Mon. Not. R. Astron. Soc. 364, 253–271 (2005) doi:10.1111/j.1365-2966.2005.09572.x Optimized Nekhoroshev stability estimates for the Trojan asteroids with a symplectic mapping model of co-orbital motion C. Efthymiopoulos1 and Z. Sándor2 1 Research Centre for Astronomy and Applied Mathematics, Academy of Athens, Soranou Efessiou 4, GR-11527 Athens, Greece of Astronomy, Eötvös University, Pázmány Péter stny. 1/A, H-1117 Budapest, Hungary 2 Department Accepted 2005 August 26. Received 2005 July 26 ABSTRACT This paper reports analytic estimates of the domain of Nekhoroshev stability for the orbits of Jupiter’s Trojan asteroids calculated in the space of proper elements (D p , e p ), for a stability time exceeding the age of the Solar system (t stability = 1010 yr). The model used is a family of Hadjidemetriou mappings, for different values of the proper eccentricity e p , that represent the Poincaré sections of co-orbital motion in the Hamiltonian of the planar and circular restricted three-body problem. These explicit mappings are shown to reproduce accurately the dynamics that is implicitly induced by the corresponding Hamiltonian model. Optimal Nekhoroshev estimates are obtained by constructing the Birkhoff normal form for symplectic mappings. Our optimization is based on an ‘iterated remainder’ criterion. The asymptotic behaviour of the Birkhoff series is determined by a precise analysis of the accumulation of small divisors in the series terms at consecutive orders of normalization. About 35 per cent of asteroids from a recent catalogue (AstDys), with proper inclination I p 5◦ , are shown to be Nekhoroshevstable over the age of the Solar system. By calculating a resonant Birkhoff normal form, this percentage increases to 48 per cent. Key words: celestial mechanics – minor planets, asteroids – Solar system: general. 1 INTRODUCTION A key concept in the study of non-linear dynamical systems is the concept of exponential stability. This refers to Hamiltonian systems of n degrees of freedom of the form H (J , φ) = H0 (J ) + H1 (J , φ), (1) where (J , φ) are n-dimensional action–angle variables, H 0 and H 1 are the integrable part and the perturbation, respectively, and the Hamiltonian (1) satisfies appropriate steepness and analyticity conditions. Then for a sufficiently small the drift of all orbits in an open domain of the space of actions is exponentially slow, i.e. the following statement holds true: |J (t) − J (0)| < O( α ) for all t T , with T = O e(0 /) , b (2) where α, b and 0 are parameters depending on the number of degrees of freedom and the particular form of H 0 and H 1 . The proof of (2) is the content of the theorem of Nekhoroshev (1977) – see also Benettin et al. (1985), Lochak (1992) and Pöshel (1993). In the case of motion around an elliptic equilibrium, the effective perturbation is identified to the amplitude of oscillations, i.e. the distance of orbits from the equilibrium point. One may thus obtain E-mail: [email protected] (CE); [email protected] (ZS) C C 2005 RAS 2005 The Authors. Journal compilation times of stability that are exponentially long in the inverse of the distance from the elliptic equilibrium (Giorgilli 1988; Bazzani, Marmi & Turchetti 1990; Fassò, Guzzo & Benettin 1998; Guzzo, Fassò & Benettin 1998; Niederman 1998). Conversely, by fixing the time T, equation (2) can be used to estimate the size of a domain of stability around the equilibrium point, i.e. the maximum distance that can be reached by an orbit that remains within the domain of stability for a time at least equal to T. In Solar system dynamics, T is equal to the age of the Solar system. Before the theorem of Nekhoroshev, particular examples of exponential stability were given in the literature by Moser (1955) and Littlewood (1959a,b). However, the notion of exponential stability was overshadowed for a number of years by the parallel notion of KAM stability. The KAM theorem (Kolmogorov 1954; Arnold 1963a,b; Moser 1962) asserts stability for all times of those orbits with initial conditions belonging to a Cantor set of tori, of non-zero measure, on which the phase flow is invariant. On the other hand, exponential stability applies to all the orbits in open domains of phase space, independently of whether a particular orbit does or does not lie on an invariant torus. This global character of exponential stability renders it physically relevant to the characterization of stability in generic Hamiltonian dynamical systems. The example given by Littlewood (1959a,b) deals with a model of great interest for celestial mechanics: the Lagrangian equilateral configuration in the restricted three-body problem (RTBP). The 254 C. Efthymiopoulos and Z. Sándor Birkhoff normal form, and (b) the use of better variables as coordinates (polar instead of rectangular). The use of a computer program that performs the perturbative expansions is essential, as it allows one to calculate explicitly the size of the most important terms in the remainder series, which, in turn, determine the size of the domain of Nekhoroshev stability. Supplemented with a lemma on the accumulation of round-off errors, a computer-assisted estimate obtained in the above way acquires the status of a real theorem [see, for example, the computer-assisted proof of KAM stability in a model Hamiltonian system by Celletti, Giorgilli & Locatelli (2000)]. As explained below, the obtained estimates are quite precise even without a rigorous treatment of the round-off error. We should point out that the use of the circular RTBP as a model for Trojan dynamics is already a great simplification. This neglects all the phenomena caused by the overlapping of resonances in the secularly changing elliptic RTBP. In particular, the common practice of averaging over short-period terms with a period equal to Jupiter’s mean motion renders the averaged Hamiltonian of the planar and circular problem integrable. However, in the case of co-orbital motion, the influence of the short-period terms in determining the size of the stability region is non-negligible. In the present paper we demonstrate how the small divisors introduced by the circular RTBP model alone affect the asymptotic behaviour of the Birkhoff series and, thereby, Nekhoroshev stability. We may conclude that using a Hamiltonian model averaged over the short-period terms should be avoided in the study of Nekhoroshev stability, although it is harmless in the determination of proper elements (Beaugé & Roig 2001), which, by definition, refer to nearly integrable orbits. This implies that, besides its mathematical challenge, the optimization of Nekhoroshev estimates in the circular case already represents a physically interesting problem. The generalization of these estimates in the elliptic and secularly changing elliptic RTBP is an obvious next step that would bring the theoretical estimates closer to the physical reality. In a recent paper (Efthymiopoulos 2005), improved estimates of the size of the domain of Nekhoroshev stability of the Trojan asteroids were obtained by using a mapping model of co-orbital motion (Sándor, Érdi & Murray 2002) in the framework of the planar and circular RTBP. These estimates were expressed in terms of the asteroids’ proper element values. The region shown to be Nekhoroshev-stable corresponds to asteroids with proper eccentricity e p = 0 and proper inclination I p = 0 (with respect to Jupiter’s orbit). Asteroids with libration amplitudes up to Dp = 10.◦ 6 were shown to be Nekhoroshev-stable for a time of at least 1010 yr. The theoretically calculated libration amplitude is equal to about onethird of the value of the maximum observed libration amplitude for real asteroids (35◦ ). A comparison with real asteroids with e p 0.07 and I p 10◦ , from the catalogue of proper elements of Milani (1993), showed that about 28 per cent are included in the theoretically calculated region of stability. However, from the 667 named objects in the recent AstDys catalogue,1 only 11 per cent with I p 5◦ and e p 0.03 are included in the so-determined stability region. Now, our recently obtained improvement with respect to previous estimates was partly due to the choice of better canonical variables, that is, modified Delaunay-like variables. Nevertheless, the use of a mapping model means that these estimates are not strictly comparable to previous estimates on the same problem which were obtained with the Hamiltonian model of the circular RTBP. This following proposition is proved: If a massless particle is placed in the vicinity of either one of the two Lagrangian equidistant equilibrium points (L 4 or L 5 ), the particle will remain in the neighbourhood of the same points for a time at least as long as Tstability O exp 1 log µ 1/2 , (3) where µ is the mass parameter (ratio of mass of less massive primary to total mass of primaries), and is the amplitude of oscillations around L 4 or L 5 in a linearized approximation of the equations of motion. The proof of equation (3) is based on an analytic calculation of formal integrals, i.e. asymptotic series of the canonical variables corresponding to approximate integrals of motion valid over exponentially long times. The production of such integrals in an indirect way, i.e. by the normal form of Birkhoff (1920), lies also at the core of the so-called ‘analytical part’ of Nekhoroshev’s theorem. The logarithm of in the estimate (3) can be removed by a better treatment of the number theoretical properties of the ratio of fundamental frequencies of oscillation around L 4 and L 5 . As a result, one is led from equation (3) to equation (2). Furthermore, in the framework of the elliptic restricted three-body problem, it is possible to show that the necessary conditions for applying Nekhoroshev’s theorem are fulfilled in a phase space open neighbourhood around the triangular points (Benettin, Fassò & Guzzo 1998). The best-studied example of a Lagrangian equilateral configuration in our Solar system is the population of Trojan asteroids at the L 4 and L 5 equilibrium points of the Sun–Jupiter system (see Érdi 1997, for a review). The dynamics of the Trojan asteroids has been the subject of intense research in recent years, mostly by numerical (e.g. Levison, Shoemaker & Shoemaker 1997; Tsiganis, Dvorak & Pilat-Lohinger 2000; Tsiganis, Varvoglis & Dvorak 2005; Dvorak & Schwarz 2005; Robutel, Gabern & Jorba 2005) or semi-analytical (Milani 1993; Beaugé & Roig 2001; Sándor & Érdi 2003) methods. Such investigations have revealed a rich resonant structure at the boundary of the domain of stability around L 4 or L 5 . Unravelling this structure seems hardly tractable by current implementations of Nekhoroshev theory. The latter, instead, seeks to determine a rigorous estimate of the size of the domain of practical stability around L 