Abstract

We analytically compute the long-term orbital variations of a test particle orbiting a central body acted upon by an incident monochromatic plane gravitational wave. We assume that the characteristic size of the perturbed two-body system is much smaller than the wavelength of the wave. Moreover, we also suppose that the wave's frequency νg is much smaller than the particle's orbital one nb. We make neither a priori assumptions about the direction of the wavevector k nor on the orbital configuration of the particle. While the semi-major axis a is left unaffected, the eccentricity e, the inclination I, the longitude of the ascending node Ω, the longitude of pericenter ϖ and the mean anomaly ℳ undergo non-vanishing long-term changes of the form dΨ/dt=F(Kij;e,I,Ω,ω),Ψ=e,I,Ω,ϖ,M, where Kij, i,j=1,2,3 are the coefficients of the tidal matrix K. Thus, in addition to the variations of its orientation in space, the shape of the orbit would be altered as well. Strictly speaking, such effects are not secular trends because of the slow modulation introduced by K and by the orbital elements themselves: they exhibit peculiar long-term temporal patterns which would be potentially of help for their detection in multidecadal analyses of extended data records of planetary observations of various kinds. In particular, they could be useful in performing independent tests of the inflation-driven ultra-low gravitational waves whose imprint may have been indirectly detected in the Cosmic Microwave Background by the Earth-based experiment BICEP2. Our calculation holds, in general, for any gravitationally bound two-body system whose orbital frequency nb is much larger than the frequency νg of the external wave, like, e.g., extrasolar planets and the stars orbiting the Galactic black hole. It is also valid for a generic perturbation of tidal type with constant coefficients over timescales of the order of the orbital period of the perturbed particle.

Highlights

  • Gravitational waves [1, 2] are a key theoretical prediction of the general theory of relativity (GTR)

  • In addition to the variations of its orientation in space, the shape of the orbit would be altered as well. Speaking, such effects are not secular trends because of the slow modulation introduced by K and by the orbital elements themselves: they exhibit peculiar long-term temporal patterns which would be potentially of help for their detection in multidecadal analyses of extended data records of planetary observations of various kinds. They could be useful in performing independent tests of the inflation-driven ultra-low gravitational waves whose imprint may have been indirectly detected in the Cosmic Microwave Background by the Earthbased experiment BICEP2

  • Since GTR relies upon the Lorentz invariance, which carries with it the concept of a limiting speed for physical interactions, the existence of gravitational waves is a natural consequence of it

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Summary

INTRODUCTION

Gravitational waves [1, 2] are a key theoretical prediction of the general theory of relativity (GTR). Iorio: Orbital effects of a monochromatic plane gravitational wave on a gravitationally bound two-body system technically valid for waves with higher frequencies with respect to the solar system ones; they might be as high as about 106 Hz corresponding to the green-light blue part of the spectrum in Figure 1 of Prince et al [12] Another scenario to which our analysis can be applied is the stellar system orbiting the supermassive black hole (SBH) hosted by the galactic center (GC) in Sgr A* [75], where the orbital periods of the stars discovered so far are larger than 16 years corresponding to frequencies smaller than 2 Â 109 Hz. On the other hand, our results are not necessarily limited to the very-low frequency waves case, being valid for any tidal force with constant (over particle’s characteristic timescales) matrix coefficients as well, independently of its physical origin. We will consider the particular case of eq (16) (kb 1⁄4 f0; 0; Æ1g), widely treated in literature

THE LONG-TERM VARIATIONS OF THE KEPLERIAN ORBITAL ELEMENTS
Monochromatic plane gravitational wave propagating along a generic direction
Monochromatic plane gravitational wave propagating along the z axis
A comment on the approximation used for the harmonic wave functions
CONFRONTATION WITH OTHER APPROACHES IN LITERATURE
SUMMARY AND CONCLUSIONS
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