On The Applicability of Ring-Moon Cycles to Exoplanets
Isabella E. Ward, Matija Ćuk
TL;DR
This work extends Solar System ring–moon cycle theory to exoplanets, evaluating two observationally testable pathways: non-despun Neptune-like planets and despun planets in secular spin–orbit resonances. By computing Roche limits $a_{RRL}$ and $a_{FRL}$, the synchronous orbit $a_{synch}$, and Lindblad-torque limits $a_{Lind}$, the authors classify planetary regimes and estimate ring lifetimes and equivalent thickness $d$, linking these to transit observability. The study finds that ring–moon cycles can yield long-lived, optically thick rings around some exoplanets, particularly non-despun Neptune-like planets, and that despun resonant planets can also host rings detectable in transit through cross-section enhancements, with a measurable impact on apparent radii for some systems. The results suggest exoring detections could inform obliquity histories, interior structure, and exomoon formation pathways, while highlighting degeneracies with limb darkening and atmosphere that require careful transit modeling and system comparisons.
Abstract
The presence of rings and moons around exoplanets is likely to be one of the next great discoveries in exoplanet research. Using theories developed for the Solar System, we explore the possibility of coupled ring-moon cycles around exoplanets and what these processes mean for the observability of these features. Around Neptune- and Earth-like planets, we find that ring-moon cycles are capable of producing long-lived rings of comparable and greater relative transit depths than Saturn's. In multi-planet systems, secular spin-orbit resonances can provide the necessary planetary obliquity for these rings to contribute noticeably to transit lightcurves. We model the geometry of a ring's cross-section at various angles in comparison to the cross-section of a transiting planet to determine whether the ring may be detectable during the planet's transit. Ringed planets have also been proposed as an alternative to inflated planetary radii seen in transit, leading to abnormally low observed densities. Ring-moon cycles can produce late-forming and sometimes long-lived rings that can have the potential of explaining at least some of these observations. We also discuss some inconsistencies in the calculation of exoplanet oblateness due to rotation that we have come across in the course of this work.
