1995
DOI: 10.1111/j.1365-246x.1995.tb06839.x
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Forced nutations of a rigid mantle-liquid core earth model in canonical formulation

Abstract: S U M M A R YThe canonical formalism for the rotation of an earth model composed of a rigid mantle and a liquid core, established in Getino (1995b), starting from the model of Sevilla & Romero (1987), is applied here to the study of the forced nutations caused by the perturbing lunisolar potential. The main purpose of this paper is not to get accurate values for the nutation terms, since the earth model considered does not include the effect of the elasticity. This approach should be understood as a generaliza… Show more

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Cited by 29 publications
(50 citation statements)
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“…If we neglect the dissipation (Αχ = 0), the out-of-phase terms disappears, and we get similar expressions as those obtained in Getino (1995b) for the conservative case. Even more, if we particularize to the rigid case (A c = 0), then F a = 1, and we obtain the same expressions as in Kinoshita's theory.…”
Section: Forced Nutationssupporting
confidence: 66%
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“…If we neglect the dissipation (Αχ = 0), the out-of-phase terms disappears, and we get similar expressions as those obtained in Getino (1995b) for the conservative case. Even more, if we particularize to the rigid case (A c = 0), then F a = 1, and we obtain the same expressions as in Kinoshita's theory.…”
Section: Forced Nutationssupporting
confidence: 66%
“…The study of the Earth rotation is not an exception, and the theory of Kinoshita (1977) is the most complete and accurate among those for a rigid Earth model. Recently, the Hamiltonian approach has been followed by the authors in order to extend Kinoshita's theory to general models of deformable Earth through a series of papers, first considering an elastic mantle (Getino and Ferrândiz, 1995), then a liquid core (Getino, 1995a(Getino, , 1995b. We only point out here that the results obtained are completely analytical, and depend on parameters that are provided by the different Earth models available.…”
Section: Introductionmentioning
confidence: 99%
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“…(37) is of the second order in σ. Therefore, due to the smallness of variables σ, σ c ∼ 10 −6 rad (Nikitina 1990), neglecting this term we obtain the first order the relationship (Getino 1995b;Getino & Ferrándiz 1997) µ +ν = Ω .…”
Section: Unperturbed Solutionsmentioning
confidence: 99%