Formation of Ultra-Short-Period Planets by Obliquity-Driven Tidal Runaway
Sarah Millholland, Christopher Spalding

TL;DR
This paper proposes a new mechanism where obliquity-driven tidal runaway causes inward migration of small, rocky planets, explaining the formation of ultra-short-period planets close to their host stars.
Contribution
It introduces planetary obliquity tides and a positive feedback loop as a novel pathway for ultra-short-period planet formation, supported by secular dynamics analysis.
Findings
Obliquity tides can cause runaway inward migration of close-in planets.
Conditions for runaway migration are consistent with observed ultra-short-period planet features.
High obliquity states can stall migration, explaining observed period distributions.
Abstract
Small, rocky planets have been found orbiting in extreme proximity to their host stars, sometimes down to only stellar radii. These ultra-short-period planets (USPs) likely did not form in their present-day orbits, but rather migrated from larger initial separations. While tides are the probable cause of this migration, the tidal source has remained uncertain. Here we introduce planetary obliquity tides as a natural pathway for the production of USPs within close-in multi-planet systems. The crucial idea is that tidal dissipation generally forces planetary spin vectors to equilibrium configurations called "Cassini states", in which the planetary obliquities (axial tilts) are non-zero. In these cases, sustained tidal dissipation and inward orbital migration are inevitable. Migration then increases the obliquity and strengthens the tides, creating a positive feedback loop. Thus,…
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Taxonomy
TopicsAstro and Planetary Science · Stellar, planetary, and galactic studies · Astronomy and Astrophysical Research
