Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/2641
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dc.contributor.authorSengupta, S-
dc.date.accessioned2008-07-11T11:08:33Z-
dc.date.available2008-07-11T11:08:33Z-
dc.date.issued2008-08-
dc.identifier.citationThe Astrophysical Journal Letters, Vol. 683, No. 2, pp. L195 – L198en
dc.identifier.urihttp://hdl.handle.net/2248/2641-
dc.description.abstractThe 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.extent109419 bytes-
dc.format.mimetypeapplication/pdf-
dc.language.isoenen
dc.publisherIOP Scienceen
dc.relation.urihttp://iopscience.iop.org/1538-4357/683/2/L195-
dc.rights© The American Astronomical Society. All rights reserved.-
dc.subjectPlanetary Systemsen
dc.subjectStars:Individual(HD 189733)en
dc.subjectPolarization-
dc.subjectScattering-
dc.titleCloudy atmosphere of the extra-solar planet HD189733b: A possible explanation of the detected B-band polarizationen
dc.typeArticleen
Appears in Collections:IIAP Publications

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