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Origins of Hot Jupiters from the Stellar Obliquity Distribution
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Origins of Hot Jupiters from the Stellar Obliquity Distribution
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The obliquity of a star, or the angle between its spin axis and the average orbit normal of its companion planets, provides a unique constraint on that system's evolutionary history. Unlike the Solar System, where the Sun's equator is nearly aligned with its companion planets, many hot Jupiter systems have been discovered with large spin-orbit misalignments, hosting planets on polar or retrograde orbits. We demonstrate that, in contrast to stars harboring hot Jupiters on circular orbits, those with eccentric companions follow no population-wide obliquity trend with stellar temperature. This finding can be naturally explained through a combination of high-eccentricity migration and tidal damping. Furthermore, we show that the joint obliquity and eccentricity distributions observed today are consistent with the outcomes of high-eccentricity migration, with no strict requirement to invoke the other hot Jupiter formation mechanisms of disk migration or in-situ formation. At a population-wide level, high-eccentricity migration can consistently shape the dynamical evolution of hot Jupiter systems.
Forward citations
Cited by 3 Pith papers
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Warm Sub-Saturns Orbiting Single Stars Are Spin-Orbit Aligned
Warm sub-Saturns around single cool stars are predominantly aligned whereas hot sub-Saturns are frequently misaligned (3.2σ), a separation-dependent transition the authors attribute to high-eccentricity migration.
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Companion Architectures of Sub-Saturns: Distinct Migration Pathways Across the Neptunian Landscape
Desert/ridge sub-Saturns show ~10% nearby-companion rates like hot Jupiters; savanna ones show ~70% like warm Jupiters, supporting HEM versus quiescent migration.
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On the Eccentricity Distribution and Tidal Evolution of Transiting Brown Dwarfs
Short-period (P<16 d) transiting brown dwarfs are low-eccentricity while longer-period ones are more excited; assuming a shared primordial Beta distribution, tidal evolution constrains Q_BD ≈ 10^{7.1–8.1}.
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