Rayleigh scattering in the transit spectrum of HD 189733b (original) (raw)
A&A 481, L83-L86 (2008)
Letter to the Editor
1 CNRS, UMR 7095, Institut d'Astrophysique de Paris, 98bis boulevard Arago, 75014 Paris, France e-mail: lecaveli@iap.fr
2 UPMC Univ. Paris 6, UMR 7095, Institut d'Astrophysique de Paris, 98bis boulevard Arago, 75014 Paris, France
3 Physikalisches Institut, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
Received: 11 January 2008
Accepted: 18 February 2008
Abstract
The transit spectrum of the exoplanet HD 189733b has recently been obtained between 0.55 and 1.05 _μ_m. Here we present an analysis of this spectrum. We develop first-order equations to interpret absorption spectra. In the case of HD 189733b, we show that the observed slope of the absorption as a function of wavelength is characteristic of extinction proportional to the inverse of the fourth power of the wavelength (). Assuming an extinction dominated by Rayleigh scattering, we derive an atmospheric temperature of 1340 ± 150 K. If molecular hydrogen is responsible for the Rayleigh scattering, the atmospheric pressure at the planetary characteristic radius of 0.1564 stellar radius must be 410 ± 30 mbar. However the preferred scenario is scattering by condensate particles. Using the Mie approximation, we find that the particles must have a low value for the imaginary part of the refraction index. We identify MgSiO3 as a possible abundant condensate whose particle size must be between ~10-2 and ~10-1 _μ_m. For this condensate, assuming solar abundance, the pressure at 0.1564 stellar radius is found to be between a few microbars and few millibars, and the temperature is found to be in the range 1340–1540 K, and both depend on the particle size.
Key words: stars: planetary systems / scattering / techniques: spectroscopic / stars: individual: HD 189733b
© ESO, 2008