Global 3-D Radiation Magnetohydrodynamic Simulations for FU Ori's Accretion Disk and Observational Signatures of Magnetic Fields
Zhaohuan Zhu, Yan-Fei Jiang, James M. Stone

TL;DR
This study uses global 3D radiation MHD simulations to explore magnetic fields and wind launching mechanisms in FU Ori's accretion disk, aligning with observations and revealing new insights into disk structure and magnetic field configurations.
Contribution
It provides the first comprehensive global 3D radiation MHD simulations of FU Ori's inner disk, demonstrating the impact of magnetic fields on accretion and wind launching, and comparing results with observational data.
Findings
Magnetically dominated atmosphere facilitates surface accretion.
Moderate disk wind with observed-like properties is launched in vertical magnetic fields.
Magnetic field structures vary between wind launching and accreting regions.
Abstract
FU Ori is the prototype of FU Orionis systems which are outbursting protoplanetary disks. Magnetic fields in FU Ori's accretion disks have previously been detected using spectropolarimetry observations for Zeeman effects. We carry out global radiation ideal MHD simulations to study FU Ori's inner accretion disk. We find that (1) when the disk is threaded by vertical magnetic fields, most accretion occurs in the magnetically dominated atmosphere at zR, similar to the "surface accretion" mechanism in previous locally-isothermal MHD simulations. (2) A moderate disk wind is launched in the vertical field simulations with a terminal speed of 300-500 km/s and a mass loss rate of 1-10\% the disk accretion rate, which is consistent with observations. Disk wind fails to be launched in simulations with net toroidal magnetic fields. (3) The disk photosphere at the unit optical depth…
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