Recurrent Perihelion Activity in (3200) Phaethon
Jing Li, David Jewitt

TL;DR
This study observes recurrent perihelion activity in asteroid (3200) Phaethon, suggesting dust ejection caused by thermal processes near perihelion, which may contribute to the Geminid meteor stream.
Contribution
First detailed analysis of Phaethon's perihelion brightening linked to dust ejection mechanisms, ruling out sublimation and thermal emission as primary causes.
Findings
Phaethon brightened unexpectedly at large phase angles.
Thermal emission is insufficient to explain the brightening.
Dust ejection likely results from thermal fracture or mineral decomposition.
Abstract
We present a study of planet-crossing asteroid (3200) Phaethon at three successive perihelia in 2009, 2010 and 2012, using the NASA STEREO spacecraft. Phaethon is clearly detected in 2009 and 2012, but not in 2010. In both former years, Phaethon brightened unexpectedly by ~1 magnitude at large phase angles, inconsistent with the ~1 magnitude of steady fading expected from a discrete, macroscopic body over the same phase angle range. With a perihelion distance of 0.14 AU and surface temperatures up to ~1000 K, a thermal origin of this anomalous brightening is strongly suspected. However, simple thermal emission from Phaethon is too weak, by a factor >1000, to explain the brightening. Neither can ice survive on this body, ruling out comet-like sublimation. Our preferred explanation is that brightening occurs as a result of dust produced and ejected from Phaethon, perhaps by thermal…
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