2003/10/07 by Ken Rice, W. K. M. Rice, Philip J. Armitage · 4 citations
Physics and Astronomy · #Accretion (finance) #Astro and Planetary Science #Astrobiology #Astronomy #Astrophysics #Astrophysics and Star Formation Studies #Exoplanet #Formation and evolution of the Solar System #Gas giant #Giant planet #Jupiter (rocket family) #Jupiter mass #Physics #Planet #Planetary mass #Planetary migration #Planetary system #Planetesimal #Protoplanet #Protoplanetary disk #Solar System #Stellar, planetary, and galactic studies #astro-ph
paper · pdf · doi:10.1086/380390
published as Astrophys.J. 598 (2003) L55 · ApJL, in press
arxiv created 2003/10/07 · openalex publication_date 2003/10/31 · arxiv updated 2009/12/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/08/05
Numerical simulations show that the migration of growing planetary cores may be dominated by turbulent fluctuations in the protoplanetary disk, rather than by any mean property of the flow. We quantify the impact of this stochastic core migration on the formation timescale and core mass of giant planets at the onset of runaway gas accretion. For standard solar nebula conditions, the formation of Jupiter can be accelerated by almost an order of magnitude if the growing core executes a random walk with an amplitude of a few tenths of an AU. A modestly reduced surface density of planetesimals allows Jupiter to form within 10 Myr, with an initial core mass below 10 M ⊕ , in better agreement with observational constraints. For extrasolar planetary systems, the results suggest that core accretion could form massive planets in disks with lower metallicities, and shorter lifetimes, than the solar nebula.