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  • The models [Petit and Luzum, 2010] include effects for tidal displacements of the solid (body) Earth (the largest single effect), ocean loading, atmospheric pressure loading (S1, S2, and higher harmonics of the solar day), as well as tidal variations in the geopotential due to the solid Earth, ocean, and atmosphere, and the corresponding oscillations in the Earth's rotations, mostly owing to the o
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