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Radial Teukolsky Equation and Physical Solutions

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The separated radial Teukolsky equation becomes a physical problem only after its basis solutions, asymptotic phases, and flux normalization are declared. “Ingoing” and “upgoing” name global solutions by what is absent at a past boundary, not merely by the sign of a local exponential. This page fixes those meanings for e−iωt+imϕe^{-i\omega t+im\phi}, derives the constant weighted Wronskian, and distinguishes retarded scattering data from quasinormal and bound-state conditions.

Required background. Frames, Coframes, and Anholonomy supplies the tetrad weights needed to interpret horizon asymptotics.

Helpful background. Black-Hole Geometry and Mechanics supplies Kerr horizon generators; PDEs and Green Functions for Gravitation supplies Green functions, Wronskians, and boundary-value problems; Formulations of General Relativity supplies characteristic fluxes and constraints.

Radial operator and characteristic frequencies

Section titled “Radial operator and characteristic frequencies”

In the subextremal Kerr exterior define

Δ=(r−r+)(r−r−),r±=GM±(GM)2−a2,\Delta=(r-r_+)(r-r_-), \qquad r_\pm=GM\pm\sqrt{(GM)^2-a^2},

and use the radial equation

Δ−sddr(Δs+1dRdr)+[K2−2is(r−GM)KΔ+4isωr−λ]R=T(r),\Delta^{-s}\frac{d}{dr} \left(\Delta^{s+1}\frac{dR}{dr}\right) +\left[ \frac{K^2-2is(r-GM)K}{\Delta} +4is\omega r-\lambda \right]R=T(r),

where K=(r2+a2)ω−amK=(r^2+a^2)\omega-am and λ=Asℓm+a2ω2−2amω\lambda=A_{s\ell m}+a^2\omega^2-2am\omega. The field convention and projected source normalization are those fixed in the derivation page; rescaling RR rescales every amplitude below.

Choose a tortoise coordinate by

dr∗dr=r2+a2Δ.\frac{dr_*}{dr}=\frac{r^2+a^2}{\Delta}.

Then r∗→−∞r_*\to-\infty at the future event horizon and r∗→+∞r_*\to+\infty at spatial infinity. The horizon generator is χH=∂t+ΩH∂ϕ\chi_H=\partial_t+\Omega_H\partial_\phi, with ΩH=a/(r+2+a2)\Omega_H=a/(r_+^2+a^2), so the horizon-frame frequency is

kH=ω−mΩH.k_H=\omega-m\Omega_H.

The factor e−ikHr∗e^{-ik_Hr_*} is ingoing at the future horizon when combined with e−iωt+imϕe^{-i\omega t+im\phi} and a horizon-regular angular coordinate. Powers of Δ\Delta additionally depend on ss and on whether the Kinnersley or a regular tetrad component is used. Teukolsky gives these Frobenius behaviors and their physical interpretation at both boundaries Teukolsky 1973, § V, Eqs. (5.1)–(5.8), (5.10)–(5.11), printed pp. 642–643.

The radial powers can be derived rather than memorized. Put d=r+−r−d=r_+-r_-, DH=r+2+a2D_H=r_+^2+a^2 and x=r−r+x=r-r_+. Near the horizon, Δ=dx+O(x2)\Delta=dx+O(x^2) and r∗=(DH/d)log⁡x+O(1)r_*=(D_H/d)\log x+O(1). Inserting R∼xpR\sim x^p in the homogeneous equation gives, with bH=DHkH/db_H=D_Hk_H/d,

p(p+s)+bH2−isbH=(p−ibH)(p+s+ibH)=0.p(p+s)+b_H^2-isb_H=(p-ib_H)(p+s+ib_H)=0.

The roots give eikHr∗e^{ik_Hr_*} and Δ−se−ikHr∗\Delta^{-s}e^{-ik_Hr_*}. At infinity, insert R=eηiωr∗rpR=e^{\eta i\omega r_*}r^p, where η=±1\eta=\pm1. The first uncancelled coefficient, after division by rRrR, is 2iω[η(p+s+1)+s]2i\omega[\eta(p+s+1)+s]. Thus the incoming power is p=−1p=-1 and the outgoing power is p=−2s−1p=-2s-1.

