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Cloudy atmosphere of the extra-solar planet HD189733b: A possible explanation of the detected B-band polarization

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dc.contributor.author Sengupta, S
dc.date.accessioned 2008-07-11T11:08:33Z
dc.date.available 2008-07-11T11:08:33Z
dc.date.issued 2008-08
dc.identifier.citation The Astrophysical Journal Letters, Vol. 683, No. 2, pp. L195 – L198 en
dc.identifier.uri http://hdl.handle.net/2248/2641
dc.description.abstract The peak amplitude of linear polarization detected recently from an extraso- lar hot giant planet HD 189733b, is a few times of 10−4 , more than an order of magnitude higher than all theoretical predictions. Rayleigh scattering off H2 and He may although give rise to a planet-star flux ratio of the order of 10−4 in the blue band, it cannot account for the high polarization unless the planet has an unusually extended atmosphere. Therefore, it is suggested that the high polariza- tion should be attributed to the presence of a thin cloud of sub-micron size dust grains in the upper visible atmosphere which supports the observational finding of an almost feature-less transmission spectrum in the optical with no indication of the expected alkaline absorption features. It is found that the polarimetry observation allows for a small eccentricity of the orbit that is predicted from the time delay of the secondary eclipse of the planet. The estimated longitude of the ascending node is 16o ± 6 which interestingly coincides with the observationally inferred location of the peak hemisphere-integrated brightness. en
dc.format.extent 109419 bytes
dc.format.mimetype application/pdf
dc.language.iso en en
dc.publisher IOP Science en
dc.relation.uri http://iopscience.iop.org/1538-4357/683/2/L195
dc.rights © The American Astronomical Society. All rights reserved.
dc.subject Planetary Systems en
dc.subject Stars:Individual(HD 189733) en
dc.subject Polarization
dc.subject Scattering
dc.title Cloudy atmosphere of the extra-solar planet HD189733b: A possible explanation of the detected B-band polarization en
dc.type Article en


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