Thomas R. Geballe
University of Hawaii at Manoa
312 Papers
4.5K Citations
Thomas R. Geballe is an academic researcher from University of Hawaii at Manoa. The author has contributed to research in topics: Stars & Brown dwarf. The author has an hindex of 71, co-authored 301 publications.
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Papers
The Spitzer Infrared Spectrometer view of V4334 Sgr (Sakurai's Object)
A. Evans,V. H. Tyne,J. Th. van Loon,Barry Smalley,Thomas R. Geballe,Robert D. Gehrz,Charles E. Woodward,Albert A. Zijlstra,Elisha Polomski,M. T. Rushton,S. P. S. Eyres,Sumner Starrfield,Joachim Krautter,R. M. Wagner +13 more
TL;DR: In this paper, a very late thermal pulse object V4334 Sgr (Sakurai's Object) was observed with the Infrared Spectrometer (IRS) on the Spitzer Space Telescope.
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Titan's 5 micrometers spectral window: carbon monoxide and the albedo of the surface.
TL;DR: The spectrum of Titan near 5 micrometers is found to be dominated by absorption from the carbon monoxide 1-0 vibration-rotation band and the mole fraction of CO in the atmosphere is significantly lower than previous estimates for tropospheric CO.
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The Spitzer IRS view of V4334 Sgr (Sakurai's Object)
A. Evans,V. H. Tyne,J. Th. van Loon,Barry Smalley,Thomas R. Geballe,Robert D. Gehrz,Chick E Woodward,A. A. Zijlstra,Elisha Polomski,M. T. Rushton,S. P. S. Eyres,Sumner Starrfield,J. Krautter,Robert Wagner +13 more
TL;DR: In this paper, a very late thermal pulse object V4334 Sgr (Sakurai's Object) was observed with the Infrared Spectrometer (IRS) on the Spitzer Space Telescope.
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High-resolution spectroscopy of Saturn at 3 microns : CH4, CH3D, C2H2, C2H6, PH3, clouds, and haze
TL;DR: In this paper, a high-resolution 2.87-3.54-μm spectrum of the southern temperate region of Saturn was obtained with NIRSPEC at Keck II.
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Evidence for Germane in Saturn
TL;DR: In this article, it is suggested that future more realistic radiative transfer models that include the effects of scattering within a cloud layer will probably only reduce the mole fraction presently derived for germane, by increasing the effective path length in a given atmospheric layer.
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