For real nonzero ω\omega away from thresholds, fix an “in” solution by

Rin∼{BtransΔ−se−ikHr∗,r→r+,Bincr−1e−iωr∗+Brefr−2s−1e+iωr∗,r→∞,R^{\mathrm{in}}\sim \begin{cases} B^{\mathrm{trans}}\Delta^{-s}e^{-ik_Hr_*},&r\to r_+,\\ B^{\mathrm{inc}}r^{-1}e^{-i\omega r_*} +B^{\mathrm{ref}}r^{-2s-1}e^{+i\omega r_*},&r\to\infty, \end{cases}

and an “up” solution by

Rup∼{Cupe+ikHr∗+CrefΔ−se−ikHr∗,r→r+,Ctransr−2s−1e+iωr∗,r→∞.R^{\mathrm{up}}\sim \begin{cases} C^{\mathrm{up}}e^{+ik_Hr_*} +C^{\mathrm{ref}}\Delta^{-s}e^{-ik_Hr_*},&r\to r_+,\\ C^{\mathrm{trans}}r^{-2s-1}e^{+i\omega r_*},&r\to\infty. \end{cases}

For s=−2s=-2, these reduce to the familiar Δ2e−ikHr∗\Delta^2e^{-ik_Hr_*} transmitted factor and r3e+iωr∗r^3e^{+i\omega r_*} outgoing factor. Sasaki and Tagoshi give exactly this gravitational normalization and use it to construct the retarded sourced solution Sasaki–Tagoshi 2003, § 2.1, Eqs. (14)–(20), printed p. 9. Different rescaled variables have different powers; phases and fluxes, after reconstruction, are the invariant comparison.

The names describe causal scattering bases. RinR^{\mathrm{in}} has no wave emerging from the past horizon; RupR^{\mathrm{up}} has no wave incident from past null infinity. Teukolsky and Press emphasize that opposite-spin representations can be mathematically better conditioned in different asymptotic regions Teukolsky–Press 1974, §§II–IV, pp. 444–453.

Call the zeroth-order bracket in the raw radial equation UsU_s. Multiplying the homogeneous equation by Δs\Delta^s puts its derivative part in Sturm–Liouville form:

ddr(Δs+1dRdr)+ΔsUsR=0.\frac{d}{dr}\left(\Delta^{s+1}\frac{dR}{dr}\right) +\Delta^s U_sR=0.

For any two solutions R1,R2R_1,R_2 of the same (s,ℓ,m,ω)(s,\ell,m,\omega) equation,

Ws[R1,R2]=Δs+1(R1dR2dr−R2dR1dr)W_s[R_1,R_2] =\Delta^{s+1} \left(R_1\frac{dR_2}{dr}-R_2\frac{dR_1}{dr}\right)

is independent of rr. Differentiate it, substitute both equations, and the potential terms cancel. This weighted Wronskian is the normalization invariant needed for variation of parameters; the unweighted expression is generally not constant.

Let W=Ws[Rin,Rup]≠0W=W_s[R^{\mathrm{in}},R^{\mathrm{up}}]\ne0 and, for definiteness, take TT to have compact radial support strictly inside the exterior. Distributions with that support are allowed. The ingoing/outgoing radial solution is

R(r)=1W[Rup(r)∫r+rRin(r′)Δ(r′)sT(r′) dr′+Rin(r)∫r∞Rup(r′)Δ(r′)sT(r′) dr′].\begin{aligned} R(r)=\frac1W\bigg[& R^{\mathrm{up}}(r)\int_{r_+}^{r}R^{\mathrm{in}}(r')\Delta(r')^sT(r')\,dr'\\ &+R^{\mathrm{in}}(r)\int_{r}^{\infty}R^{\mathrm{up}}(r')\Delta(r')^sT(r')\,dr' \bigg]. \end{aligned}

The factors of Δs\Delta^s follow from the exact source normalization; importing a formula for Δ−2T\Delta^{-2}T without translating the equation changes the amplitude. Outside the source the solution is outgoing at infinity and ingoing at the horizon. Noncompact sources require separate convergence and boundary hypotheses. The retarded time-domain field is obtained by causal Fourier–Laplace inversion, continuing the resolvent from the upper half-plane (the ω+i0\omega+i0 prescription where its boundary value exists); a bare real-frequency formula does not select that contour.