4 or L 5 for a time equal to the age of the Solar system, which is obtained by analytical means. The discovery of exoplanetary systems offers new grounds for the implementation of Nekhoroshev theory. In particular, if there is a giant planet in the habitable zone of an exoplanetary system, a habitable terrestrial planet can exist near the stable Lagrangian points of the star–giant planet system (Érdi & Sándor 2005). Thus the techniques of Nekhoroshev theory offer an analytical way to prove the existence of such stable regions around the equilateral Lagrangian points. The present paper presents optimized estimates of the size of the domain of stability of Jupiter’s Trojan asteroids in our Solar system, in the framework of the planar and circular RTBP. The first realistic estimates of the size of the region of Nekhoroshev stability around L 4 or L 5 , using the circular RTBP, were given by Giorgilli & Skokos (1997) and Skokos & Dokoumetzidis (2001). The size of the region of stability found by these authors, for a Nekhoroshev time T = 1010 yr, was about one-tenth of the size of the domain within which real asteroids are observed. Four real objects were included in the determined region of stability. This was a serious improvement compared to previous estimates on the same problem, which gave a size of only about 104 km (Simó 1989; Celletti & Giorgilli 1991). The improvement was due to (a) the use of a computer program to perform the algebra of calculation of the 1 C http://hamilton.dm.unipi.it/cgi-bin/astdys C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation Nekhoroshev stability estimates for Trojan asteroids remark notwithstanding, there are a number of reasons for which a mapping model is clearly preferable over a Hamiltonian model in the context of the study of Nekhoroshev stability. We mention here the two main reasons: (a) The natural choice of origin for perturbative expansions in the Trojan problem is the family of short-period orbits that surround the triangular equilibrium points. One such orbit corresponds to one elliptic fixed point in a Poincaré surface of section of the Hamiltonian model of the circular RTBP, for a value of the Jacobi constant equal to that of the periodic orbit. Similarly, this orbit corresponds to an elliptic fixed point in the mapping model of co-orbital motion, for a constant value of the proper eccentricity. However, in the mapping case the perturbative expansion can be explicitly carried out in the neighbourhood of the elliptic fixed point, since its position, as well as the mapping equations, are explicitly known. On the other hand, in the Hamiltonian case the short-period orbit can only be calculated numerically. Thus, the only analytically known centre for a Birkhoff expansion is the Lagrangian equilibrium point, i.e. the limit of the short-period orbits for e p = 0. This fact poses a severe restriction in the study of Nekhoroshev stability. Let us note that, in the case of the elliptic RTBP, there are no triangular equilibrium points, and therefore there is no analytically known starting point for a Birkhoff construction in the Hamiltonian case. On the other hand, the corresponding 4D symplectic mapping has elliptic fixed points (Sándor & Érdi 2003), which correspond again to bifurcations of the short-period family. Therefore, a Birkhoff construction around these points is always possible in the mapping model, while it is not possible in the Hamiltonian model. (b) Linked to the above remark, the study of stability in the neighbourhood of the short-period family is closer in spirit to Nekhoroshev’s theorem itself. In fact, this approach is equivalent to studying Nekhoroshev stability in the 1:1 ‘single resonant’ domain of the action space (Morbidelli & Guzzo 1997). A point at the centre of this domain, i.e. a short-period orbit, is transformed to an elliptic fixed point of the symplectic mapping for a specific value of e p . In view of the above remarks, our choice was to repeat the calculation of Nekhoroshev stability by constructing a mapping model for co-orbital motion, via the Hadjidemetriou (1991) method, in a way that reproduces as accurately as possible the dynamics of the Hamiltonian model of the planar and circular RTBP. At the same time, we extended the calculation to a much wider class of mapping models representing the Poincaré surface of section of the Hamiltonian model for a number of values of the proper eccentricity up to e p 0.21. This allowed us to obtain estimates covering almost the entire domain of proper elements e p and D p where real asteroids are observed. The construction of the mapping models, as well as a number of comparison tests with the corresponding Poincaré mappings in the exact Hamiltonian model, are described in Section 2. In the previous paper (Efthymiopoulos 2005), the Nekhoroshev estimates were obtained by a direct construction of formal integrals, i.e. without use of a normal form. This is the discrete analogue of the Contopoulos (1960) ‘third integral’ (see Contopoulos 2002 for a review of formal integrals). In the present paper the integrals are constructed by the Birkhoff normal form, as explained in Section 3. There are a number of advantages to this approach. The crucial quantity is the remainder of the normal-form series at a particular order of truncation r. Fixing r, the remainder is a convergent series starting with terms of order r + 1, the size of which determines the size of the domain of Nekhoroshev stability for any fixed time of stability. Our analytical treatment is based on an optimized analytical calculation C C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation 255 called ‘iterated remainder’. This is an improvement of the iterated remainder used by Bazzani et al. (1990) in their analytical proof of exponential stability in isochronous symplectic mappings. Section 4 presents the outcome of our new optimized analytical treatment. In summary, about 35 per cent of asteroids with proper elements taken from AstDys, with I p 5◦ , are shown to be Nekhoroshev-stable over the age of the Solar system. The size of the estimated domain of Nekhoroshev stability is about half the size of the domain occupied by real asteroids in the space of proper elements. Besides being, to our knowledge, the best available Nekhoroshev estimates in the literature, these estimates are quite realistic, rendering the present analytical method competitive to other numerical methods of determination of the domain of stability. The main resonances (small divisors) responsible for the asymptotic behaviour and, eventually, divergence of the formal series are analysed. A non-rigorous extension of our results by using a resonant Birkhoff normal-form construction suggests a still higher percentage (48 per cent) of Nekhoroshev-stable asteroids. Section 5 summarizes the main conclusions from the present study. 2 THE MAPPING MODEL 2.1 Derivation of the mapping model The Hamiltonian of the circular and planar restricted three-body problem is most conveniently expressed in terms of modified Delaunay-like variables (Brown & Shook 1964): x= a − 1, a x2 = τ = λ − λ , a ( 1 − e2 − 1), a (4) , (5) where a is semimajor axis, e is the eccentricity, λ is the mean longitude, is the longitude of the pericentre of the asteroid, and the primed variables refer to Jupiter. The Hamiltonian is H = H0 − µR, (6) where H0 = − 1 − (1 + x) 2(1 + x)2 (7) is the integrable part (Kepler’s problem in a frame rotating with the mean motion of Jupiter), µ = m /(m 0 + m ) = 0.000 953 875 36 is the mass parameter (m 0 is the mass of the Sun, m is the mass of Jupiter), and R is the perturbing function. The latter can be expressed as a function of the above canonical variables and of the eccentric anomaly E: R= 1 1 1 − − r cos φ + , r 2 = (r 2 − 2r cos φ + 1)1/2 , r = a(1 − e cos E), φ = τ + v − M, v − M = 2 arctan √ (1 + e)(1 − e) tan (E/2) − E + e sin E. A mapping model for Trojan asteroids can be derived by using the method proposed by Hadjidemetriou (1991), which is based on 256 C. Efthymiopoulos and Z. Sándor √ (x − 1)( 1 − e2 − 1) is a first integral of the mapping (14), which represents the connection between x (or practically a) and e. In fact, a constant value of x 2 refers to an almost constant value of e because the variation (a − a )/a is quite small. Thus, instead of x 2 we rather use e (when x = 0) as the parameter of the mapping. Furthermore, on the mapping plane, one has for the proper eccentricity of the asteroid e p = e + e, so that e p = e in the circular case. Therefore, the adopted values of e are practically equal to proper eccentricity values e p . In the sequel we shall use e p to denote both the value of the eccentricity on the Poincaré section and the value of the proper eccentricity. In order to calculate a normal form for the mapping (14), the latter should be expressed in polynomial form. This is achieved by a two-variable Taylor expansion around the period-one elliptic fixed point (τ ∗ , x ∗ ), which is located in the neighbourhood of L 4 . This fixed point is determined by finding the corresponding root of the mapping (14). Introducing the new variables u and v through τ = τ ∗ + u and x = x ∗ + v, the expansion for a fixed initial e p has the form the averaged Hamiltonian of the problem. According to Sándor et al. (2002), the averaged Hamiltonian reads H̄ = H0 − µ 1 2π 2π R dM, (8) 0 that is, the averaging is performed with respect to the mean anomaly M of the asteroid. However, it is convenient to transform the averaging process to one according to the eccentric anomaly E: 1 R̄ = 2π 2π 0 1 R dM = 2π 2π R(1 − e cos E) dE. (9) 0 We note that the averaged perturbing function depends only on the canonical variables x, τ and x2 : R̄ = R̄(x, τ, x2 ). According to Schubart (1964), during the averaging E is varied between 0 and 2π, and the other variables are kept fixed. Now, a symplectic mapping is obtained by the following mixedvariables generating function: W = xn+1 τn − Tshort [H0 (xn+1 ) + µ R̄(xn+1 , τn , x2 )], (10) where, in our case, the short period is T short = 2π. The mapping corresponds to the canonical transformation via the generating function (10), namely ∂W ∂W xn = , τn+1 = . (11) ∂τn ∂xn+1 ∂ R̄1 (x, τ, x2 ) ∂x + O(x 2 ). x=0 z n+1 = eiω0 z n , (13) τn+1 = τn − 2π ∂ R̄0 (τn , x2 ) ∂τn 1 − 2πµ ∂ R̄1 (τn , x2 ) ∂τn dH0 (xn+1 ) − 2πµ R̄1 (τn , x2 ). dxn+1 −1 z − z∗ z + z∗ √ , Y = √ , (18) 2 2i where X and Y are the normal coordinates of the linearized mapping. (In the variables u and v the invariant curves of the linearized mapping are ellipses, whose semimajor axes are rotated by an angle ϕ 0 . By a standard canonical transformation, these ellipses are transformed to concentric circles – see Appendix.) , X= (14) The averaged perturbing function R̄ and the coefficients R̄0 and