Abstract
The dynamic analysis of the Earth pole oscillatory motion is used to study the gravitational-tidal mechanism of formation of the annual component of the process. The results of an analysis of the interaction between the fine resonance structure of the long-period perturbation and the diurnal and semidiurnal tides are used to derive equations for the amplitude and phase of the oscillatory process of six-year pole wobble.
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GFZ Potsdam, Department 1, The GRACE Mission. URL: http://op.gfz-potsdam.de/grace.
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Original Russian Text © V.V. Perepelkin, 2013, published in Izvestiya Akademii Nauk. Mekhanika Tverdogo Tela, 2013, No. 6, pp. 15–18.
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Perepelkin, V.V. Amplitude-frequency analysis of the earth polar oscillation process. Mech. Solids 48, 613–615 (2013). https://doi.org/10.3103/S0025654413060022
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DOI: https://doi.org/10.3103/S0025654413060022