A Primordial Origin of the Laplace Relation Among the Galilean Satellites
arXiv:astro-ph/0210589 · doi:10.1126/science.1076557
Abstract
Understanding the origin of the orbital resonances of the Galilean satellites of Jupiter will constrain the longevity of the extensive volcanism on Io, may explain a liquid ocean on Europa, and may guide studies of the dissipative properties of stars and Jupiter-like planets. The differential migration of the newly formed Galilean satellites due to interactions with a circumjovian disk can lead to the primordial formation of the Laplace relation n_1 - 3 n_2 + 2 n_3 = 0, where the n_i are the mean orbital angular velocities of Io, Europa, and Ganymede, respectively. This contrasts with the formation of the resonances by differential expansion of the orbits from tidal torques from Jupiter.
13 pages, including 4 figures; uses scicite.sty
References in corpus (1)
Cited by in corpus (39)
- Tidal Evolution of Close-in Extra-Solar Planets
- A seven-planet resonant chain in TRAPPIST-1
- On the tidal evolution of Hot Jupiters on inclined orbits
- Tidally Heated Terrestrial Exoplanets: Viscoelastic Response Models
- Calibration of Equilibrium Tide Theory for Extrasolar Planet Systems
- Origin of the Different Architectures of the Jovian and Saturnian Satellite Systems
- Calibration of Equilibrium Tide Theory for Extrasolar Planet Systems II
- N-body Simulations of Satellite Formation around Giant Planets: Origin of Orbital Configuration of the Galilean Moons
- Increased Tidal Dissipation Using Advanced Rheological Models: Implications for Io and Tidally Active Exoplanets
- Formation of Giant Planet Satellites
- Effects of Type I Migration on Terrestrial Planet Formation
- The Effect of an Early Planetesimal-Driven Migration of the Giant Planets on Terrestrial Planet Formation
- One of the closest exoplanet pairs to the 3:2 Mean Motion Resonance: K2-19b \& c
- Magnetic Coupling in the Disks Around Young Gas Giant Planets
- Planetary and satellite three body mean motion resonances
- Powering the Galilean Satellites with Moon-Moon Tides
- Isotopic evidence of long-lived volcanism on Io
- Three Pathways for Observed Resonant Chains
- The Formation and Dynamics of Super-Earth Planets
- Building the Galilean moons system via pebble accretion and migration: A primordial resonant chain
- Super-Earths: A New Class of Planetary Bodies
- Long-term evolution of the Galilean satellites: the capture of Callisto into resonance
- Early stages of Galilean moon formation in a water-depleted environment
- Growth and evolution of satellites in a Jovian massive disc
- Solar System Moons as Analogs for Compact Exoplanetary Systems
- Origin of Europa and the Galilean Satellites
- Dynamical history of the Galilean satellites for a fast migration of Callisto
- The Lense-Thirring effect in the Jovian system of the Galilean satellites and its measurability
- Tidally Heated Exomoons around Eridani b: Observability and prospects for characterization
- Photoevaporation of the Jovian circumplanetary disk I. Explaining the orbit of Callisto and the lack of outer regular satellites
- On the Origin of the Pluto System
- Enrichment of the HR 8799 planets by minor bodies and dust
- Circumplanetary disk ices II. Composition
- The Dynamical Viability of an Extended Jupiter Ring System
- Callisto's Nonresonant Orbit as an Outcome of Circum-Jovian Disk Substructure
- Not Just Gas: How Solid-Driven Torques Shaped the Migration of the Galilean Moons
- Formation of Water-rich Giant Planet Satellites at Decretion Disk Ice Lines
- The recent crossing of the 7:3 resonance between Ganymede and Callisto
- Satellites and small bodies with ALMA: Insights into Solar System formation & evolution