R̄1 of its Taylor expansion have been calculated (via symbolic algebra manipulation software) by approximating the integral in equation (9) by a trapezoidal rule N 1 w j R(τ, x, x2 , E j )(1 − e cos E j ), R̄(τ, x, x2 ) = N 2.2 Correction of the rotation number The implementation of Hadjidemetriou’s method as above, i.e. by setting the averaged Hamiltonian equal to the perturbing term of a near-identity generating function, yields an O(T 3short ) error in the rotation number of the central elliptic point with respect to that of the Hamiltonian Poincaré surface of section. This can be readily shown by the following elementary example: Consider the stroboscopic Poincaré map, with period T short , of the harmonic oscillator Hamiltonian 1 H = ( p 2 + ω2 q 2 ). (19) 2 The rotation number of the elliptic point q = p = 0 of the stroboscopic map is, simply, rot = T short /T , where T = 2π/ω. On the j=1 (15) R̄0 (τ, x2 ) = R̄(τ, x=0, x2 ), R̄1 (τ, x2 ) = ∂ R̄(τ, x, x2 ) ∂x (17) where ω is the rotation angle of the central fixed point. The complex conjugate variables z and z ∗ are defined by which according to equation (7) leads to the explicit mapping xn+1 = xn + 2πµ (16) i, j=1 Finally, the mapping (16) is expressed in complex form by the complex conjugate variables z and z ∗ in which the linearized mapping can be written as W = x n+1 τn − 2πH0 (xn+1 ) − 2πµ R̄0 (τn , x2 ) βi j u in vnj . (1) calculation of (τ ∗ , x ∗ ) for a given value of e p , (2) two-variable Taylor expansion of the generating function (9) around τ ∗ and x∗ up to power 80 of the new variables u and v, (3) derivation of the equations of the mapping by using the expanded generating function, (4) two-variable Taylor expansion of the equations of the mapping around u = 0 and v = 0 up to order 80. (12) Denoting the constant term of the above Taylor expansion by R̄0 (τ, x2 ) and the coefficient of the first-order term by R̄1 (τ, x2 ), we obtain the generating function vn+1 = The above expansion has been obtained in the following steps. − xn+1 2µ R̄1 (τn , x2 ), i+ j=80 αi j u in vnj , i, j=1 The above equations result in an implicit mapping in the variable x n+1 . In order to derive an explicit mapping, we developed the averaged perturbing function around x = 0 up to first order: R̄(x, τ, x2 ) = R̄(x=0, τ, x2 ) + x i+ j=80 u n+1 = , x=0 where E j = 2π j/N , w 1 = w N = 1/2 and wj = 1 for 1 < j < N . −14 In our calculations we used N = 15, which value provided a 10 accuracy in evaluating R̄. (We compared R̄ with [0,2π] R dE, where this integral was evaluated by the internal numerical integration routine of the symbolic algebra manipulation program.) The mapping (14) depends on two parameters: the mass parameter µ and x 2 . For a fixed value of x 2 , the equation x2 = C C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation Nekhoroshev stability estimates for Trojan asteroids 257 other hand, if one considers the Hadjidemetriou mapping via the generating function oscillator example, the linear mapping (21) admits the family of invariant ellipses 2 1 Tshort pn+1 + ω2 qn2 , 2 one readily finds the linear symplectic mapping 2C = p 2 − ω2 Tshort qp + ω2 q 2 , W (qn , pn+1 ) = qn pn+1 + (20) 2 qn+1 = qn + Tshort pn − Tshort ω2 qn , pn+1 = pn − Tshort ω2 qn , (21) so that the rotation number of the elliptic point at the origin is r ot = 1 cos−1 2π π2 Tshort = + T 6 1− 2 ω2 Tshort 2 Tshort T 3 +O Tshort T 5 . (22) Now, in the case of the Trojan mapping, we have T short /T = 0.0807. . . at L 4 , and therefore π2 6 Tshort T 3 = 8.6 × 10 −4 −3 ∼ 10 . (23) which differ from the invariant ellipses of the Hamiltonian (19) (with H = 2C) by the presence of the non-diagonal term qp, which causes the angular deformation of the ellipses. From a dynamical point of view, this deformation can be expressed as a phase difference in the Érdi (1988) model for the long periodic variations of the Trojans’ elements. Namely, if q is identified with q = λ − λ − π/3 (for L 4 ), then the first equation in Érdi’s model, 1 a = a + dp sin θ + O dp2 , λ = λ + π + Dp cos θ + O Dp2 , 3 (24) should be replaced in the mapping case by a = a + dp sin(θ − θ0 ), where θ 0 is given by 1 Tshort ω2 , θ0 = tan−1 − 2 1 − ω2 This difference in the third digit may be thought to be not very important for the dynamics. However, Nekhoroshev estimates depend crucially on the small divisor structure of formal perturbative series, and the value of some small divisors changes appreciably due to this difference (Section 4.2). Therefore, the mappings (14) or (16) have to be corrected with respect to the rotation number. In order to do so, we simply consider as new mapping model the composition of equation (14) with the 2D rotation map U (φ) with angle φ = −2π × 10−3 . i.e. for T short T , one has θ 0 = O(T 3short ). However, this change does not appreciably affect the value of the proper elements d p and d p , in terms of which the Nekhoroshev estimates below are expressed. The difference in the proper element values between the Hamiltonian and mapping cases is given by q0,mapping − q0,hamiltonian ≡ Dp q0,hamiltonian 2.3 Comparison of the Hamiltonian and mapping models For T short /T = 0.0807. . . , one finds D p 0.8 per cent. Therefore, the proper element D p calculated by the mapping differs by less than one per cent from that calculated for the same level curve in the Poincaré section of the precise Hamiltonian. (b) The mapping sections accurately reproduce the position of the central periodic orbit as well as of higher-order periodic orbits of the Poincaré plane of the Hamiltonian model. The period-one elliptic fixed points of the mapping and of the Hamiltonian Poincaré sections correspond to the periodic orbits (having simple oval shape) of the short-period family emanating from L 4 . Fig. 2(a) shows the comparison between its calculated position in the Hamiltonian and mapping models as a function of the proper eccentricity e p . Increasing the eccentricity, the centre of libration departs from τ 0 = π/3. The mapping model follows the position of the fixed point with great precision. This agrees with the results of Namouni & Murray (2000). Furthermore, as shown in Fig. 2(b), the rotation number of the fixed point, calculated by the mapping model, shows an excellent agreement to the one derived by the Hamiltonian model (rotation numbers in both models are considered as positive). The mapping model agrees also with the Hamiltonian model as regards the positions and stability of the chains of fixed points corresponding to the 1/13, 1/14 and 1/15 resonances between the shortand long-period components. (c) Finally, the extension (maximum variations of τ and x) of the islands of stability in the Hamiltonian and mapping cases have an overall agreement, except for very small values of the eccentricity (e.g. top panels of Fig. 1), where the border of stability in the mapping model extends to a smaller distance from the centre (τ max = 2.1 in the mapping case compared to 2.3 in the Hamiltonian case), i.e. there is some more chaos at the border of the island of stability of the mapping model. In what follows we intend to show that the mapping (14) well reproduces the phase dynamics of the precise Hamiltonian model in the neighbourhood of the triangular points. To this end, it can be proven (Sándor et al. 2002) that, in the co-orbital region, mapping (14) has three period-one fixed points, which, when e p = 0, correspond precisely to the Lagrangian solutions L 3 , L 4 and L 5 . When e p = 0, these points correspond to the intersections of period-one periodic orbits that pass from the neighbourhood of the Lagrangian points by an appropriate Poincaré surface of section. Thus it is convenient to refer to them as the fixed points L3 , L4 and L5 of the mapping (14), from which L4 and L5 are elliptic fixed points, while L3 is a hyperbolic fixed point. The comparison between the phase portraits of the precise Hamiltonian and of the mapping is shown in Fig. 1. The three left-hand panels show the Poincaré surface of section (τ , x) when = 0 and ˙ < 0 in the Hamiltonian (6) of the planar and circular RTBP, for three different values of the Jacobi constant E J corresponding to three characteristic values of the proper eccentricity. The variation of the eccentricity as we move from the central fixed point L4 outwards is written above each panel. The three right-hand panels show the corresponding mapping sections derived by the explicit mapping (14) for the values of the eccentricity e p = 0.001 (top), e p = 0.06 (middle) and e p = 0.15 (bottom). The following can be observed: (a) The invariant curves in the mapping sections are angularly deformed with respect to those of the Poincaré section of the Hamiltonian case. This deformation is due to the method of production of the mapping. Namely, referring again to the harmonic C C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation π2 Tshort 2 1 = 1 − . = 8 2 T 1 − ω2 Tshort /4 (25) 258 C. Efthymiopoulos and Z. Sándor Figure 1. Comparison of the Poincaré surface of section of the Hamiltonian of co-orbital motion in the circular RTBP (equation 6, left-hand panels) with the mapping sections (right-hand panels) for e = e p = 0.001 (top), e = 0.06 (middle) and e = 0.15 (bottom). in which the point z = 0 is an elliptic fixed point, i.e. F non−linear (0, 0) = 0 and ω0 ∈ R. Assuming that the quantity ω 0 /2π, called the rotation number, is an irrational number, the aim of the nonresonant normal-form construction is to find a normalizing canonical transformation z = (ζ , ζ ∗ ), such that in the new variables (ζ , ζ ∗ ) the mapping (26) is transformed to a twist mapping In conclusion, the mapping model (14) reproduces the dynamics of the Poincaré mapping of the Hamiltonian model of co-orbital motion (equation 6) with good precision. We shall now use this mapping to obtain analytical Nekhoroshev estimates for the stability around the family of fixed points L4 (or L5 ). ζ = U (ζ, ζ∗ ) ≡ eiω(ζ ζ∗ ) ζ, 3 BIRKHOFF NORMAL FORM AND O P T I M I Z AT I O N O F N E K H O RO S H E V E S T I M AT E S (27) Consider a symplectic mapping of the plane given in complex conjugate canonical variables (z, z ∗ ), where the function ω(ζ ζ ∗ ) is equal to ω 0 plus a correction, i.e. ω(ζ ζ ∗ ) = ω 0 + ω 1 (ζ ζ ∗ ). If a transformation with the above properties exists, and the inverse function ζ = (z, z ∗ ) = −1 (z, z ∗ ) can be defined in an open domain including the origin, then the mapping (26) is called integrable. The exact integral of the mapping (27) is I = ζ ζ ∗ , or, in the old coordinates, z = F(z, z ∗ ) = eiω0 z + Fnon-linear (z, z ∗ ), I = (z, z ∗ )∗ (z, z ∗ ). 