2009ApJ...699..478D


Query : 2009ApJ...699..478D

2009ApJ...699..478D - Astrophys. J., 699, 478-485 (2009/July-1)

Search for carbon monoxide in the atmosphere of the transiting exoplanet HD 189733b.

DESERT J.-M., LECAVELIER DES ETANGS A., HEBRARD G., SING D.K., EHRENREICH D., FERLET R. and VIDAL-MADJAR A.

Abstract (from CDS):

Water, methane, and carbon monoxide are expected to be among the most abundant molecules besides molecular hydrogen in the hot atmosphere of close-in extrasolar giant planets. Atmospheric models for these planets predict that the strongest spectrophotometric features of those molecules are located at wavelengths ranging from 1 to 10 µm making this region of particular interest. Consequently, transit observations in the mid-infrared (mid-IR) allow the atmospheric content of transiting planets to be determined. We present new primary transit observations of the hot-Jupiter HD 189733b, obtained simultaneously at 4.5 and 8 µm with the Infrared Array Camera onboard the Spitzer Space Telescope. Together with a new refined analysis of previous observations at 3.6 and 5.8 µm using the same instrument, we are able to derive the system parameters, including planet-to-star radius ratio, impact parameter, scale of the system, and central time of the transit from fits of the transit light curves at these four wavelengths. We measure the four planet-to-star radius ratios, to be (Rp/R{*})_3.6 µm_= 0.1545 ± 0.0003, (Rp/R{*})_4.5 µm_= 0.1557±0.0003, (Rp/R{*})_5.8 µm_= 0.1547±0.0005, and (Rp/R{*})_8 µm_= 0.1544±0.0004. The high accuracy of the planet radii measurement allows the search for atmospheric molecular absorbers. Contrary to a previous analysis of the same data set, our study is robust against systematics and reveals that water vapor absorption at 5.8 µm is not detected in this photometric data set. Furthermore, in the band centered around 4.5 µm we find a hint of excess absorption with an apparent planetary radius ΔRp/R*= 0.00128±0.00056 larger (2.3σ) than the one measured simultaneously at 8 µm. This value is 4σ above what would be expected for an atmosphere where water vapor is the only absorbing species in the near-IR. This shows that an additional species absorbing around 4.5 µm could be present in the atmosphere. Carbon monoxide (CO) being a strong absorber at this wavelength is a possible candidate and this may suggest a large CO/H2 O ratio between 5 and 60.

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Journal keyword(s): eclipses - planetary systems - stars: individual: HD189733b - techniques: photometric

Simbad objects: 5

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Number of rows : 5
N Identifier Otype ICRS (J2000)
RA
ICRS (J2000)
DEC
Mag U Mag B Mag V Mag R Mag I Sp type #ref
1850 - 2026
#notes
1 * bet Pic PM* 05 47 17.0876901 -51 03 59.441135 4.13 4.03 3.86 3.74 3.58 A6V 2087 1
2 Ross 905 PM* 11 42 11.0933350978 +26 42 23.650782778   12.06 10.613 10.272 8.24 M3V 750 1
3 HD 189733 BY* 20 00 43.7129433648 +22 42 39.073143456 9.241 8.578 7.648 7.126 6.68 K2V 991 1
4 HD 189733b Pl 20 00 43.7129433648 +22 42 39.073143456           ~ 1610 1
5 HD 209458b Pl 22 03 10.7727465312 +18 53 03.549393384           ~ 2037 1

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