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A Simple Theory on the Dynamical Effects of a Stratified Fluid Core upon Nutational Motion of the Earth
[chapter]

1980
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Nutation and the Earth's Rotation
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The theory of Molodensky (1961) on dynamical effects of a stratified fluid outer core upon nutations and diurnal Earth tides is recon structed on a new and probably much simpler ground. A theory equiva lent to Molodensky's is well represented on the basis of two linear equations for angular-momentum balance of the whole Earth and the fluid outer core, which differ from the well-known equations of Poincare (1910) only in the existence of products of inertia due to deformations of the whole Earth

doi:10.1007/978-94-010-9568-6_27
fatcat:dt6y27us5fgrjfd6eev2f2vanq