3.1 Birkhoff normal form (26) C (28) C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation Nekhoroshev stability estimates for Trojan asteroids 259 Figure 2. Comparison of the Hamiltonian (solid curves) and mapping (dashed curves with squares) models: (a) position of the elliptic fixed point corresponding to a tadpole periodic orbit on the Poincaré surface of section, and (b) rotation number of the elliptic fixed point. The level curves I = constant are invariant circles on the plane defined by the coordinates (ζ , ζ ∗ ), which correspond to closed invariant curves on the plane of the old coordinates (z, z ∗ ). The definition of the normalizing transformation and of the normal form follows by the solution of the so-called conjugation equation (Servizi et al. 1983; Bazzani et al. 1990). Namely, one may write z as z = (ζ , ζ ∗ ) = (U (ζ , ζ ∗ ), U ∗ (ζ , ζ ∗ )), or as z = F(z, z ∗ ) = F((ζ , ζ ∗ ), ∗ (ζ , ζ ∗ )). Equating the right-hand side (RHS) of these equations yields (U (ζ , ζ ∗ ), U ∗ (ζ , ζ ∗ )) = F((ζ , ζ ∗ ), ∗ (ζ , ζ ∗ )), or ( ◦ U ) (ζ, ζ∗ ) = (F ◦ ) (ζ, ζ∗ ). (29) The solution to equation (29) is obtained, step by step, by an iterative procedure. Let the mapping, normalized transformation and normal form be expanded in polynomial series of the canonical variables around the origin, F(z, z ∗ ) = e iω0 z + F2 (z, z ∗ ) + F3 (z, z ∗ ) + · · · , U (z, z ∗ ) = e iω0 ζ + U2 (ζ, ζ∗ ) + U3 (ζ, ζ∗ ) + · · · , (30) (ζ, ζ∗ ) = z + 2 (ζ, ζ∗ ) + 3 (ζ, ζ∗ ) + · · · . Then it can be readily shown that the solution of the conjugation equation (29) for the terms of order N is equivalent to the solution of the homological equation N eiω0 ζ, e−iω0 ζ∗ − N (ζ, ζ∗ ) + U N (ζ, ζ∗ ) = Q N (ζ, ζ∗ ), where QN = N N −1 ω0 ζ κ ζ∗λ = ei(κ−λ)ω0 − eiω0 ζ κ ζ∗λ , i.e. any monomial of the form ζ κ ζ λ∗ is an eigenfunction of the operator ω0 with eigenvalue equal to (ei(κ−λ) ω0 − eiω0 ). This means that the operator ω0 is invertible in the subspace of monomials, R(ω0 ) ≡ ζ κ ζ∗λ , (κ, λ) ∈ Z 2 , κ − λ = 1 , (35) called the range of ω0 . The inverse operator has the same eigenfunctions as ω0 with inverse eigenvalues, i.e. (ei(κ−λ)ω0 − eiω0 )−1 . On the other hand, the image of the subspace of monomials, N (ω0 ) ≡ ζ κ ζ∗λ , (κ, λ) ∈ Z 2 , κ − λ = 1 , (36) under the action of ω0 is just the null space, and thus N (ω0 ) is identified with to the kernel of ω0 . Following these definitions, the general solution of equation (34) is given by the relations U N = kernel terms ofQ N with respect toω0 N = −1 ω0 (Q N − U N ) + arbitrary kernel terms wrtω0 . (37) For N even, we simply have UN = 0 and there can be no arbitrary kernel terms in N . For N odd, we have in general UN = 0, while there can be one arbitrary term in N , namely [N /2]+1 [N /2] ζ∗ , N = −1 ω0 (Q N − U N ) + b N ζ N [ f ]N ≡ f N , (32) with f i meaning polynomial terms of degree i in the canonical variables for any complex function f . By introducing the linear difference operator ω0 defined as ω0 f (ζ, ζ∗ ) = f (eiω0 ζ, e−iω0 ζ∗ ) − f (ζ, ζ∗ ), C The definition of ω0 yields that ∂[]N ∂[∗ ]N ∂[]N ∂[∗ ]N − ∂ζ ∂ζ∗ ∂ζ∗ ∂ζ (38) = 1 + O(N ). and the following notation is used: [ f ]N ≡ f 1 + f 2 + · · · + f N , (34) {[]N , [∗ ]N } = k ([U ]N −1 , [U∗ ]N −1 ) k=2 ω0 N + U N = Q N . where bN is arbitrary. However, there is one more restriction imposed by the request that be a symplectic transformation. Namely, the real part of bN is determined by the request that [] N be symplectic up to order N − 1, that is Fk ([]N −1 , [∗ ]N −1 ) k=2 − (31) equation (31) takes the form (33) C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation The imaginary part of bN is left undetermined even after the symplecticity condition and it can be assigned arbitrary values. The most common choice is to set Im(bN ) = 0. 3.2 Remainder We consider now the iterative procedure after r − 1 steps, i.e. U and are defined up to r, called the order of truncation of the normal 260 C. Efthymiopoulos and Z. Sándor the same parity as k. In particular, the properties of the normal form imply that form. According to (38), the normalizing transformation z = [(ζ, ζ∗ )]r (39) gk(r ) (φ) = 0, if k r , k even, is symplectic only up to terms of order r. The mapping F(z, z ∗ ), which in general contains terms of any order beyond r, is transformed, via the normalizing transformation (39), to a new mapping in the variables (ζ , ζ ∗ ), which can be written as ζ = f (r ) (ζ, ζ∗ ) = [U ]r (ζ, ζ∗ ) + R (r ) (ζ, ζ∗ ). gk(r ) (φ) = 1, if k r , k odd. Taking the imaginary part of the principal logarithm of (44) yields the mapping of the angles (40) φ = φ + ω0 + Im (r ) The mapping (40) is symplectic also up to order r. The quantity R , called the remainder at the rth order of truncation, is an infinite series that contains all the terms beyond r produced by the terms of the original mapping F(z, z ∗ ). The fact that R (r ) is a non-symplectic perturbation to the integrable mapping [U ] r (ζ , ζ ∗ ) has no influence on the study of dynamics in the normalized variables (ζ , ζ ∗ ), because the mapping (40) is a precise transformation of the original symplectic mapping [see, for example, the use of (40) in the proof of Nekhoroshev stability by Bazzani et al. (1990)]. The mapping (40) is determined as follows: The inverse transformation ζ = (r ) (z, z ∗ ) of (39) is first determined by inverting the polynomial (39). The relevant homological equation to be solved is obtained by the identity condition z = ( (r ) (z, z ∗ ), ∗(r ) (z, z ∗ )) r , N(r ) =− r k ( (r ) , N −1 2 ρ =ρ ∗(r ) N −1 ) , f (r ) = (r ) ◦ F ◦ []r . R (rJ ) = and Rφ(r ) = , (43) . (47) ) R (rJ ,sk J s/2 eikφ (48) (r ) Rφ,sk J s/2 eikφ (49) 3.4 Nekhoroshev estimates with the one-turn remainder In order to obtain an estimate of the size of the domain of Nekhoroshev stability, for a time equal to T = 109 periods of Jupiter, we first implement the discrete analogue of the analytical treatment of the normal form of the Hamiltonian case as in Giorgilli & Skokos (1997). Essentially, one tries to prove that the remainder term R (r ) in the mapping (40) produces a quite small perturbation to the integrable dynamics induced by the normal-form term U r in the same mapping. This means that the cumulative effect of R (r ) up to the time T should be small enough that the orbits cannot escape from a properly defined area of stability. The above concepts are quantified as follows. Consider the annulus D(ρ 0 , ρ) = {ζ : 2ρ 0√ −ρ |ζ | ρ}√ determined by two nearby circles with radii ρ0 = 2J0 and ρ = 2J > ρ0 on the plane of the mapping (40). If the remainder term in the mapping (40), or its equivalent terms in the mapping (47), were absent, an orbit started anywhere on the circle |ζ | = ρ 0 would remain on the same circle for all times. However, the presence of the remainder term causes a drift of an orbit, at every step, from its initial circle to a nearby circle. If ρ is set equal to the radius of the most distant circle visited by the orbit within a time T, then the cumulative effect of the remainder ρ k−1 gk(r ) (φ) (46) k=2 ) (r ) , Rφ,sk ∈ C. with s, k ∈ Z, and R (rJ ,sk The mapping (40) is next converted to a mapping in polar coordi nates. Setting ζ = ρ eiφ and ζ = ρ eiφ , and taking into account that the normal form U starts with the term U1 = eiω0 ζ , equation (40) takes the form 1+ (r ) ρ k−1 g∗,k (φ) sr +2, |k|s 3.3 Remainder in action–angle variables ρe 1+ ∞ sr +2, |k|s The polynomial truncation [ f (r ) (ζ , ζ ∗ )] r of the series f (r ) (ζ , ζ ∗ ) should coincide with the polynomial [U ] r up to terms of order r. In the computer implementation, the two series turn out to be different as a result of cumulative error due to round-offs. Thus, by comparing the polynomials [ f (r ) ] r with [U ] r , we determine the size of the round-off error at the order of truncation r. We then check that the error, normalized to the size of [U ] r , is smaller than a prescribed tolerance (10−12 ). =e ρ k−1 gk(r ) (φ) where the remainders RJ and R φ are both derived from the remainder of the mapping (27). In particular, since the remainder R (r ) is a sum of homogeneous polynomials in the variables (ζ , ζ ∗ ), the functions RJ and R φ are given by series of the form (42) or, simply, ρ e 1+ ∞ φ = φ + ω(r ) (J ) + Rφ(r ) (φ, J ), = (r ) (F([]r (ζ, ζ∗ ), [∗ ]r (ζ, ζ∗ )), ∞ (45) J = J + R (rJ ) (φ, J ), ζ = (r ) (z , z ∗ ) = (r ) (F(z, z ∗ ), F∗ (z, z ∗ )) , which is again expanded as a trigonometric series. Finally, defining the action variable J = ρ 2 /2, the mappings (46) and (45) take the form of a perturbed twist mapping in action–angle variables, N iφ 2 k=2 for N = 2, . . . , ∞. In computer implementations, the iterative procedure is stopped at some high order M with N M and M r . A criterion for selecting the value of M is discussed below. Following the determination of (r ) , the mapping (40) is obtained by the old mapping (26) via the composition iω0 ρ k−1 gk(r ) (φ) which can be expanded in a trigonometric series by Taylor expansion of log (1 + x) around zero. On the other hand, multiplying equation (44) by its complex conjugate equation yields the mapping of polar radii (41) k=2 iφ log 1 + ∞ k=2 which leads to the recursive formulae 1(r ) = z, (44) k=2 For any fixed value of k, the functions g (rk ) (φ) are sums of trigonometric terms of the form e iK φ with K ∈ Z, |K | k and K having C C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation Nekhoroshev stability estimates for Trojan asteroids after T steps causes an uncertainty of the position of the orbit within the domain D(ρ 0 , ρ). Defining now the norm (r ) RJ D(ρ0 ,ρ) = sup R (rJ ) (φ, J ) (50) D(ρ0 ,ρ) and assuming the expansion (48), yields (r ) RJ D(ρ0 ,ρ) = sr +2, |k|s (r ) s (r ) R J ,sk ρ = R J . ρ (51) The quantity ||R (rJ ) || ρ is called the norm of the remainder at distance ρ. After N iterations of the mapping (47), the maximum distance travelled in action space is |J − J0 | N R (rJ ) D(ρ (52) 0 ,ρ) or ρ 2 − ρ02 2N R (rJ ) D(ρ 0 ,ρ) . (53) If we now fix the radii ρ 0 and ρ, the time N (number of iterations) needed to cross the annulus is bounded from below by a minimum time N min : ρ2 − ρ2 N Nmin = (r ) 0 . 