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dc.contributor.authorReisinger, N.
dc.contributor.authorBacchini, F.
dc.date2026
dc.date.accessioned2026-02-17T12:34:17Z
dc.date.available2026-02-17T12:34:17Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/14597
dc.descriptionContext. Magnetic reconnection is an explosive process that accelerates particles to high energies in Earth’s magnetosphere, offering a unique natural laboratory to study this phenomenon. Aims. This study investigates how well data-driven fully kinetic simulations can reproduce the ion and electron energy distributions observed during a reconnection event by the Magnetospheric Multiscale (MMS) mission. Methods. We performed fully kinetic 2D simulations initialized with plasma parameters derived from the MMS event and compared the resulting ion and electron energy distributions with observations. Key numerical and physical parameters were systematically varied to assess their influence on the resulting particle spectra. Results. The simulations capture the overall shape and evolution of nonthermal energy distributions for both species, but generally underestimate the very high-energy tail of the electron spectrum. Variations in numerical parameters have negligible effects on the resulting spectra, while the initial upstream temperatures instead play a more pronounced role in reproducing the observed distributions. Conclusions. We present a novel analysis of data-driven fully kinetic simulations of MR, showing that key aspects of particle acceleration can be captured, while also highlighting the limitations of 2D simulations and the need for more realistic (e.g., 3D) setups to reproduce the observed particle energization accurately.
dc.languageeng
dc.titleComparing simulated and observed particle energy distributions through magnetic reconnection in Earth’s magnetotail
dc.typeArticle
dc.subject.frascatiPhysical sciences
dc.audienceScientific
dc.subject.freeacceleration of particles
dc.subject.freemagnetic reconnection
dc.subject.freemethods: numerical
dc.source.titleAstronomy & Astrophysics
dc.source.volume706
dc.source.pageL18
Orfeo.peerreviewedYes
dc.identifier.doi10.1051/0004-6361/202558575
dc.identifier.url


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