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The Lunar Theory ELP Revisited. Introduction of New Planetary Perturbations

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The Lunar Theory ELP Revisited. Introduction of New Planetary Perturbations A&A 404, 735–742 (2003) Astronomy DOI: 10.1051/0004-6361:20030529 & c ESO 2003 Astrophysics The lunar theory ELP revisited. Introduction of new planetary perturbations J. Chapront and G. Francou Observatoire de Paris, SYRTE, UMR 8630/CNRS, 61 avenue de l’Observatoire, 75014 Paris, France Received 19 September 2002 / Accepted 21 March 2003 Abstract. On the basis of the semi-analytical theory ELP, a new solution has been built that makes use of the planetary pertur- bations MPP01 constructed by P. Bidart. This new solution, called ELP/MPP02, is an analytical solution that contains all the perturbations to represent the lunar motion. The level of truncation for the series is the centimeter. This limit induces analytical developments of a reasonable dimension. ELP/MPP02 is compared to the JPL ephemerides DE405 and DE406. After fitting the constants and the reference frame to DE405, over a few centuries, numerical comparisons with DE405 show a significant improvement in precision, in particular for the radius vector. Over the long range of several millennia, comparisons with DE406 show an improvement in the long periodic perturbations due to planets. On the time interval of one century around J2000 we added to ELP/MPP02 numerical complements ρ405 based on the differ- ences with DE405 in such a way that ELP/MPP02+ρ405 has the precision of the numerical integration. Using this new ephemeris to analyse LLR data provided since 1970, we build the solution ELP/MPP02(LLR) fitted to LLR observations. Various approximations have been also tested on the residuals DE406 - ELP/MPP02. We first determined corrections to the secular variations of the mean longitude, longitudes of the node and perigee under a simple polynomial form; they reduce the differences between ELP/MPP02 and DE406 to less than 3 arcsec in longitude and latitude and 2 km in distance over the whole time interval of DE406 [ 3000; +3000]. Next, the differences themselves between the two solutions are approxi- mated over 2 millennia with Poisson− series in a pseudo analytical form similar to ELP/MPP02. We reduce the residuals to less than 0.03 arcsec in longitude and latitude and 30 m in distance. Key words. planets and satellites: general – celestial mechanics – ephemerides 1. Introduction second, an approximation of the differences between the 2 solutions themselves with Poisson series. This paper presents various aspects of improvements of the so- lution ELP. In the first part, we recall the main features of the 2. Improvements of the planetary perturbations solution ELP, emphasizing its major deficiency due to the com- putation of planetary perturbations. To improve the planetary in ELP developments we make use of a new solution named MPP01 2.1. The solution ELP by Bidart (2000). In the second part, after simplifications of the original developments of MPP01, fit of constants and tests of The construction of the complete lunar theory ELP goes back precision, we derive a new solution ELP/MPP02. Several pa- to 1980. Its first version was the semi-analytical solution rameters and the reference frame are fit to the JPL ephemeris ELP2000-82 (Chapront-Touz´e & Chapront 1983). This solu- DE405 (Standish 1998). The solution ELP/MPP02(405) is then tion includes: compared to DE405/DE406 over various time intervals. In par- - the solution of the Main Problem (Earth, Moon and Sun with ticular its validity over a long period of time is tested over the a Keplerian heliocentric orbit for the Earth-Moon barycen- whole time interval of DE406 [ 3000; +3000]. Then, the pa- ter) including partials with respect to various constants and rameters and frame are independently− fitted to LLR observa- parameters; tions leading to the final solution ELP/MPP02(LLR). In the - the Earth’s figure perturbations; third part, further numerical experiments have been tested to - the direct and indirect planetary perturbations that contain make ELP/MPP02 and DE406 approach over several millen- in particular the effects of the secular motions in eccentric- nia. Two approaches are examined: first, a fit of the secular ity and perihelion of the Earth-Moon barycenter EMB and variations of the lunar arguments to the numerical integration, the secular motion of the ecliptic; the planetary motions come from VSOP82 (Bretagnon 1982) ; Send offprint requests to: J. Chapront, - the relativistic effects; e-mail: [email protected] - the tidal perturbations; Article published by EDP Sciences and available at http://www.aanda.org or http://dx.doi.org/10.1051/0004-6361:20030529 736 J. Chapront and G. Francou: The lunar theory ELP revisited - the Moon’s figure perturbations and coupling