2 R J D(ρ ,ρ) (54) 0 According to equation (51), the value of |R (rJ ) | D(ρ0 ,ρ) depends only on the outer radius ρ of the annulus, and it is an increasing function of ρ. Now, at the limit ρ = ρ 0 , the RHS of equation (54) yields N min = 0. This reflects the trivial fact that an orbit will certainly depart from its initial condition at the next iteration. On the other hand, at the limit ρ → ∞ one has limρ→∞ |R (rJ ) | D(ρ0 ,ρ) = ∞, yielding again N min = 0. In other words, if one looks at how long it takes an orbit to go from ρ 0 to ρ ρ 0 , one has to overestimate the speed of diffusion by its upper value at ρ, thus underestimating N min . This implies that an optimal estimate for the minimum Nekhoroshev time N min is given by the maximum of the RHS of equation (54) with respect to ρ. We set ρ2 − ρ2 Nnek = max (r ) 0 ρ 2 R J D(ρ ,ρ) (55) 0 Now, standard arguments of the normal-form theory (e.g. Bazzani et al. 1990) assert that the series R (rJ ) is convergent in a disc 0 < ρ ρ c . This allows one to express the norm of the remainder |R (rJ ) | D(ρ0 ,ρ) , given by equation (51), in terms of the size of the first-order term of the remainder only. Precisely, for any ρ ∗ ρ c , there is a positive number CJ (r , ρ F , ρ ∗ ), depending on the order of the optimization r and the radius of convergence ρ F of the original mapping, such that for any ρ with 0 < ρ < ρ ∗ one has (r ) RJ D(ρ0 ,ρ) C J (r , ρ F , ρ∗ )ρ r +2 . (56) Essentially, CJ (r , ρ F , ρ ∗ ) is equal to the first order of the remainder ) |R r(r+2 | times a coefficient that depends on the value of the radius of convergence of |R (r ) |. In particular, replacing equation (56) into equation (55) yields the optimal Nekhoroshev time Nnek = max ρ ρ 2 − ρ02 . 2C J (r , ρ F , ρ∗ )ρ r +2 (57) However, the maximum in the above equation can be calculated by simply differentiating the RHS of equation (57) with respect to ρ. The radius of the maximum is ρm = C r +2 ρ0 . r (58) C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation 261 Substituting equation (58) into equation (57) yields the optimal Nekhoroshev time, as a function of the initial radius, 1 Nnek = . (59) r (1 + 2/r )(r +2)/2 C J (r , ρ F , ρ∗ )ρ0r Fixing the value of N nek (=109 periods), we have the following lemma. Lemma 1. Assume ρ ∗ ρ c , where ρc is the radius of convergence of |R (rJ ) |. Then, for any time t N nek , an orbit of the mapping (47) with initial conditions on the circle J = ρ 20 /2, where ρ0 = 1 r (1 + 2/r )(r +2)/2 Nnek C J (r , ρ F , ρ∗ ) 1/r , (60) cannot travel a distance greater than ρ m − ρ 0 , where ρ m is given by equation (58), provided that ρ m ρ ∗ . In the computer implementation, in order to obtain an optimal estimate, one fixes the order of normalization r and the time N nek to some value, and then proceeds in the following way: (1) A first value of ρ ∗ is obtained by implementing equation (60), where CJ (r , ρ F , ρ ∗ ) is replaced by the first order of the remainder |R (rJ,r) +2 |, then equation (58), and then by setting ρ ∗ = ρ m . This is an overestimate, because |R (rJ,r) +2 | CJ (r , ρ F , ρ ∗ ). (2) The value of CJ (r , ρ F , ρ ∗ ) is calculated as follows. Provided that ρ ∗ is smaller than the radius of absolute convergence of the remainder series ρ c , the norm of the remainder series at ρ ∗ is given by (r ) R J = R (rJ ,r) +2 ρ∗r +2 + R (rJ ,r) +3 ρ∗r +3 + · · · ρ∗ ∞ (r ) s R J ,M ρ∗ , ) M ρ∗ + + R (rJ ,M (61) s=M+1 where M is the maximum order of computer expansion. The terms in equation (61) are given by the computer expansion, but the terms of order beyond M are not known explicitly. The size of these terms must be bounded from above analytically. It turns that this size is quite small, compared to the whole size of the remainder, provided that r is not very close to M. In our implementation, a coefficient B ∗ (ρ F ) is determined, where ρ F is the radius of convergence of the initial mapping (26), so that the size of the terms beyond N is incorporated into the last term of the expansion known explicitly. Namely, the following expression is precise: (r ) R J R (rJ ,r) +2 ρ∗r +2 + R (rJ ,r) +3 ρ∗r +3 + · · · ρ∗ ) M ρ∗ . + B∗ (ρ F ) R (rJ ,M (62) The determination of B ∗ (ρ F ) can be done analytically by the rigorous bounds provided in Bazzani et al. (1990). In all cases we find B ∗ (ρ F ) 2. Thus, in the computer implementation we simply substitute B ∗ (ρ F ) with a safety factor equal to 2. If, now, we determine the coefficient (r ) r +2 1 R J ,r +2 ρ∗ C J (r , ρ F , ρ∗ ) = (r ) R J ,r +2 ρ∗r +2 ) M + R (rJ ,r) +3 ρ∗r +3 + · · · + B∗ (ρ F ) R (rJ ,M ρ∗ , (63) then, for any 0 < ρ < ρ ∗ , the statement of equation (56) holds true. (3) Having fixed the value of CJ (r , ρ F , ρ ∗ ), the algorithm returns to equation (60) and determines new values for ρ 0 and ρ m . Then the algorithm goes to step 2, determining a new ρ ∗ = ρ m and a new CJ (r , ρ F , ρ ∗ ). Since the old ρ ∗ and CJ (r , ρ F , ρ ∗ ) were overestimated, the new ρ 0 , ρ ∗ = ρ m and CJ (r , ρ F , ρ ∗ ) are underestimated. 262 C. Efthymiopoulos and Z. Sándor Let us now temporarily ignore the term S (r,N ) (J , φ) and focus on the first term. This function Thus the algorithm repeats the previous steps iteratively until the differences in successive values of CJ (r , ρ F , ρ ∗ ) become smaller than a prescribed tolerance. R (rJ ,N ) (J , φ) = The value of ρ 0 determined in the last iteration determines an area of Nekhoroshev stability for which Lemma 1 holds. This is a value of ρ 0 corresponding to a particular Nekhoroshev time N nek , but also to a particular choice of normalization order r. The calculation is repeated for different normalization orders in the range 3 r M, and the optimal radius ρ nek 0 is selected as the maximum of the values ρ 0 found for different orders r. In practice, in our calculation we set M = 80, but we do not consider normalization orders beyond r = 60. Thus, the terms of at least the first 20 orders (= 80–60) of the remainder series R (r ) are known explicitly, the remaining terms representing a negligible contribution. This is an improvement as regards the precision of our estimates compared to previous estimates in the literature. For example, in Giorgilli & Skokos (1997), the total size of the remainder is estimated as twice the size of its first-order ) term R r(r+1 . Our calculations show that this is an underestimate by a factor of 1000 at the order of truncation r = 38, which results in an overestimate of the radius ρ 0 by a factor of 10001/38 1.2. ) R (rJ ,sk J s/2 sr +2, |k|s × N −1 exp ik φ + mω (J ) (r ) . (67) m=0 The sum in large parentheses is simply 1 − exp iN kω(r ) (J ) × eikφ , 1 − exp ikω(r ) (J ) and thus R (rJ ,N ) (J , φ) = sr +2, |k|s 1 − exp iN kω(r ) (J ) 1 − exp ikω(r ) (J ) ) × R (rJ ,sk J s/2 exp(ikφ). (68) Equation (68) implies that the Fourier coefficients of the iterated remainder R (r,N ) differ from the respective coefficients in the oneturn remainder by the quantity 1 − exp iN kω(r ) (J ) , 1 − exp ikω(r ) (J ) R (rJ ) J (m−1) , φ + (m − 1)ω(r ) (J ) . which for most frequencies ω(r ) (J ) is O(1). However, the most important Fourier terms in the remainder are those in which the wavenumber k is a multiple of q ∈ N ∗ , where q is the denominator of a rational approximation to ω(r ) (J ), namely ω(r ) (J ) = 2π p/q + . For these terms, it can be easily shown that, if N is equal to the denominator of a higher order rational approximation to w(r ) (J ), then (64) m=1 Since the variation of the action is small, the actions J (m) for m = 0, . . . , N − 1 are given by J (m) = J + mJ (m) , where J (m) is a quantity of the order of O(|R (rJ ) |). Thus, equation (64) takes the form RJ R (rJ ,N ) (J , φ) = while the first of equations (47) takes the form J (N ) − J = ) R (rJ ,sk J s/2 eikφ . sr +2, |k|s φ (N ) = φ + N ω(r ) (J ), (r ) (66) Equation (66) then gives If [J (N ) , φ (N ) ] denotes the Nth image of some initial point (J , φ) of the mapping, we readily obtain N R (rJ ) = φ = φ + ω(r ) (J ). will be called the N-iterated remainder of order r of the mapping (47). The key point in this definition is that N − 1 successive values of the one-turn remainder are added algebraically rather than by their absolute values. This is motivated by the physically relevant picture that the drift in action space is not realized by steps that are all in the same direction, i.e. of increasing or decreasing J (m). On the contrary, the drift in action space is the overall sum of a number of steps, each of which may cause a positive or negative variation of the action. The long-term behaviour of the N-iterated remainder can be determined by recalling that the one-turn remainder R (rJ ) is a sum of Fourier terms (equation 48) The above described estimates by the remainder of the ‘one-turn’ map can be improved further by considering an ‘iterated remainder’, which is an improvement of the iterated remainder method used by Bazzani et al. (1990). This section contains the basic formulae used in the implementation of the new method, while the technical details are deferred to the Appendix. Let us assume that for a number of iterations N N nek the variation of the action J = J fin − J from an initial value J is small enough that the frequency ω in equation (47) can be considered as practically constant, equal to its initial value ω(r ) (J ). Under this simplifying assumption, the angular part of the mapping (47) is obtained by neglecting the term R φ in equation (47) and also the variation of the action. One then has J (N ) − J = R (rJ ) J , φ + (m − 1)ω(r ) (J ) m=1 3.5 Nekhoroshev estimates with an iterated remainder N N 1 − exp iN kω(r ) (J ) = O(k 2 /N ). 1 − exp ikω(r ) (J ) J , φ + (m − 1)ω(r ) (J ) + S (r ,N ) (J , φ). (65) This means that the coefficient of a nearly resonant term in the iterated remainder can be even smaller than the coefficient of the same term in the one-turn remainder, at values of N that are multiples of the multiplicity of the respective near-resonance. In conclusion, the size of the N-iterated remainder is expected to be very similar to, or even smaller than, the size of the one-turn remainder, for N not very small. This, in turn, leads to improved estimates of the size of the area of stability. In fact, any estimate of this size based on equation (60) is improved by essentially the m=1 Equation (65) is precise if the quantity S (r,N ) (J , φ) is calculated by the full mapping (47), without the above approximations. In the Appendix, it is shown that the size of S (r,N ) (J , φ) is of the order of O(N 3 |R (rJ ) (J , φ)|2 ). Thus, if the quantity |R (rJ ) (J , φ)| is small, the second term on the RHS of equation (65) is much smaller than the first term, which is O(|R (rJ ) (J , φ)|), even for N not very small (in our calculations we find that N can be as high as N = 2000). C C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation Nekhoroshev stability estimates for Trojan asteroids factor of N 1/r , since the Nekhoroshev time for the iterated mapping is N nek = N nek /N . The precise formulae used in the computer implementation of the iterated remainder are given in the Appendix. Table 1. Optimal Nekhoroshev stability estimates. 