Flux normalization and Starobinsky identities

Section titled “Flux normalization and Starobinsky identities”

A raw Teukolsky amplitude is not itself energy flux. We now make the conversion explicit for a vacuum gravitational in-scattering mode with real ω>0\omega>0, kH≠0k_H\ne0, ℓ≥2\ell\ge2 and regular angular eigenfunctions. The rates are quadratic, cycle-averaged Killing-energy fluxes; an eternal monochromatic wave does not have finite total radiated energy. Keep the chapter’s angular normalization:

δΨ4=ρNP4R−2 −2S(θ)e−iωt+imϕ,∫0π∣sS∣2sin⁡θ dθ=1.\delta\Psi_4=\rho_{NP}^4 R_{-2}\,{}_{-2}S(\theta) e^{-i\omega t+im\phi}, \qquad \int_0^\pi |{}_sS|^2\sin\theta\,d\theta=1.

There is no 1/2π1/\sqrt{2\pi} in this separation. Hence the squared norm of SeimϕS e^{im\phi} on the full sphere is 2π2\pi. The complex curvature field encodes two real strains; do not take its real part as though it were one real scalar and insert an extra factor 1/21/2 into the following rates.

Write Zin=BincZ_{\rm in}=B^{\rm inc}, Zout=BrefZ_{\rm out}=B^{\rm ref} and ZH=BtransZ_H=B^{\rm trans} for the s=−2s=-2 coefficients. For the companion physical δΨ0=R+2 +2Se−iωt+imϕ\delta\Psi_0=R_{+2}\,{}_{+2}S e^{-i\omega t+im\phi}, let YinY_{\rm in}, YoutY_{\rm out} and YHY_H multiply the respective branches r−1e−iωr∗r^{-1}e^{-i\omega r_*}, r−5eiωr∗r^{-5}e^{i\omega r_*} and Δ−2e−ikHr∗\Delta^{-2}e^{-ik_Hr_*}. Put μ=GM\mu=GM and

λ=λ−2,λ+2=λ−4,κH=r+−r−2DH,ϵH=κH2.\lambda=\lambda_{-2},\qquad \lambda_{+2}=\lambda-4, \qquad \kappa_H=\frac{r_+-r_-}{2D_H}, \qquad \epsilon_H=\frac{\kappa_H}{2}.

Choose the relative angular phases used by Teukolsky and Press. The Starobinsky constant is then specified by

∣C∣2=[(λ+2)2+4amω−4a2ω2][λ2+36amω−36a2ω2]+(2λ+3)(96a2ω2−48amω)+144ω2(μ2−a2),Im⁡C=12μω,Re⁡C=+∣C∣2−(12μω)2.\begin{aligned} |\mathcal C|^2={}&[(\lambda+2)^2+4am\omega-4a^2\omega^2] [\lambda^2+36am\omega-36a^2\omega^2]\\ &+(2\lambda+3)(96a^2\omega^2-48am\omega) +144\omega^2(\mu^2-a^2),\\ \operatorname{Im}\mathcal C={}&12\mu\omega,\\ \operatorname{Re}\mathcal C={}&+\sqrt{|\mathcal C|^2-(12\mu\omega)^2}. \end{aligned}

The angular adjoint identity makes the radicand nonnegative for the regular real-frequency eigenfunction; Im⁡C≠0\operatorname{Im}\mathcal C\ne0 makes C\mathcal C nonzero in this sector. Notice the μ2\mu^2 in the last term: the original printed Eq. (3.23) omits the mass square. The dimensionally consistent expression is printed in Sasaki–Tagoshi 2003, § 5.6, Eq. (176), p. 41, PDF.

Define D∓=∂r∓iK/Δ\mathcal D_\mp=\partial_r\mp iK/\Delta. For the physical-field radial functions, the complete fourth-order identities are

D−4R−2=C4R+2,Δ2D+4(Δ2R+2)=4CˉR−2.\mathcal D_-^4R_{-2}=\frac{\mathcal C}{4}R_{+2}, \qquad \Delta^2\mathcal D_+^4(\Delta^2R_{+2})=4\bar{\mathcal C}R_{-2}.

