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dc.contributor.authorBarman, Travis Stuart
dc.date.accessioned2014-03-03T20:07:34Z
dc.date.available2014-03-03T20:07:34Z
dc.date.issued2002-05
dc.identifier.otherbarman_travis_s_200205_phd
dc.identifier.urihttp://purl.galileo.usg.edu/uga_etd/barman_travis_s_200205_phd
dc.identifier.urihttp://hdl.handle.net/10724/20497
dc.description.abstractAtmospheric models have been calculated for M dwarf stars found in post- common envelope binary systems and extra-solar giant planets (EGPs) which have very small orbital separations. In such systems, the radiation ¯eld from the hotter companion effects the atmosphere of the much cooler M dwarf or planet. The PHOENIX model atmosphere code has been adapted to explicitly include the extrinsic radiation in the solution of either the plane parallel or spherically symmetric radia- tive transfer equation and in the calculation of the temperature structure. The updated PHOENIX code also employs a new modi¯ed UnsÄold-Lucy temperature cor- rection procedure that is stable and ensures that energy conservation is satis¯ed even in the presence of strong extrinsic °ux.|Irradiated planets located at various orbital separations from either a dM5 or a G2 primary star have been modeled for two extreme cases: one where dust clouds form and remain suspended in the atmosphere, and another where dust clouds form but completely settle out of the atmosphere. The atmospheric structure and emer- gent spectrum strongly depend on the presence or absence of dust clouds. It has also been demonstrated that neutral sodium is not in local thermodynamic equilibrium (LTE) in the outer atmosphere of irradiated EGPs.|Pre-cataclysmic variables (pre-CVs) containing a hot white dwarf (WD) and cool M dwarf have also been modeled. These models demonstrate that dramatic changes can occur in the atmosphere of an M dwarf secondary due to the incident °ux from a WD primary. A large temperature inversion, similar in appearance to a chromospheric transition region, forms in the upper atmosphere of the secondary. Also, the e®ects of irradiation have been shown to vary across the surface of the secondary leading to distinct spectra at di®erent orbital phases and inclinations.
dc.publisheruga
dc.rightspublic
dc.subjectStars
dc.subjectPlanetary Systems
dc.subjectRadiative Transfer
dc.subjectAtmospheres
dc.titleIrradiated model atmospheres for extrasolar giant planets and secondary stars of pre-cataclysmic variables
dc.typeDissertation
dc.description.degreePhD
dc.description.departmentPhysics and Astronomy
dc.description.majorPhysics
dc.description.advisorPeter H. Hauschildt
dc.description.committeePeter H. Hauschildt
dc.description.committeeLoris Magnani
dc.description.committeeHeinz-Bernd Schuttler
dc.description.committeeJames Scott Shaw
dc.description.committeePhillip C. Stancil


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