4 R E S U LT S 0.001 0.03 0.06 0.09 0.12 0.15 0.18 0.21 e This section presents the results of the determination of the area of Nekhoroshev stability on the plane of the canonical variables (τ , x), for the mapping models determined in Section 2. An explicit symplectic mapping, as well as the normal form, remainder and iterated remainder, were calculated for each of the values of the proper eccentricity e p = 0.001, 0.03, 0.06, . . . , 0.21. Optimal order 39 41 45 53 >60 >60 >60 >60 D p (degree) one-turn iterated 11.61 11.76 11.47 11.32 12.28 10.52 7.01 5.44 12.84 12.89 12.64 12.23 12.87 11.30 7.49 5.83 263 Number of remainder iterations N 700 800 600 700 600 1300 1500 1500 4.1 The domain of Nekhoroshev stability in the space of proper elements The domain of Nekhoroshev stability is first determined as a disc on the plane of the normalized canonical variables (ζ , ζ ∗ ) centred at the origin (Section 3.1). All asteroids located within this disc are shown to be Nekhoroshev-stable for a time equal to at least N nek = 109 periods of Jupiter. The radius ρ 0 of the disc is determined by equation (60), in which the values of the optimal order of truncation r and of the reference radius ρ ∗ are determined by steps 1 to 3 of the algorithm of Section 3.4. Two different radii are calculated, corresponding to the optimal values found by the use of the one-turn remainder and of the N-iterated remainder, respectively. In the case of the one-turn remainder, the quantity CJ appearing in equation (58) is given by equation (63). In the case of the N-iterated remainder, for a fixed value of N, the radius of Nekhoroshev stability is corrected for the effect of the term S (r ,N ) ρ∗ as discussed in the Appendix. The results are transformed to proper element values by the following procedure: The disc of radius ρ 0 corresponds to a deformed disc in the original complex canonical variables (z, z ∗ ) with an outermost boundary given by z = (r ) (ρ0 eiφ , ρ0 e−iφ ), 0 φ < 2π. (69) It follows that this boundary is given in the canonical variables (u, v) (Section 2.1) by u(ρ0 , φ) = U (r ) ρ0 eiφ , ρ0 e−iφ , (r∗ ) ρ0 eiφ , ρ0 e−iφ v(ρ0 , φ) = V (r ) ρ0 eiφ , ρ0 e−iφ , (r∗ ) ρ0 eiφ , ρ0 e−iφ , (70) for 0 φ < 2π. Finally, the maximum libration amplitude for which an orbit is Nekhoroshev-stable is given by Dp = 1 (u max − u min ), 2 where (71) u max = max u(ρ0 , φ), 0 φ < 2π , φ u min = min u(ρ0 , φ), 0 φ < 2π . φ One value of D p is found for each different mapping derived for one value of e p (Table 1). Fig. 3 shows the final result. The left-hand solid line joins the points (e p , D p ) corresponding to the upper limit of D p for which we have Nekhoroshev stability with the one-turn remainder criterion. The right-hand solid line joins the points of Nekhoroshev stability determined by the N-iterated remainder. The dashed line corresponds to a criterion with the resonant Birkhoff normal form discussed below. It should be noted, however, that the precise calculation was done only on the points of Table 1 along the above lines. C C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation Figure 3. Calculated area of Nekhoroshev stability in the space (D p , e p ) with the one-turn remainder criterion (left-hand solid line), the N-turn remainder criterion (right-hand solid line) and a non-rigorous estimate with the resonant Birkhoff normal form (dashed line). Open circles correspond to real asteroids with 0 I p 5◦ which are Nekhoroshev-stable for 1010 yr with the N-turn remainder criterion, while the squares correspond to asteroids outside the area of Nekhoroshev stability. The domain shown to be Nekhoroshev-stable for 109 periods of Jupiter has an area that is about 50 per cent of the total area occupied by real asteroids on the (D p , e p ) plane. However, this area is not uniformly populated by asteroids. We have used the data of 667 numbered objects from the AstDys data base.2 It turns out that the percentage of asteroids in this catalogue shown to be Nekhoroshevstable is smaller. Precisely, 28 per cent of the asteroids (29 out of 102) with proper inclinations I p 5 are shown to be Nekhoroshevstable with the one-turn remainder criterion, and 35 per cent (36 out of 102) with the iterated remainder criterion. Our previous result was Dp = 10.◦ 6 with a simplified mapping model for e p = 0. In the AstDys catalogue, this corresponds to a percentage of 11 per cent of asteroids in the range I p 5◦ , e p 0.03. We would like to point out an apparent similarity of our analytical result to recently obtained results on the stability of Trojans by semianalytical or numerical methods (Sándor & Érdi 2003; Tsiganis et al. 2005; Robutel et al. 2005), in the framework of a much more realistic model, i.e. the elliptic RTBP including the effects of Saturn. Fig. 3 shows a rough agreement with the separation of asteroids into stable or chaotic according to a Lyapunov time criterion (T L > 400 000 yr for the stable Trojans; Tsiganis et al. 2005). This agreement may not be totally coincidental. In particular, as demonstrated by Sándor & Érdi (2003) and Robutel et al. (2005), the interaction of the indirect effects of Saturn broaden the already existing chaotic 2 http://hamilton.dm.unipi.it/cgi-bin/astdys 264 C. Efthymiopoulos and Z. Sándor of the size of the remainder, as a function of r, can be found by a detailed analysis of the propagation of small divisors in the various terms of the series [see Servizi et al. (1983) and Efthymiopoulos, Contopoulos & Giorgilli (2004) for detailed discussions of the mapping and Hamiltonian cases, respectively]. The outcome of this analysis is that the series ||R (r ) || appears as ‘piecewise geometrical’, namely, the ratio λ r =||R (r +2) /R (r ) || is almost constant within fixed intervals of values of r, but it increases by abrupt steps at particular values of r. These values are equal to r = qn + dn , with qn and dn integers, qn being the denominator of the nth member of the continued fraction sequence of ω 0 . The integer dn qn is called ‘retardation’ (Turchetti 1989) or ‘delay’ [see Efthymiopoulos et al. (2004) for an analysis and quantitative estimate of dn ]. In the case of mappings, the piecewise constant geometrical ratio λr can be defined by a generalization of the formula for the Hamiltonian case (Efthymiopoulos et al. 2004) layers in the elliptic RTBP, thus creating large overlapping domains where chaotic diffusion may take place. However, precisely because of this extended overlapping, the relevant region of phase space does not have a ‘Nekhoroshev-type’ structure (Froeschlé, Guzzo & Lega 2000). On the other hand, it is likely that the small divisors generated by the circular RTBP are the ones that produce the dominant effect of Nekhoroshev stability in most of the open circles domain of Fig. 3, even after the addition of terms induced by the elliptic problem or the effects of Saturn. This is because the relevant frequencies are well separated (Beaugé & Roig 2001), so that the divisors induced by the extra terms are expected to affect the Birkhoff series at orders of normalization well beyond the optimal orders of truncation cited in Table 1. We are currently investigating this subject in detail. 4.2 Small divisors and the divergence of the Birkhoff series It is well known that the procedure for the construction of the Birkhoff normal form (Section 3) is generically divergent (Rüssmann 1959). The precise meaning of this statement is the following: Except for a residual set of integrable mappings of the form of equation (26), one has that, while for any fixed order of truncation r, the remainder R (r ) is an absolutely convergent series, the radius of its convergence ρ (rc ) tends to zero as r tends to infinity. Therefore, it is impossible to transform a non-integrable mapping to an integrable one by this formal construction. The divergence of the Birkhoff series is attributed to the mechanism of accumulation of the so-called small divisors. The latter are quantities ar defined by 1 1 ≡ iK ω ar |e r 0 − 1| λr = max ρ r (72) r k k=2 ak , (74) 0 1 2 3 5 , , , , , .... 1 12 25 37 62 Thus, new small divisors ar appear at the orders r = 1, 12, 25, 37, 62, . . . . The values of these small divisors correspond to the local minima of the curve ar (equation 72) as a function of r (Fig. 4a). The terms containing these divisors determine a ‘piecewise geometrical’ growth of the remainder in the Birkhoff series. The corresponding ratio λ r , calculated by equation (74), is shown in Fig. 4(b). One sees that each jump to a new minimum divisor, as r increases (Fig. 4a), causes a respective jump to a higher value of the geometrical ratio λ r in Fig. 4(b). The behaviour of λ r shown in Fig. 4(b) determines the growth of the size of the remainder terms in the Birkhoff series. Fig. 4(c) shows +2) ) the ratio of the first-order terms of the remainders ||R r(r+3 /R r(r+1 || for the Birkhoff normal form of the mapping with e p = 0.001. This ratio forms ‘plateaux’ corresponding to an almost constant value for an interval of values of r. The transition from one plateau to the next is by quite abrupt steps. However, consecutive transitions appear with a delay with respect to the orders of appearance of the corresponding new small divisors. Thus, the transition to the first plateau is around the order r = 18, while the responsible divisor is a 12 , appearing at r = 12. Similarly, the transition to the second plateau is around the order r = 41, while the responsible divisor is a 25 , appearing at r = 25. Finally, the transition to the third plateau is around the order r = 70, while the responsible divisor is a 37 , appearing at r = 37. Thus the delay increases at consecutive transitions, in accordance with the theoretical predictions of Efthymiopoulos et al. (2004). +2) ) If one calculates the ratio of the value ||R r(r+3 /R r(r+1 || (Fig. 4c) over the theoretically calculated value λ r (Fig. 4b), one finds a ratio A = 7.02 for the first plateau, A = 7.93 for the second plateau, = O(r !a ρ r ), where A is a real positive constant depending on the size of the non-linear part of the mapping. The ratio λr changes value abruptly whenever r = qn , the denominator of the next fraction in the sequence of continued fraction approximations of ω 0 , or at some linear combination of the form r = mn qn + m n q n , with mn and m n integers. The above analysis reproduces quite accurately the asymptotic behaviour of the Birkhoff series in the case of the mapping (14) for the Trojan asteroids. Let us consider, for example, the small divisor structure in the case of the mapping for e p = 0.001. The rotation angle is ω 0 = 2π × 0.080 729 943 153 368 41. The first members of the continued fraction sequence of ω 0 /2π are that appear in the formal construction at every iterative step. Precisely, the form of the second recursive equation in (37) implies that the term N of the generating transformation will contain divisors of the form eiω0 ar with K r = κ − λ − 1, with κ + λ − 1 = r , which are the eigenvalues of the operator ω0 . According to well-known results of number theory (see e.g. Berry 1978), the real number ω 0 /2π is most rapidly approximated by the sequence of rational numbers pn /qn belonging to its continued fraction representation. In