“…Where, the dynamic accelerationã consists of the following ones: [1] two-body gravitational attractions of Earthã TB , [2] N-body gravitational attractions of the Sun, Moon and so onã NB , [3] relativistic perturbationã RL , [4] gravitational attractions of the non-spherical Earthã NS (Earth gravity model JGM3 (Tapley et al, 1996;Xu, 2007;Xu and Xu, 2013), truncated to the 10th degree and order), [5] gravitational attractions of solid-Earth tides , oceanic tides and atmospheric tides a TD (Li, 1995;Wahr, 1981;Xu, 2007;Xu and Xu, 2013;McCarthy and Petit, 2004), [6] perturbation of Earth's rotational deformationã ED (Buffett et al, 1993), [7] radiation pressure of the Sunã SR (Tapley et al, 2004;Parkinson et al, 1960;Xu, 2007;Xu and Xu, 2013;McCarthy and Petit, 2004), [8] Earth albedo radiation pressureã ER (Sehnal, 1980;Borderies and Longaretti, 1990), [9] empirical radial-transverse-normal accelerations a TR (Huang et al, 2011;Eanes and Bettaadpur, 1996) and…”