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Detection of Thermal Emission from an Extrasolar Planet

David Charbonneau et al 2005 ApJ 626 523-529   doi: 10.1086/429991  Help

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David Charbonneau1, Lori E. Allen1, S. Thomas Megeath1, Guillermo Torres1, Roi Alonso2, Timothy M. Brown3, Ronald L. Gilliland4, David W. Latham1, Georgi Mandushev5, Francis T. O'Donovan6 and Alessandro Sozzetti1,7
1 Harvard-Smithsonian Center for Astrophysics, 60 Garden Street, Cambridge, MA 02138
2 Instituto de Astrofísica de Canarias, 38200 La Laguna, Tenerife, Spain
3 High Altitude Observatory, National Center for Atmospheric Research, 3450 Mitchell Lane, Boulder, CO 80307
4 Space Telescope Science Institute, 3700 San Martin Drive, Baltimore, MD 21218
5 Lowell Observatory, 1400 West Mars Hill Road, Flagstaff, AZ 86001
6 California Institute of Technology, 1200 East California Boulevard, Pasadena, CA 91125
7 Home institution: Department of Physics and Astronomy, University of Pittsburgh, 100 Allen Hall, 3941 O'Hara Street, Pittsburgh, PA 15260
E-mail: dcharbonneau@cfa.harvard.edu

ABSTRACT. We present Spitzer Space Telescope infrared photometric time series of the transiting extrasolar planet system TrES-1. The data span a predicted time of secondary eclipse, corresponding to the passage of the planet behind the star. In both bands of our observations, we detect a flux decrement with a timing, amplitude, and duration as predicted by published parameters of the system. This signal represents the first direct detection of (i.e., the observation of photons emitted by) a planet orbiting another star. The observed eclipse depths (in units of relative flux) are 0.00066 ± 0.00013 at 4.5 μm and 0.00225 ± 0.00036 at 8.0 μm. These estimates provide the first observational constraints on models of the thermal emission of hot Jupiters. Assuming that the planet emits as a blackbody, we estimate an effective temperature of Tp = 1060 ± 50 K. Under the additional assumptions that the planet is in thermal equilibrium with the radiation from the star and emits isotropically, we find a Bond albedo of A = 0.31 ± 0.14. This would imply that the planet absorbs the majority of stellar radiation incident upon it, a conclusion of significant impact to atmospheric models of these objects. We also compare our data to a previously published model of the planetary thermal emission, which predicts prominent spectral features in our observational bands due to water and carbon monoxide. This model adequately reproduces the observed planet-to-star flux ratio at 8.0 μm; however, it significantly overpredicts the ratio at 4.5 μm. We also present an estimate of the timing of the secondary eclipse, which we use to place a strong constraint on the expression e cos ω, where e is the orbital eccentricity and ω is the longitude of periastron. The resulting upper limit on e is sufficiently small that we conclude that tidal dissipation is unlikely to provide a significant source of energy interior to the planet.

Subject headings: binaries: eclipsing; infrared: stars; planetary systems; stars: individual (TrES-1); techniques: photometric

Print publication: Issue 1 (2005 June 10)
Received 2005 February 3, accepted for publication 2005 March 1

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