Migration of massive planets in accreting disks
Christoph D\"urmann, Wilhelm Kley

TL;DR
This study investigates the migration of massive planets in accreting disks, revealing that their migration rate is governed by disk torques and not the classical type II regime, with implications for planet formation models.
Contribution
It demonstrates that massive planet migration is independent of viscous inflow and that gap formation does not lead to classical type II migration, challenging existing theories.
Findings
Migration rate depends on disk torques, not viscous inflow.
Gap does not isolate inner and outer disk, allowing gas crossing.
Migration can be faster or slower than classical type II.
Abstract
Massive planets that open a gap in the accretion disk are believed to migrate with exactly the viscous speed of the disk, a regime termed type II migration. Population synthesis models indicate that standard type II migration is too rapid to be in agreement with the observations. We study the migration of massive planets between and corresponding to 0.2 to 2 Jupiter masses . in order to estimate the migration rate in comparison to type II migration. We follow the evolution of planets embedded in two-dimensional, locally isothermal disks with non-zero mass accretion which is explicitly modelled using suitable in- and outflow boundary conditions to ensure a specific accretion rate. After a certain relaxation time we release the planet and measure its migration through the disk and the dependence on parameters such as viscosity, accretion rate…
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