2 t S m and the estimation of their mean values together with periodic constituents on given time-period. Stability of the positions of the equatorial inertia axes (A , B) and the angle between two quadrupole axes located in the plane of the axes A and C of inertia is found. The estimated longitude A of the principal axis A as the parameter of the Earth's triaxiality in the precession-nutation theory and 2 J precession rate A p of the precession constant are recommended for the Earth's rotation theory. Additionally to some permanent constituents periodic components at seasonal and shorter time scale were evaluated.
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