with libration. like VSOP82. The reference plane of the theory is the mean This first version of ELP has not been fitted directly to ob- dynamical ecliptic at J2000. For recent determination of the servations but via the JPL lunar ephemeris DE200-LE200. quantities related to the reference frame, see Chapront et al. VSOP82 used the same source of comparisons and fits. (2002). The classical Delaunay’s arguments D, F, l and l0 are In order to increase the time domain of validity, a second used in the Main Problem series and perturbation series with: version has been developed: ELP2000-85 with a higher trun- D = w T + 180 ; F = w w ; l = w w ; l = T $ ; w , 1 − ◦ 1 − 3 1 − 2 0 − 0 1 cation level but introducing new expressions for the mean w2,andw3 are respectively the secular mean lunar longitude, lunar arguments (Chapront-Touz´e & Chapront 1988). With the mean longitude of the perigee and the mean longitude of respect to ELP2000-82 the main improvement consists of the node; T and $0 are respectively the mean longitude of EMB computing secular terms proportional to powers 3 and 4 and its perihelion. of the time. Correlatively a comparison with the JPL lunar The luni-solar parameters that are used for fitting the solu- ephemeris LE51 (Newhall et al. 1983) over a long range has tion to LLR observations and that are considered in Table 1 are been performed to estimate the accuracy of the secular terms. the following: Later, the new mean lunar arguments of ELP2000-85 were in- (0) (0) (0) w1 , w2 , w3 : the mean longitude and the mean longitudes of troduced in ELP2000-82, giving ELP2000-82B. perigee and node at J2000; Further improvements have been brought concerning ν: the sidereal mean motion of the Moon; mainly the lunar and terrestrial masses, the perturbations due Γ: an inclination coefficient of the dimension of the inclination to the Moon and Earth’s figures including more recent values of the Moon; of the gravitational parameters, the tidal perturbations with a E: an eccentricity coefficient of the dimension of the eccentric- new model separating diurnal and semi-diurnal tides on the ity of the Moon; Earth and taking into account the tides on the Moon. As a ba- (0) (0) T and $0 : the solar mean longitude, and the mean longi- sic JPL ephemeris for comparisons and fits of the constants tude of perihelion at J2000; we then used DE245. In parallel an improvement of the lunar n0: the sidereal mean motion of the Sun; librations by Moons (1982) has been done. Finally, a prelimi- e0: the solar eccentricity. nary fit of the improved ELP2000-82B to LLR observations has When comparing to observations we have to add 2 parameters been realized (Chapront & Chapront-Touz´e 1997). From now fixing the reference frame (R): on, the improved analytical solution ELP2000-82B is simply (R): the inclination of the inertial mean ecliptic on the equator called ELP. of (R); Our last version was ELP2000-96, obtained by adding nu- φ(R): the separation between the origin of the right ascension merical complements to ELP; a complete analysis of Lunar in (R) and the ascending node of the inertial mean ecliptic on Laser Ranging (LLR) observations from 1972 till 1998 has the equator of (R) for J2000. been performed using this solution and the completed Moons’ The half secular deceleration of the lunar mean longitude due to theory of the lunar libration (Chapront et al. 1999). (2) tidal forces is taken into account through w1 . Finally two bias ELP provides the polar coordinates σ (longitude V, lati- parameters in the perigee and node motions can be retained tude U and distance r) under the general formulation: (1) to compensate the deficiencies of the analytical solution: ∆w2 and ∆w(1). They are determined with a fit either to a close nu- σ = tn A(n) 3 X X i1;i2;:::;ip merical integration or to the observations themselves. n 0 i1;i2;:::;ip ≥ sin (i λ + i λ + ::: + i λ + φ(n) ): (1) 1 1 2 2 p p i1;i2;:::;ip × 2.2. The planetary perturbations in MPP01 In the case of V one has to add to the previous formula the secular mean longitude: MPP01 is a new solution for planetary perturbations in the or- bital motion of the Moon that has been elaborated by Bidart (0) (1) (2) 2 w1 = w1 + w1 t + w1 t + ::: (2000, 2001a). It has been constructed within the framework of the ELP solution and the perturbation method is inspired by A(n) are numerical coefficients, φ(n) are numerical i1;i2;:::;ip i1;i2;:::;ip Brown’s lunar theory whose basic concepts are discussed in phases and λ j are literal arguments standing for polynomial Chapront-Touz´e & Chapront (1980). We knew that in ELP the (k) k functions of the time: λ j = k 0 λ j t . In the case of the Main main limitation in precision resulted from the computation of P ≥ Problem, we have also at our disposal the derivatives of the co- the series for direct and indirect planetary perturbations.
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