A Mass Function Constraint on Extrasolar Giant Planet Evaporation Rates
arXiv:astro-ph/0702276 · doi:10.1086/513422
Abstract
The observed mass function for all known extrasolar giant planets (EGPs) varies approximately as M^{-1} for mass M between 0.2 Jupiter masses (M_J) and 5 M_J. In order to study evaporation effects for highly-irradiated EGPs in this mass range, we have constructed an observational mass function for a subset of EGPs in the same mass range but with orbital radii <0.07 AU. Surprisingly, the mass function for such highly-irradiated EGPs agrees quantitatively with the M^{-1} law, implying that the mass function for EGPs is preserved despite migration to small orbital radii. Unless there is a remarkable compensation of mass-dependent orbital migration for mass-dependent evaporation, this result places a constraint on orbital migration models and rules out the most extreme mass loss rates in the literature. A theory that predicts more moderate mass loss gives a mass function that is closer to observed statistics but still disagrees for M < 1 M_J.
accepted by Astrophys. J. Letters on 1 February 2007
References in corpus (3)
Cited by in corpus (23)
- Kepler planets: a tale of evaporation
- Atmospheric Escape from Hot Jupiters
- Understanding the Mass-Radius Relation for Sub-Neptunes: Radius as a Proxy for Composition
- A giant comet-like cloud of hydrogen escaping the warm Neptune-mass exoplanet GJ 436b
- The Role of Core Mass in Controlling Evaporation: the Kepler Radius Distribution and the Kepler-36 Density Dichotomy
- How Thermal Evolution and Mass Loss Sculpt Populations of Super-Earths and Sub-Neptunes: Application to the Kepler-11 System and Beyond
- Tidal Evolution of Close-in Extra-Solar Planets
- The Interior Structure, Composition, and Evolution of Giant Planets
- Super-Earth Atmospheres: Self-Consistent Gas Accretion and Retention
- The physical properties of extrasolar planets
- Observable Consequences of Planet Formation Models in Systems with Close-in Terrestrial Planets
- Exoplanet HD209458b: inflated hydrogen atmosphere but no sign of evaporation
- Heating efficiency in hydrogen-dominated upper atmospheres
- Probing the Blow-Off Criteria of Hydrogen-Rich "Super-Earths"
- XUV exposed non-hydrostatic hydrogen-rich upper atmospheres of terrestrial planets. Part I: Atmospheric expansion and thermal escape
- Atmospheric Regimes and Trends on Exoplanets and Brown Dwarfs
- Rocky super-Earths or waterworlds: the interplay of planet migration, pebble accretion and disc evolution
- Escaping Particle fluxes in the atmospheres of close-in exoplanets: I. model of hydrogen
- The Roles of Tidal Evolution and Evaporative Mass Loss in the Origin of CoRoT-7 b
- Hierarchical Bayesian calibration of tidal orbit decay rates among hot Jupiters
- How planets grow by pebble accretion II: Analytical calculations on the evolution of polluted envelopes
- Evaporation of Jupiter like planets orbiting extreme horizontal branch stars
- The effects of viewing angle on the mass distribution of exoplanets