These identities relate the same physical perturbation, not independently normalized arbitrary solutions. Teukolsky and Press’s intermediate negative-spin radial function is multiplied by C\mathcal C when forming their physical field; that factor has already been absorbed into our R−2R_{-2} Teukolsky–Press 1974, § III, Eqs. (3.22), (3.28)–(3.30), pp. 447–448, PDF. Applying the identities to the endpoint expansions gives

CYin=64ω4Zin,4ω4Yout=CˉZout,CYH=64DH4ikH(kH2+4ϵH2)(4ϵH−ikH)ZH.\begin{aligned} \mathcal C Y_{\rm in}&=64\omega^4Z_{\rm in},\\ 4\omega^4Y_{\rm out}&=\bar{\mathcal C}Z_{\rm out},\\ \mathcal C Y_H&=64D_H^4ik_H(k_H^2+4\epsilon_H^2) (4\epsilon_H-ik_H)Z_H. \end{aligned}

For example, D−\mathcal D_- acting on the incoming infinity phase has leading factor −2iω-2i\omega; its fourth power and the outer factor four give 64ω464\omega^4. Near the horizon the four factors acting on x2−iDHkH/dx^{2-iD_Hk_H/d} are 2−j−2iDHkH/d2-j-2iD_Hk_H/d for j=0,1,2,3j=0,1,2,3. Their product gives the last line. The outgoing relation follows most directly from the second fourth-order identity Teukolsky–Press 1974, Eqs. (4.10)–(4.11), (4.42), pp. 449, 451, PDF.

At infinity use retarded time uret=t−r∗u_{\rm ret}=t-r_*. In the Kinnersley frame the outgoing curvature obeys Ψ4=∂uret2(h+−ih×)/2\Psi_4=\partial_{u_{\rm ret}}^2(h_+-ih_\times)/2. Integrating ⟨∣∂uret(h+−ih×)∣2⟩r2/(16πG)\langle|\partial_{u_{\rm ret}}(h_+-ih_\times)|^2\rangle r^2/(16\pi G) over the sphere therefore gives the reflected rate below. The incoming Kinnersley curvature has the corresponding coefficient two, rather than one half. At the horizon one instead uses the regular-tetrad shear and the area balance. The symmetric null frame in Metric Reconstruction and Radiative Observables instead gives an outgoing coefficient one. Its boost to the asymptotic Kinnersley frame multiplies the outgoing null leg by 2\sqrt2 and the ingoing leg by 1/21/\sqrt2, halving Ψ4\Psi_4; physical strain and power do not change. With the endpoint conversions already applied, the rates are

Finc=∣Yin∣232Gω2=128ω6G∣C∣2∣Binc∣2,Fref=∣Bref∣22Gω2,FH=ω∣YH∣232GkH(kH2+4ϵH2)DH3=128DH5ωkH(kH2+4ϵH2)(kH2+16ϵH2)G∣C∣2∣Btrans∣2.\begin{aligned} \mathcal F_{\rm inc} &=\frac{|Y_{\rm in}|^2}{32G\omega^2} =\frac{128\omega^6}{G|\mathcal C|^2}|B^{\rm inc}|^2,\\ \mathcal F_{\rm ref} &=\frac{|B^{\rm ref}|^2}{2G\omega^2},\\ \mathcal F_H &=\frac{\omega|Y_H|^2} {32Gk_H(k_H^2+4\epsilon_H^2)D_H^3}\\ &=\frac{128D_H^5\omega k_H(k_H^2+4\epsilon_H^2)(k_H^2+16\epsilon_H^2)} {G|\mathcal C|^2}|B^{\rm trans}|^2. \end{aligned}

Infinity reflection is positive outward; horizon transmission is positive inward. The horizon expression includes the boost from the Kinnersley to the regular Hawking–Hartle tetrad and the shear response; it is not a raw Weyl amplitude squared Teukolsky–Press 1974, Eqs. (4.12)–(4.16), (4.38)–(4.44), pp. 449–451, PDF. If instead one uses the unit-sphere harmonic Ys=Sseimϕ/2π\mathbb Y_s=S_s e^{im\phi}/\sqrt{2\pi}, the radial coefficients become B=2πB\mathcal B=\sqrt{2\pi}B. The familiar expression ∣Bref∣2/(4πGω2)|\mathcal B^{\rm ref}|^2/(4\pi G\omega^2) is then the same reflected rate, not a competing normalization.

The horizon rate has the sign of kHk_H for ω>0\omega>0. Moreover,

FJ,H=mωFH,Fχ=FH−ΩHFJ,H=kHωFH≥0.\mathcal F_{J,H}=\frac m\omega\mathcal F_H, \qquad \mathcal F_\chi=\mathcal F_H-\Omega_H\mathcal F_{J,H} =\frac{k_H}{\omega}\mathcal F_H\ge0.

