Plasma and Magnetic-Field Variations at Asteroid-Belt Distances: A Ulysses Case Study

02 November 2026, Version 1
This content is an early or alternative research output and has not been peer-reviewed by Cambridge University Press at the time of posting.

Abstract

We investigate possible interactions between coronal mass ejections (CMEs), solar-wind plasma, and as teroids in the asteroid belt. We focus on variations in the magnetic-field magnitude, proton temperature, proton number density, and plasma and magnetic pressures. We examine whether interactions with potentially magnetized asteroids could contribute to localized plasma disturbances or magnetic reconnec tion. Our analysis combines magnetohydrodynamic (MHD)considerations with an archival case study us ing Ulysses measurements obtained on 2 March 1991 at a heliocentric distance of approximately 2.25 AU. Within the selected interval, the proton temperature increased by approximately 48%, while the magnetic field magnitude decreased by approximately 55%. Proton thermal pressure increased, whereas mag netic pressure decreased. These variations are qual itatively compatible with plasma processes involv ing magnetic-energy redistribution, but the available measurements are insufficient to identify magnetic re connection conclusively. Furthermore, the observa tions do not establish a causal connection between the measured variations and an asteroid encounter, and the interval has not been independently confirmed as a CME event. We therefore propose asteroid-related, potentially recurrent magnetic reconnection as a hy pothesis for future investigation rather than an es tablished mechanism. Further work should combine verified spacecraft-asteroid geometry, suitable control intervals, and plasma measurements capable of con straining magnetic topology and energy transfer.

Keywords

Solar wind
Magnetic reconnection
Asteroid belt
Ulysses spacecraft
Magnetohydrodynamics
Interplanetary magnetic field

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