Issue |
A&A
Volume 580, August 2015
|
|
---|---|---|
Article Number | A12 | |
Number of page(s) | 22 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/201525982 | |
Published online | 20 July 2015 |
Modelling the local and global cloud formation on HD 189733b
1
SUPA, School of Physics and Astronomy, University of St
Andrews, North Haugh, St
Andrews, Fife
KY16 9SS, UK
2
NYU Abu Dhabi, PO Box 129188, Abu
Dhabi, UAE
3
Niels Bohr Institute & Centre for Star and Planet
Formation, University of Copenhagen, 2100
Copenhagen,
Denmark
Received: 27 February 2015
Accepted: 21 May 2015
Context. Observations suggest that exoplanets such as HD 189733b form clouds in their atmospheres which have a strong feedback onto their thermodynamical and chemical structure, and overall appearance.
Aims. Inspired by mineral cloud modelling efforts for brown dwarf atmospheres, we present the first spatially varying kinetic cloud model structures for HD 189733b.
Methods. We apply a 2-model approach using results from a 3D global radiation-hydrodynamic simulation of the atmosphere as input for a detailed, kinetic cloud formation model. Sampling the 3D global atmosphere structure with 1D trajectories allows us to model the spatially varying cloud structure on HD 189733b. The resulting cloud properties enable the calculation of the scattering and absorption properties of the clouds.
Results. We present local and global cloud structure and property maps for HD 189733b. The calculated cloud properties show variations in composition, size and number density of cloud particles which are strongest between the dayside and nightside. Cloud particles are mainly composed of a mix of materials with silicates being the main component. Cloud properties, and hence the local gas composition, change dramatically where temperature inversions occur locally. The cloud opacity is dominated by absorption in the upper atmosphere and scattering at higher pressures in the model. The calculated 8 μm single scattering albedo of the cloud particles are consistent with Spitzer bright regions. The cloud particles scattering properties suggest that they would sparkle/reflect a midnight blue colour at optical wavelengths.
Key words: planets and satellites: individual: HD 189733b / planets and satellites: atmospheres / methods: numerical
© ESO, 2015
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