1997
DOI: 10.1080/02681119708806247
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Dynamics of artificial satellite orbits with tesseral resonances including the effects of luni- solar perturbations

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Cited by 43 publications
(57 citation statements)
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“…Unless the satellite is in a state of orbital resonance, where the satellite's mean motion is commensurable with the rotational motion of the Earth, the longitude-dependent tesseral terms of the geopotential have, generally, very little effect on the orbit and can be ignored (or, averaged) when looking on timescales much longer than one orbital period. Under resonance conditions, however, the longitudinal forces from the tesseral harmonics induce long-term changes in the semimajor axis and mean motion, leading to a libration in longitude (Ely and Howell, 1997). Contrary to higher-order zonal harmonics that essentially decay at high altitudes, tesseral resonances may become important, as the orbital period approaches commensurability with the Earth's rotation.…”
Section: Dynamical Modelmentioning
confidence: 99%
“…Unless the satellite is in a state of orbital resonance, where the satellite's mean motion is commensurable with the rotational motion of the Earth, the longitude-dependent tesseral terms of the geopotential have, generally, very little effect on the orbit and can be ignored (or, averaged) when looking on timescales much longer than one orbital period. Under resonance conditions, however, the longitudinal forces from the tesseral harmonics induce long-term changes in the semimajor axis and mean motion, leading to a libration in longitude (Ely and Howell, 1997). Contrary to higher-order zonal harmonics that essentially decay at high altitudes, tesseral resonances may become important, as the orbital period approaches commensurability with the Earth's rotation.…”
Section: Dynamical Modelmentioning
confidence: 99%
“…In the present work, we perform the study of the effects of the gravitational resonances (also called tesseral resonances, see Gedeon (1969); Ely & Howell (1997)), within the LEO region. The precise definition of resonance is given as follows.…”
Section: The Geopotential Hamiltonianmentioning
confidence: 99%
“…This work extends the research performed in Celletti & Galeş (2014, 2015a, where analytical and numerical methods, mostly adopting Hamiltonian formalism, have been used to study the dynamics of objects within resonances located at large distances from the Earth (the so-called geostationary and GPS regions at distances, respectively, equal to 42 164 km and 26 560 km). We also mention Ely & Howell (1997); Formiga & Vilhena del Moraes (2011); ; for accurate modeling and analytical studies of space debris dynamics. With respect to Celletti & Galeş (2014, 2015a, the current work presents the novelty that, dealing with LEO, the model becomes more complicated, due to the effect of the geopotential, being the Earth very close, and moreover the dynamics is dissipative because of the air drag.…”
Section: Introductionmentioning
confidence: 99%
“…Often semi-analytical techniques are employed to obtain Poincaré or stroboscopic maps. For example, Ely and Howell (1997) apply averaging and Lie perturbation techniques to generate Poincaré plots for studying the stability of near-Earth orbits. Roth (1978Roth ( , 1979 uses semi-analytical techniques to stroboscopically map a perturbed orbit from pericenter to pericenter to achieve efficient propagation.…”
Section: Introductionmentioning
confidence: 99%