On the Arnold Diffusion Mechanism in Medium Earth Orbit

dc.contributor.author
Alessi, E. M.
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Baldomá, I.
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Giralt, M.
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Guardia, M.
dc.date.accessioned
2025-01-23T13:57:49Z
dc.date.available
2025-01-23T13:57:49Z
dc.date.issued
2024-11-05
dc.identifier.uri
http://hdl.handle.net/2072/480076
dc.description.abstract
Space 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, Poincar & eacute;-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.
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dc.description.sponsorship
E.M. Alessi acknowledges support received by the project entitled coorbital motion and three-body regimes in the solar system, funded by Fondazione Cariplo through the program Promozione dell'attrattivita e competitivita dei ricercatori su strumenti dell'European Research Council-Sottomisura rafforzamento. I. Baldoma has been supported by the Grant PID-2021- 122954NB-100 funded by the Spanish State Research Agency through the programs MCIN/AEI/10.13039/501100011033 and ERDF A way of making Europe. M. Giralt has been supported by the European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie Grant Agreement No 101034255. M. Giralt has also been supported by the research project PRIN 2020XB3EFL Hamiltonian and dispersive PDEs. M. Guardia has been supported by the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation programme (Grant Agreement No. 757802). M. Guardia is also supported by the Catalan Institution for Research and Advanced Studies via ICREA Academia Prizes 2019 and 2023. This work is also supported by the Spanish State Research Agency, through the Severo Ochoa and Maria de Maeztu Program for Centers and Units of Excellence in R&D (CEX2020-001084-M).
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dc.format.extent
55 p.
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dc.language.iso
eng
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dc.publisher
Springer
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dc.relation.ispartof
Journal of Nonlinear Science
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dc.rights
Attribution 4.0 International
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dc.rights.uri
http://creativecommons.org/licenses/by/4.0/
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dc.subject.other
Space debris mitigation
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dc.subject.other
Arnold diffusion
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MEO
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dc.subject.other
Third-body perturbation
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dc.title
On the Arnold Diffusion Mechanism in Medium Earth Orbit
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dc.type
info:eu-repo/semantics/article
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dc.subject.udc
51
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dc.subject.udc
52
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dc.subject.udc
53
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dc.description.version
info:eu-repo/semantics/acceptedVersion
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dc.embargo.terms
cap
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dc.identifier.doi
10.1007/s00332-024-10080-0
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dc.rights.accessLevel
info:eu-repo/semantics/openAccess


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