A mathematical description of Chandler's component of the coordinates
of the Earth's pole obtained from numerical experiments is compared to
the existing analytic solutions. An idealized model of coupled oscill
ations in the Earth-Moon system is considered. The solution to the pro
blem of eigenfrequencies is obtained as a partial solution to the equa
tions for coupled oscillators. Two known periods - draconic year (P-1
= 346.62 days) and the period P-2 = 433.6 +/- 5 days - are obtained as
the eigenfrequencies of this system. As a period of the Earth's prope
r oscillations we chose the magnitude of the pole's free motion obtain
ed experimentally and close to that given in the Ware model (P = 403.4
+/- 5 days).