Thus 0<ω<mΩH0\lt\omega\lt m\Omega_H permits negative ∂t\partial_t Killing-energy flux into the hole while the generator flux stays nonnegative. This is not a negative local energy measured by every horizon-crossing observer.

The unconjugated same-spin Wronskian used for the Green function is not itself an energy current. To obtain the physical balance, set

Xs=Δs/2r2+a2 Rs,gs=s(r−μ)r2+a2+rΔ(r2+a2)2.X_s=\Delta^{s/2}\sqrt{r^2+a^2}\,R_s, \qquad g_s=\frac{s(r-\mu)}{r^2+a^2} +\frac{r\Delta}{(r^2+a^2)^2}.

Direct substitution gives ∂r∗2Xs+VsXs=0\partial_{r_*}^2X_s+V_sX_s=0, where

Vs=K2−2is(r−μ)K+Δ(4isωr−λs)(r2+a2)2−gs2−∂r∗gs.V_s=\frac{K^2-2is(r-\mu)K+\Delta(4is\omega r-\lambda_s)} {(r^2+a^2)^2}-g_s^2-\partial_{r_*}g_s.

For real frequency and λ+2=λ−2−4\lambda_{+2}=\lambda_{-2}-4, these potentials satisfy V+2=Vˉ−2V_{+2}=\bar V_{-2}. Consequently

W=X+2∂r∗Xˉ−2−Xˉ−2∂r∗X+2\mathscr W=X_{+2}\partial_{r_*}\bar X_{-2} -\bar X_{-2}\partial_{r_*}X_{+2}

is constant: differentiation cancels the two identical potentials. Its endpoint values, in the physical amplitude convention above, are

W∞=2iω(YinZˉin−YoutZˉout),WH=2DH(4ϵH+ikH)YHZˉH.\begin{aligned} \mathscr W_\infty &=2i\omega(Y_{\rm in}\bar Z_{\rm in} -Y_{\rm out}\bar Z_{\rm out}),\\ \mathscr W_H&=2D_H(4\epsilon_H+ik_H)Y_H\bar Z_H. \end{aligned}

Substitute the three Starobinsky amplitude relations and multiply the equality by ω/(iGCˉ)\omega/(iG\bar{\mathcal C}). Every coefficient is then a physical flux coefficient:

Finc−Fref=FH.\mathcal F_{\rm inc}-\mathcal F_{\rm ref}=\mathcal F_H.

This is the radial proof of gravitational scattering balance Teukolsky–Press 1974, § V, Eqs. (5.2)–(5.8), p. 452, PDF. For Binc≠0B^{\rm inc}\ne0, define energy reflection and transmission fractions:

RE=∣C∣2256ω8∣BrefBinc∣2,TE=DH5kH(kH2+4ϵH2)(kH2+16ϵH2)ω5∣BtransBinc∣2,RE+TE=1.\begin{aligned} \mathcal R_E&=\frac{|\mathcal C|^2}{256\omega^8} \left|\frac{B^{\rm ref}}{B^{\rm inc}}\right|^2,\\ \mathcal T_E&=\frac{D_H^5 k_H(k_H^2+4\epsilon_H^2)(k_H^2+16\epsilon_H^2)} {\omega^5}\left|\frac{B^{\rm trans}}{B^{\rm inc}}\right|^2,\\ \mathcal R_E+\mathcal T_E&=1. \end{aligned}

Superradiance means TE<0\mathcal T_E\lt0 and RE>1\mathcal R_E\gt1 when transmission is nonzero. The unequal dimensions of the raw coefficients provide a quick warning against identifying amplitude ratios with energy fractions: since R−2R_{-2} has dimension L2L^2, the dimensions of Binc,Bref,BtransB^{\rm inc},B^{\rm ref},B^{\rm trans} are respectively L3,L−1,L−2L^3,L^{-1},L^{-2}.

Boundary conditions define different problems on the same ODE:

  • A retarded sourced solution is future-horizon ingoing and future-null-infinity outgoing, with the frequency contour fixed by causal continuation.
  • A quasinormal mode satisfies the same homogeneous boundary directions but only at discrete complex ω\omega where W(ω)=0W(\omega)=0 on the stated analytic sheet.
  • A scattering solution at real ω\omega retains an incident component at one past boundary and measures reflected and transmitted flux.
  • A massive bound or quasibound state would require a different field equation and an exponentially decaying infinity condition; the massless Teukolsky equation written here does not acquire that condition by relabeling its solutions.

