2015
DOI: 10.1134/s1063772915010096
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A celestial-mechanical model for the tidal evolution of the Earth-Moon system treated as a double planet

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Cited by 18 publications
(4 citation statements)
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“…There are several simplified tide models which are not explicitly parameterized by Love numbers (see, for instance Mignard (1979), Efroimsky and Williams (2009), Zlenko (2014), Celletti (1990), Antognini et al (2014), Bambusi and Haus (2015), Ferraz-Mello (2013), Correia et al (2014), Boué et al (2016), Wisdom and Meyer (2016), Ragazzo and Ruiz (2015), Ragazzo and Ruiz (2017)), two of them will be important in this paper: the first presented in Boué et al (2016) after previous work in Ferraz-Mello (2013) and Correia et al (2014), and the second presented in Ragazzo and Ruiz (2017) after previous work in Ragazzo and Ruiz (2015).…”
Section: Introductionmentioning
confidence: 99%
“…There are several simplified tide models which are not explicitly parameterized by Love numbers (see, for instance Mignard (1979), Efroimsky and Williams (2009), Zlenko (2014), Celletti (1990), Antognini et al (2014), Bambusi and Haus (2015), Ferraz-Mello (2013), Correia et al (2014), Boué et al (2016), Wisdom and Meyer (2016), Ragazzo and Ruiz (2015), Ragazzo and Ruiz (2017)), two of them will be important in this paper: the first presented in Boué et al (2016) after previous work in Ferraz-Mello (2013) and Correia et al (2014), and the second presented in Ragazzo and Ruiz (2017) after previous work in Ragazzo and Ruiz (2015).…”
Section: Introductionmentioning
confidence: 99%
“…This is more evident in the study of two-body systems, which we will pursue in a future work. Finally, due to its Lagrangian formulation our model can be used as a building block in the study of many-body systems without any further assumptions (compare to the study of a planar two body system in Zlenko (2015). (1 + λ) −2 − (1 + λ) −1 dλTr (B 2 ) = 8 15 γ Tr (B 2 ).…”
Section: Theorem 5 Suppose That the Zero Solution Of (55) Is Stable mentioning
confidence: 99%
“…The dynamics of satellites and space debris in external resonances focus on the 1:2, 1:3, and 2:3 resonances by the Hamiltonian approach. Zlenko (2015) [30] has determined a celestial-mechanical model for the tidal evolution of the Earth-Moon system of two viscoelastic spheres in the gravitational field using the Kelvin-Voigt model. Gallardo et al (2016) [10] have investigated three-body mean motion resonances for planetary and satellite by the semi-analytical method.…”
Section: Introductionmentioning
confidence: 99%