Application of a Steady-State Accretion Disk Model to Spectrophotometry and High-Resolution Spectra of Two Recent FU Ori Outbursts
Antonio C. Rodriguez, Lynne A. Hillenbrand

TL;DR
This study applies a steady-state accretion disk model to spectrophotometric data of two FU Ori outbursts, estimating accretion rates and disk temperatures, and explores model variations and parameter degeneracies.
Contribution
It introduces a detailed modeling approach for FU Ori objects using MCMC to estimate accretion rates and disk properties, including boundary region effects.
Findings
HBC 722 has an accretion rate of approximately 10^{-4.9} M_sun/yr.
Gaia 17bpi has a lower accretion rate of about 10^{-6.7} M_sun/yr.
HBC 722's accretion rate aligns with typical FU Ori objects, while Gaia 17bpi's is lower.
Abstract
We apply a conventional accretion disk model to the FU Ori-type objects HBC 722 and Gaia 17bpi. Our base model is a steady-state, thin Keplerian disk featuring a modified Shakura-Sunyaev temperature profile, with each annulus radiating as an area-weighted spectrum given by a NextGen atmosphere at the appropriate temperature. We explore departures from the standard model by altering the temperature distribution in the innermost region of the disk to account for "boundary region"-like effects. We consider the overall spectral energy distribution (SED) as well as medium- and high-resolution spectra in evaluating best-fit models to the data. Parameter degeneracies are studied via a Markov Chain Monte Carlo (MCMC) parameter estimation technique. Allowing all parameters to vary, we find accretion rates for HBC 722 of $\dot{M} = 10^{-4.90} M_\odot \textrm{ yr}^{-1}\; {}^{+0.99}_{-0.40}…
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