_N}-\frac{c}{6\sigma}.

Setting this to zero gives

σ=2cGN3Φh.\sigma_*= \frac{2cG_N}{3\Phi'_h}.

The second derivative is

d2Sgendσ2=c6σ2>0.\frac{d^2S_{\rm gen}}{d\sigma^2} = \frac{c}{6\sigma^2}>0.

Thus the extremum is a local minimum.

Suppose the no-island entropy is

Sno(t)=stht,sth=πc3β,S_{\rm no}(t)=s_{\rm th}t, \qquad s_{\rm th}=\frac{\pi c}{3\beta},

and the island entropy is approximately constant,

Sisland(t)=SBH.S_{\rm island}(t)=S_{\rm BH}.

Estimate tPaget_{\rm Page}.

Solution

The Page transition occurs when the two saddles have equal generalized entropy:

Sno(tPage)=Sisland(tPage).S_{\rm no}(t_{\rm Page})=S_{\rm island}(t_{\rm Page}).

Thus

sthtPage=SBH.s_{\rm th}t_{\rm Page}=S_{\rm BH}.

Using

sth=πc3β,s_{\rm th}=\frac{\pi c}{3\beta},

we obtain

tPage=SBHsth=3βπcSBH.t_{\rm Page}=\frac{S_{\rm BH}}{s_{\rm th}} =\frac{3\beta}{\pi c}S_{\rm BH}.

This estimate assumes the black-hole entropy changes slowly compared with the entropy production rate.

Exercise 6: Why the island saddle is not a violation of no-cloning

Section titled “Exercise 6: Why the island saddle is not a violation of no-cloning”

After the Page time, the radiation entanglement wedge includes an island behind the horizon. Explain why this does not mean that the same independent quantum information exists both inside the black hole and in the radiation as two separate copies.

Solution

The island statement is a statement about reconstruction in a gravitational code. It says that operators in the island have representatives acting on the radiation Hilbert space, within an appropriate code subspace. It does not say that there are two independent tensor-factor copies of the same degrees of freedom.

This is analogous to quantum error correction. A logical operator can have multiple physical reconstructions on different sets of physical qubits, but the logical degree of freedom is not duplicated as independent quantum data. The different reconstructions are different representatives of the same encoded operator.

In gravitational language, after the Page transition the island lies in the entanglement wedge of the radiation. The interior description and the radiation reconstruction are complementary descriptions inside the code, not two independent copies violating monogamy or no-cloning.