On the Arnold Diffusion Mechanism in Medium Earth Orbit

dc.contributor.authorAlessi, Elisa Maria
dc.contributor.authorBaldomá Barraca, Inmaculada
dc.contributor.authorGiralt Miron, Mar
dc.contributor.authorGuàrdia Munárriz, Marcel
dc.date.accessioned2026-01-29T13:52:56Z
dc.date.available2026-01-29T13:52:56Z
dc.date.issued2024-11-05
dc.date.updated2026-01-29T13:52:56Z
dc.description.abstractSpace debris mitigation guidelines represent the most effective method to preserve the circumterrestrial environment. Among them, end-of-life disposal solutions play a key role. In this regard, effective strategies should be conceived not only on the basis of novel technologies, but also following an advanced theoretical understanding. A growing effort is devoted to exploit natural perturbations to lead the satellites toward an atmospheric reentry, reducing the disposal cost, also if departing from high-altitude regions. In the case of the Medium Earth Orbit region, home of the navigation satellites (like GPS and Galileo), the main driver is the gravitational perturbation due to the Moon, that can increase the eccentricity in the long term. In this way, the pericenter altitude can get into the atmospheric drag domain and the satellite can eventually reenter. In this work, we show how an Arnold diffusion mechanism can trigger the eccentricity growth. Focusing on the case of Galileo, we consider a hierarchy of Hamiltonian models, assuming that the main perturbations on the motion of the spacecraft are the oblateness of the Earth and the gravitational attraction of the Moon. First, the Moon is assumed to lay on the ecliptic plane and periodic orbits and associated stable and unstable invariant manifolds are computed for various energy levels, in the neighborhood of a given resonance. Along each invariant manifold, the eccentricity increases naturally, achieving its maximum at the first intersection between them. This growth is, however, not sufficient to achieve reentry. By moving to a more realistic model, where the inclination of the Moon is taken into account, the problem becomes non-autonomous and the satellite is able to move along different energy levels. Under the ansatz of transversality of the stable and unstable manifolds in the autonomous case, checked numerically, Poincaré–Melnikov techniques are applied to show how the Arnold diffusion can be attained, by constructing a sequence of homoclinic orbits that connect invariant tori at different energy levels on the normally hyperbolic invariant manifold.
dc.format.extent55 p.
dc.format.mimetypeapplication/pdf
dc.identifier.idgrec764270
dc.identifier.issn0938-8974
dc.identifier.urihttps://hdl.handle.net/2445/226407
dc.language.isoeng
dc.publisherSpringer Verlag
dc.relation.isformatofVersió postprint del document publicat a: https://doi.org/10.1007/s00332-024-10080-0
dc.relation.ispartofJournal of Nonlinear Science, 2024, vol. 35
dc.relation.urihttps://doi.org/10.1007/s00332-024-10080-0
dc.rights(c) Elisa Maria Alessi et al., 2024
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess
dc.subject.classificationSistemes dinàmics diferenciables
dc.subject.classificationSistemes hamiltonians
dc.subject.classificationProblema dels tres cossos
dc.subject.classificationMecànica celeste
dc.subject.otherDifferentiable dynamical systems
dc.subject.otherHamiltonian systems
dc.subject.otherThree-body problem
dc.subject.otherCelestial mechanics
dc.titleOn the Arnold Diffusion Mechanism in Medium Earth Orbit
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/acceptedVersion

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