Thresholds ω=0\omega=0 and kH=0k_H=0, extremality r+=r−r_+=r_-, and complex frequency change the Frobenius structure and must be treated separately. The formulas above assume subextremality and ordinary nonzero characteristic frequencies.

For s=0s=0 and real ω>0\omega>0, suppose Rin∼(e−iωr∗+Reiωr∗)/rR^{\mathrm{in}}\sim(e^{-i\omega r_*}+\mathcal R e^{i\omega r_*})/r at infinity and Rin∼Te−ikHr∗R^{\mathrm{in}}\sim\mathcal T e^{-ik_Hr_*} at the horizon. Derive the constant-current relation and decide when reflected flux exceeds incident flux. Repeat the normalization using u=r2+a2Ru=\sqrt{r^2+a^2}R.

Solution

For s=0s=0 the potential is real at real ω\omega, so the conserved current is

J=Δ2i(R∗dRdr−RdR∗dr).J=\frac{\Delta}{2i} \left(R^*\frac{dR}{dr}-R\frac{dR^*}{dr}\right).

Since Δ d/dr=(r2+a2)d/dr∗\Delta\,d/dr=(r^2+a^2)d/dr_*, the infinity 1/r1/r falloff cancels the leading r2r^2 factor there. The incident/reflected cross terms cancel in the current, giving

J∞=ω(∣R∣2−1),J_\infty=\omega(|\mathcal R|^2-1),

where outward radial orientation is positive. At the horizon,

JH=−DHkH∣T∣2.J_H=-D_Hk_H|\mathcal T|^2.

Constancy gives

1−∣R∣2=DHkHω∣T∣2.1-|\mathcal R|^2 =\frac{D_Hk_H}{\omega}|\mathcal T|^2.

The horizon area factor is not a common factor that can be cancelled at both ends. For u=r2+a2Ru=\sqrt{r^2+a^2}R, direct differentiation instead gives J=Im⁡(uˉ∂r∗u)J=\operatorname{Im}(\bar u\partial_{r_*}u) exactly. Its horizon amplitude is Tu=DHT\mathcal T_u=\sqrt{D_H}\mathcal T, so the same result is 1−∣R∣2=(kH/ω)∣Tu∣21-|\mathcal R|^2=(k_H/\omega)|\mathcal T_u|^2. If kH<0k_H\lt0 and transmission is nonzero, then ∣R∣2>1|\mathcal R|^2\gt1. For s=±2s=\pm2 the complex same-spin potential precludes this scalar-current argument; the opposite-spin conversion above is essential.

Set a=0a=0 in the gravitational flux conversion. Show that the Starobinsky constant has the expected spherical polynomial and explain why the raw reflection amplitude still is not an energy fraction.

Solution

Now λ=(ℓ−1)(ℓ+2)\lambda=(\ell-1)(\ell+2) and λ+2=ℓ(ℓ+1)\lambda+2=\ell(\ell+1), so

∣C∣2=[(ℓ−1)ℓ(ℓ+1)(ℓ+2)]2+144(GM)2ω2.|\mathcal C|^2=[(\ell-1)\ell(\ell+1)(\ell+2)]^2 +144(GM)^2\omega^2.

It is nonzero for ℓ≥2\ell\ge2. The ratio ∣Bref/Binc∣2|B^{\rm ref}/B^{\rm inc}|^2 has dimension L−8L^{-8}; the factor ∣C∣2/(256ω8)|\mathcal C|^2/(256\omega^8) is still needed to form RE\mathcal R_E. Since ΩH=0\Omega_H=0, kH=ω>0k_H=\omega>0 and TE≥0\mathcal T_E\ge0, giving RE≤1\mathcal R_E\le1 as expected for Schwarzschild scattering.

  • Sasaki, Misao, and Hideyuki Tagoshi. “Analytic Black Hole Perturbation Approach to Gravitational Radiation.” Living Reviews in Relativity 6 (2003): article 6. DOI. Open PDF.
  • Teukolsky, Saul A. “Perturbations of a Rotating Black Hole. I. Fundamental Equations for Gravitational, Electromagnetic, and Neutrino-Field Perturbations.” Astrophysical Journal 185 (1973): 635–647. DOI.
  • Teukolsky, Saul A., and William H. Press. “Perturbations of a Rotating Black Hole. III. Interaction of the Hole with Gravitational and Electromagnetic Radiation.” Astrophysical Journal 193 (1974): 443–461. ADS record and PDF.