The formation of the Galilean moons and Titan in the Grand Tack scenario
Ren\'e Heller, Gabriel-Dominique Marleau, and Ralph Egon Pudritz

TL;DR
This paper investigates the formation of the Galilean moons and Titan within the Grand Tack scenario, analyzing their compositions, atmospheres, and formation timing relative to Jupiter and Saturn's migration.
Contribution
It provides a detailed thermal and dynamical model of moon formation in the Grand Tack scenario, highlighting the timing and environmental conditions affecting moon compositions and atmospheres.
Findings
Galilean moons likely formed beyond 4.5 AU before the Grand Tack.
Galilean atmospheres were probably eroded by solar radiation during the GT.
Titan formed after Saturn's own migration, at about 7 AU.
Abstract
In the Grand Tack (GT) scenario for the young solar system, Jupiter formed beyond 3.5 AU from the Sun and migrated as close as 1.5 AU until it encountered an orbital resonance with Saturn. Both planets then supposedly migrated outward for several yr, with Jupiter ending up at ~5 AU. The initial conditions of the GT and the timing between Jupiter's migration and the formation of the Galilean satellites remain unexplored. We study the formation of Ganymede and Callisto, both of which consist of ~50% HO and rock, in the GT scenario. We examine why they lack dense atmospheres, while Titan is surrounded by a thick N envelope. We model an axially symmetric circumplanetary disk (CPD) in hydrostatic equilibrium around Jupiter. The CPD is warmed by viscous heating, Jupiter's luminosity, accretional heating, and the Sun. The position of the HO ice line in the CPD, which is…
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