particular, if ω 0 /2π is irrational, the quantity ar in equation (72), being in general of order O(1), becomes though quite small [of the order of O(1/ pn )] at the precise values K r = qn . A divisor ar first appears in the series at order r = qn , and it repeatedly appears at all successive orders beyond qn . As r increases, new divisors ar , smaller than the previous ones, appear in the series whenever r becomes equal to the denominator qn of the succeeding fractions in the continued fraction sequence pn /qn . This property generates the effect of accumulation of small divisors. One can show that the size of the generating transformation, at order r, is bounded by a quantity (r ) O ρ A|κ − λ| , κ, λ ∈ N , κ + λ r |e(κ−λ)ω0 − 1| (73) where the exponent a has the value a = 2 in the case of twodimensional mappings. A similar formula holds for the size of the remainder R (r ) . The asymptotic character of the Birkhoff series follows from equation (73) [see, for example, the elementary example given in Méthodes Nouvelles (Poincaré 1892), with a = 1, ρ = 1/1000]. It should be noted that, while the bound (73) can be rigorously proven, it is by no means optimal. Optimal estimates of the growth C C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation Nekhoroshev stability estimates for Trojan asteroids 265 Figure 4. Growth of the remainder in the mapping for e p = 0.001. (a) The minimum divisor of the form (72) as a function of the order r. (b) The ratio (r +2) (r ) λ r (equation 74) as a function of r. (c) Precise calculation of the ratio of the size of the first terms of the remainder ||R r +3 /R r +1 || as a function of r. (d) Comparison of the growth of the size of the remainder (solid line with small asterisks) to the growth of the size of the mapping terms (line of open circles) in a base-10 logarithmic scale. In the latter case the growth is geometrical, while in the former case the growth ratio changes near the orders 18, 41 and 70. and A = 5.40 for the third plateau. Thus, A is not a constant. This is due to the fact that the non-linear part of the mapping contains terms beyond the order r = 3. However, the variation of A has only a small effect in the growth of the series, which is determined by the large variation of the value of the λ r at each transition to a new minimum divisor. At orders r < 12 there seems to be a small plateau around the +2) ) value ||R r(r+3 /R r(r+1 || = 100 (Fig. 4c). This plateau is not due to a small divisor, but it reflects the geometrical growth of the remainder, which follows the geometrical growth of the non-linear terms of the mapping up to the order of appearance of the first small divisor. That is, in the interval of values of r (1 r < 12), the growth of the size of the remainder is dominated by the appearance, in the Birkhoff series, of new terms generated by respective terms of the mapping (26). These terms are produced by the second term on the RHS of the solution (31) to the homological equation, while repetitions of small divisors are produced by the first term on the RHS of the same equation. For the first few orders r, the two terms have a comparable size, because the divisor (a 1 = 0.6) is of the order of unity. This effect is demonstrated in Fig. 4(d). The straight line of open circles gives the norm ||Fr || of the terms of the mapping expansion at order r. This is a convergent series, which is well represented by a geometrical progression. A power-law fit yields Fr = 0.955 × 9.226r C (75) C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation for r > 1, i.e. the radius of convergence of the polynomial mapping expansion is rF = 1/9.226 = 0.1083. Now, as shown in Fig. 4(d), the growth of the size of the remainder (upper solid curve with small asterisks) up to order r = 12 is very similar to the law (75), i.e. the two curves coincide. However, for r beyond r = 12, the series ||R (r ) || grows by a larger geometrical ratio than ||Fr ||. Furthermore, this ratio increases by an abrupt step at order 41, producing a straight segment with larger slope than the previous segment corresponding to 12 r 41. A less clear second change of the slope is at r = 70. New segments of higher and higher slope will appear at still higher orders, so that the radius of convergence of the series ||R (r ) || tends to zero as r → ∞, i.e. the Birkhoff series is asymptotically divergent. Similar phenomena are observed in all the different mappings for the values of e p = 0.3, 0.6, . . . , 0.21. The most important phenomenon is the increasing importance of the resonance 1/12 as e p increases. This is shown in Figs 5 and 6. Fig. 5 refers to the mapping for e p = 0.06, ω 0 = 2π × 0.081 331 286 276 195 97). The continued fraction sequence of ω 0 /2π is now 1/12, 3/37, . . . . Therefore, as shown in Fig. 5(c), there are now two plateaux in the remainder ratio up to order 80. The appearance of the second plateau is at order 60, meaning that the growth of the remainder is dominated by the ratio λ 12 corresponding to the divisor a 12 . As e p increases, ω 0 /2π approaches closer to the value 1/12 = 0.0833. . . (Fig. 2b). Thus, when e p = 0.15, we have 266 C. Efthymiopoulos and Z. Sándor Figure 5. Same as Fig. 4, for the mapping with e p = 0.06. The growth ratio of the remainder changes near the orders 14 and 52. ω 0 /2π = 0.082 314 483 924 536 93. The dominance of the divisor a 12 at this value of e p is clearly seen in Fig. 6. We found that the plateau due to a 12 extends up to r = 60 already at e p = 0.12. This explains why the optimal order of truncation of the series is beyond r = 60 when e p 0.12 (Table 1). Furthermore, the same phenomenon causes an abrupt turn of the boundary of the Nekhoroshev stability region to the left (Fig. 3) for e p 0.12. normalized canonical variables. This is because the level curves of formal integrals of the resonant normal form are not circles. Precisely, the new formal integrals are the level curves of the Lie generating function H (or ‘interpolating Hamiltonian’) for time t = 1, of a mapping Û which is equal to the normal-form mapping U rotated by an angle −2π p/q. To find H, one solves, order by order, the equation e D H ζ = Û (ζ, ζ∗ ), 4.3 A non-rigorous estimate with the resonant Birkhoff normal form (76) where DH stands for the Poisson bracket operator DH ≡ { · , H } and e D H is the exponential operator determined by DH . The level curves of H give ‘resonant’ formal integrals that account for both the nonresonant dynamics and the dynamics of one particular resonance. In particular, the level curves of H yield deformed circles away from the resonant domain, and island chains within the resonant domain. Even if Lemma 1 does not apply in the resonant construction, the radius given by equation (60) is expected to be a good approximation of the real size of the domain of stability if CJ is calculated by the remainder of the resonant normal form. This is because, as shown in the phase portraits of Fig. 1, the produced island chains are elongated and their shape does not deviate much from that of arcs of circles, i.e. the shape of the domain of Nekhoroshev stability is not expected to deviate much from a disc. We thus naively proceed by considering a disc of stability obtained in the following way: For each mapping, we calculate the size of the remainder ||R (rres) || of the resonant normal form and find the ratio of this quantity to the size of the remainder of the non-resonant normal form ||R (r ) ||, as a function of the order The results of the previous section strongly suggest that the rigorous estimate of the domain of Nekhoroshev stability given in Fig. 3 could be further improved by considering a resonant formal construction of the Birkhoff series (Bazzani et al. 1993). The essence of this construction is to eliminate the effect of just one divisor, by constructing a formally integrable mapping that contains resonant terms corresponding to that particular divisor. In order to do so, one solves equation (31) again by replacing the operator ω0 by a new operator µ with µ = 2π p/q, where p and q are integers and p/q is the resonance eliminated from the Birkhoff series. This new definition changes also the splitting of the space of monomials to a direct sum of kernel and range, by including new terms in the kernel. These are the terms of the form ζ k+q+1 and ζ k∗ , where k is integer and q is the denominator of the resonance (see Bazzani et al. 1993, for details). In the case of the resonant construction, Lemma 1 cannot be applied to obtain a disc of Nekhoroshev stability on the plane of C C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation Nekhoroshev stability estimates for Trojan asteroids 267 Figure 6. Same as Fig. 4, for the mapping with e p = 0.15. The growth ratio of the remainder changes near the order 12. of truncation r. We then calculate a new radius of Nekhoroshev stability ρ =ρ (r ) 1/ropt Rresopt R (ropt ) , (77) where ρ is the radius of stability found with the non-resonant normal form at the optimal order of truncation = r opt given in Table 1. Fig. 7 shows this procedure in two examples referring to the mappings for e p = 0.001 (Figs 7a and b) and e p = 0.12 (Figs 7c and d). The optimal order of truncation of the mapping for e p = 0.001 is r opt = 39 (Table 1). From Fig. 4(c) we find that just before r = 41 there is a rise of the remainder ratio due to the new small divisor a 25 . We thus construct the resonant Birkhoff normal form for the resonance p/q = 2/25. The remainder ratio for this construction is shown as the dashed curve in Fig. 7(b). Clearly, in the resonant construction, the plateau due to the previous divisor (a 12 ) survives up to r = 50, where a new jump occurs due to the divisor a 37 . On the contrary, in the non-resonant construction (solid curve with small asterisks), the plateau due to a 25 dominates the series growth for at least 10 consecutive orders below r = 50. This difference is reflected in the growth of the size of the two remainders for r 40 (Fig. 7a). Namely, the remainder of the resonant normal form at orders r 40 grows more slowly than that of the non-resonant normal form, resulting in a difference of three orders of magnitude at r = 50. This phenomenon becomes more pronounced as e p increases. Fig. 7(d) shows the difference of the size of the remainders of the non-resonant and resonant normal forms at orders r 40, which C C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation is by about six orders of magnitude. In this case, the resonant construction corresponds to the resonance p/q = 1/12, since the plateau due to a 12 dominates in the non-resonant construction up to r = 40 (Fig. 7d). The elimination of the divisor a 12 in the resonant construction causes a disappearance of this plateau and a much slower growth of the remainder of