Published December 20, 2025 | Version Published
Journal Article Open

Callisto's Nonresonant Orbit as an Outcome of Circum-Jovian Disk Substructure

  • 1. ROR icon California Institute of Technology

Abstract

The Galilean moons of Io, Europa, and Ganymede exhibit a 4:2:1 commensurability in their mean motions, a configuration known as the Laplace resonance. The prevailing view for the origin of this three-body resonance involves the convergent migration of the moons, resulting from gas-driven torques in the circum-Jovian disk wherein they accreted. To account for Callisto's exclusion from the resonant chain, a late and/or slow accretion of the fourth and outermost Galilean moon is typically invoked, stalling its migration. Here, we consider an alternative scenario in which Callisto's nonresonant orbit is a consequence of disk substructure . Using a suite of N -body simulations that self-consistently account for satellite-disk interactions, we show that a pressure bump can function as a migration trap, isolating Callisto and alleviating constraints on its timing of accretion. Our simulations position the bump interior to the birthplaces of all four moons. In exploring the impact of bump structure on simulation outcomes, we find that it cannot be too sharp nor flat to yield the observed orbital architecture. In particular, a "Goldilocks" zone is mapped in parameter space, corresponding to a well-defined range in bump aspect ratio. Within this range, Io, Europa, and Ganymede are sequentially trapped at the bump, and ushered across it through resonant lockstep migration with their neighboring, exterior moon. The implications of our work are discussed in the context of uncertainties regarding Callisto's interior structure, arising from the possibility of non-hydrostatic contributions to its shape and gravity field, unresolved by the Galileo spacecraft.

Copyright and License

© 2025. The Author(s). Published by the American Astronomical Society. Original content from this work may be used under the terms of the Creative Commons Attribution 4.0 licence. Any further distribution of this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI.

Acknowledgement

This work was supported by a Caltech Center for Comparative Planetary Evolution (3CPE) grant to the authors, and the David & Lucile Packard Fellowship to K.B.. We thank Dave Stevenson for insightful discussions on Callisto’s interior structure and caveats associated with determining icy satellite moments of inertia.

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Additional details

Funding

California Institute of Technology
Center for Comparative Planetary Evolution (3CPE) -
David and Lucile Packard Foundation

Dates

Submitted
2025-04-08
Accepted
2025-10-19
Available
2025-12-18
Published

Caltech Custom Metadata

Caltech groups
Caltech Center for Comparative Planetary Evolution, Division of Geological and Planetary Sciences (GPS)
Publication Status
Published