Late-time Evolution and Instabilities of Tidal Disruption Disks
Anthony L. Piro, Brenna Mockler

TL;DR
This paper models the long-term evolution of tidal disruption disks, revealing thermal instabilities that cause cyclical high and low accretion states, with observable consequences like outflows and radio flares, explaining late-time TDE activity.
Contribution
It introduces semi-analytic models of TDE disks that capture thermal instabilities and their observational signatures, advancing understanding of late-time TDE phenomena.
Findings
Thermal instabilities begin around 100 days post-disruption.
Disks cycle between high super-Eddington and low accretion states for up to 10 years.
Outflows during high states can produce radio flares.
Abstract
Observations of tidal disruption events (TDEs) on a timescale of years after the main flare show evidence of continued activity in the form of optical/UV emission, quasi-periodic eruptions, and delayed radio flares. Motivated by this, we explore the time evolution of these disks using semi-analytic models to follow the changing disk properties and feeding rate to the central black hole (BH). We find that thermal instabilities typically begin after the TDE, causing the disk to cycle between high and low accretion states for up to . The high state is super-Eddington, which may be associated with outflows that eject over with a range of velocities of . Collision between these mass ejections may cause radio flares. In the low state, the accretion rate slowly grows over months to…
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Taxonomy
Topicsearthquake and tectonic studies · Geomagnetism and Paleomagnetism Studies · Geophysics and Gravity Measurements