the formal series. By implementing equation (77) in all the mappings, we obtain a non-rigorous estimate of the domain of Nekhoroshev stability in the space (D p , e p ) for all the mappings with 0 e p 0.21. This is shown as a dashed line in Fig. 3. Of the asteroids with I p 5◦ from AstDys, 48 per cent (49 out of 102) are within this so-determined domain of stability. We are presently working on a rigorous treatment of Nekhoroshev estimates with the resonant Birkhoff normal form. 5 CONCLUSIONS This paper reports analytic estimates of the Nekhoroshev stability of the orbits of Jupiter’s Trojan asteroids, by calculating a region of stability in the space of proper elements (D p , e p ) for a Nekhoroshev time t = 1010 yr. The model used is a family of Hadjidemetriou mappings, for different values of the proper eccentricity e p , corresponding to the Hamiltonian of co-orbital motion in the planar and circular restricted three-body problem. Our main conclusions are as follows: (i) Except for a phase difference, the derived mappings reproduce with good precision the Poincaré surfaces of section of the Hamiltonian model. In particular, the position and rotation numbers 268 C. Efthymiopoulos and Z. Sándor Figure 7. Comparison of the growth of the size of the remainder with the resonant and non-resonant normal forms. (a) The size of the remainder of the resonant normal form (dashed line, for the resonance p/q = 2/25) and of the non-resonant normal form (solid line), as a function of r, for r 40, in the mapping with e p = 0.001. (b) Comparison of the growth ratios for the resonant (dashed) and non-resonant (solid) normal forms in the same mapping. Panels (c) and (d) are the same as (a) and (b), for the mapping with e p = 0.15. regular orbits found in other studies based on numerical integrations in the framework of the much more realistic model (elliptic RTBP including the effects of Saturn). This agreement may not be totally coincidental, because the large chaotic domains generated by the overlapping of secular resonances lie for the most part outside the domain of Nekhoroshev stability determined by the small divisors structure of the circular RTBP model. A detailed comparison of the domains of stability determined by various methods in various models is in progress. of the family of fixed points corresponding to the short-period orbit are precisely reproduced by the mappings. Furthermore, the mappings generate the same families of higher-order (long-period) island chains as in the Hamiltonian model, and at the same position. Finally, the difference in the calculation of proper element values in the mapping and Hamiltonian models is smaller than 1 per cent. (ii) An analytical theory for a rigorous calculation of a domain of Nekhoroshev stability is developed in the framework of the Birkhoff normal form for symplectic mappings. Optimized estimates are obtained by use of an iterated remainder criterion. The Birkhoff normal form is constructed for the mapping models with a computer algebra program, up to the order of expansion r = 80. AC K N OW L E D G M E N T S (iii) The calculated domain of Nekhoroshev stability (Fig. 3) comprises 35 per cent of the asteroids from the AstDys catalogue with I p 5◦ . A non-rigorous extension of the boundary of stability, by use of the resonant Birkhoff normal form, results in increasing this percentage to 48 per cent. we would like to thank Professor G. Contopoulos and Drs F. Roig and K. Tsiganis for useful discussions on the Trojan stability problem. CE received support from an Archimidis (EPEAEK) project of the Greek Ministry of Education. Part of the normal-form calculations were done on a virtual parallel machine cluster funded by Empirikion Foundation. ZS gratefully acknowledges the support of the Hungarian Scientific Research Fund (OTKA) under the grants D048424 and T043739. (iv) The accumulation of small divisors, responsible for the divergence of the Birkhoff series, is analysed. This analysis is in agreement with the theoretical predictions of Servizi et al. (1983) and with the analytical formulae for the growth of the size of the remainder given in Efthymiopoulos et al. (2004). The ‘delay’ mechanism in the accumulation of small divisors plays an important role in the choice of quasi-resonance for the construction of the resonant Birkhoff normal form. REFERENCES Arnold V. I., 1963a, Russ. Math. Surv., 18, 9 Arnold V. I., 1963b, Russ. Math. Surv., 18, 85 Bazzani A., Marmi S., Turchetti G., 1990, Celest. Mech. Dyn. Astron., 47, 333 (v) The domain of Nekhoroshev stability determined analytically by our model shows an apparent agreement with the domain of C C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation Nekhoroshev stability estimates for Trojan asteroids Bazzani A., Giovannozzi M., Servizi G., Todesco E., Turchetti G., 1993, Physica D, 64, 66 Beaugé C., Roig F., 2001, Icarus, 153, 391 Benettin G., Galgani L., Giorgilli A., 1985, Celest. 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Astron., in press Turchetti G., 1989, in Turchetti G., ed., Conf. on Nonlinear Dynamics. World Scientific, Singapore APPENDIX Transformation to normal coordinates Let the primed variables τ and x denote one iterate of the mapping (10) with initial values τ and x. Mapping (14) can be written formally as τ = τ (τ, x), x = x (τ, x). (78) Linearization around τ = τ 0 and x = x 0 , or u = v = 0, yields u =u ∂τ ∂τ +v τ0 ,x0 ∂τ ∂x , v =u τ0 ,x0 ∂x ∂τ +v τ0 ,x0 Denoting the elements of the Jacobian matrix by a11 = ∂τ ∂τ , a12 = τ0 ,x0 ∂τ ∂x , a21 = τ0 ,x0 ∂x ∂τ ∂x ∂x . (79) τ0 ,x0 , τ0 ,x0 a22 = ∂x ∂x , (80) τ0 ,x0 the following steps lead to the normal coordinates X and Y: 1 ϕ0 = arctan 2 b= a22 − a11 , a21 ωx = X= C a11 − a22 a12 + a21 c=− , (81) a12 , a21 (82) 1 cos2 ϕ0 + c sin ϕ0 − b sin 2ϕ0 , 2 ωy = 2 ωx (u cos ϕ0 − v sin ϕ0 ), ωy Y = 1 sin2 ϕ0 + c cos2 ϕ0 + b sin 2ϕ0 , 2 ωy (u sin ϕ0 + v cos ϕ0 ). ωx C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation (83) (84) 270 C. Efthymiopoulos and Z. Sándor Formulae for the N-iterated remainder We first define convenient norms for the remainder functions RJ and R φ of the mapping (47) given by equations (48) and (49), respectively. The norm of the function R (rJ ) at the value of action J is defined by (r ) RJ = J (r ) s/2 R J ,sk J , (85) sr +2, |k|s with a similar definition for the norm ||R (rφ ) || J . Both norms are real analytic functions of J in the disc J < J 0 , where J 0 is the minimum of the radii of absolute convergence of the series R (rJ ) and R (rφ ) . Furthermore, for any J 1 and J 2 in the same disc, we have R (rJ ) J1 R (rJ ) J2 if and only if J 1 J 2 . Similarly for the norm of R (rφ ) . Let us consider now a fixed value of the action J ∗ , and a second value J = J∗ − N R (rJ ) J∗ where N is a fixed number of iterations. We assume that J ∗ is small enough that J∗ − 2N R (rJ ) J∗ 0. Finally, we consider initial conditions (J (0) , φ (0) ) on the circle J (0) = J and call (J (m) , φ (m) ), m = 1, . . . , N , the iterates of the mapping (47) with these initial conditions. Defining now the quantity J (m) = J ∗ − J (m) , and taking into account the above inequalities on the norms, yields |J (m) | 2N R (rJ ) J , (86) ∗ meaning that all the iterates (J (m) , φ (m) ), m = 1, . . . , N , belong to an annulus around the central circle J =J (0) with half-width bounded from above by the value of R (rJ ) J∗ . Furthermore, the angular part of the mapping (47) can be written as φ (m+1) = φ (m) + ω(r ) J (m) + Rφ(r ) J (m) , φ (m) . (87) However, in view of the mean value theorem for real analytic functions, there is a positive real number ξ (m) in the interval J ∗ − J (m) ξ (m) J ∗ such that dω(ξ (m) ) J (m) . dJ ω(r ) J (m) = ω(r ) (J∗ ) + Thus we get dω(ξ (m) ) J (m) + Rφ(r ) J (m) , φ (m) . dJ Applying the above equation N times, for m = 0, 1, . . . , N − 1, and adding all the equations yields φ (m+1) = φ (m) + ω(r ) (J∗ ) + φ (N ) = φ + N ω(r ) (J∗ ) + φ (N ) , where the quantity φ (N ) dω(ξ (m) ) is defined as N −1 φ (N ) = dJ m=0 (88) J (m) + N −1 Rφ(r ) J (m) , φ (m) , (89) m=0 where φ ≡ φ (0) . The following inequality then holds for the norms: (N ) φ 2N 2 R (rJ ) + N Rφ(r ) . J∗ J∗ (90) Writing the mapping of the actions as in (47), i.e. J m = 0, 1, . . . , N − 1, yields J (N ) = J + N −1 (m+1) =J (m) + R (rJ ) (J (m) ,φ (m) ), and adding the first N equations of this mapping for R (rJ ) (J (m) , φ (m) ). m=0 (m) However, implementing again the mean value theorem for real analytic functions, there are positive numbers s (m) s (m) J with J ∗ − J J (m) (m) (r ) (r ) (m) J ∗ and s φ with φ + mω (J ∗ ) s φ φ + mω (J ∗ ) + φ such that R (rJ ) J (m) , φ (m) = R (rJ ) J∗ , φ + mω(r ) (J∗ ) + ∂R (rJ ) (m) (m) (m) ∂R (rJ ) (m) (m) (m) s J , sφ J + s J , sφ φ . ∂J ∂φ Thus, the action mapping takes the form J (N ) − J = R (rJ ,N ) (J∗ , φ) + S (r ,N ) (J , φ; J∗ ), where the function S (r ,N ) (J , φ; J∗ ) = ) (J ∗ , R (r,N J φ) is the N-iterated remainder defined in equation (67), while the function S N −1 ∂R (r ) J m=0 ∂J (91) (m) s (m) J (m) + J , sφ ∂R (rJ ) ∂φ (r,N ) (J , φ;J ∗ ) is defined by (m) s (m) φ (m) , J , sφ (92) with all the quantities appearing in equation (92) being defined in the equations above it. Taking into account the bounds given by equations (86) and (90), it follows that the size of the variation of the action after N iterations is bounded by the inequality |J (N ) (r ) (r ) (r ) (r ,N ) ∂ω N 2 ∂R (rJ ) (r ) 3 ∂R J (r ) 2 ∂R J (r ) − J | RJ + N R sup + R + 2N RJ J , φ J J∗ J∗ J∗ ∗ ∂φ ∂J 2 ∂φ ∂J D J∗ J∗ J∗ (93) J∗ where D J∗ is the domain defined by J∗ − 2N R (rJ ) J∗ J J∗ . C C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation Nekhoroshev stability estimates for Trojan asteroids 271 The analytic calculation of the domain of Nekhoroshev stability with the iterated remainder criterion is based on the following algorithm: (1) For given order of truncation r, we repeat the steps 1–3 of the algorithm of Section 3.4, with the one-turn remainder R (rJ ) replaced by ) the iterated remainder R (r,N (J ∗ , φ), and J ∗ set equal to J ∗ = ρ 2∗ /2. The radius ρ 0 is then corrected to a new value J ρ0 = ρ02 − 2 S (rJ ,N ) J , ∗ where (r ) (r ) (r ) (r ) 2 (r ,N ) S J = N 3 ∂R J R (rJ ) sup ∂ω + N ∂R J Rφ(r ) + 2N 2 ∂R J R (rJ ) , J∗ J∗ J∗ J∗ ∂φ ∂J 2 ∂φ ∂J D J∗ J∗ J∗ J∗ in view of the inequality (93) (2) For fixed r, the procedure is repeated for many values of N, until the value yielding the maximum ρ 0 is identified. (3) Steps 1 and 2 are repeated for different orders of truncation r, until the optimal order, corresponding to the maximum value of ρ 0 , is found. This paper has been typeset from a TEX/LATEX file prepared by the author. C C 2005 RAS, MNRAS 364, 253–271 2005 The Authors. Journal compilation
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