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Radio science investigations of the Saturn system with Voyager 1 - Preliminary resultsAnalyses of Voyager 1 radio occultation measurements of the Saturn atmosphere near 75 deg south latitude and of the Titan equatorial atmosphere are presented. Molecular nitrogen appears to be the primary atmospheric constituent of Titan, whose clouds are probably methane ice. Solar abundance considerations of the data suggest large quantities of surface methane near its triple-point temperature, so that the three phases of methane could play a role on Titan analogous to that of water on earth. Ionospheric electron concentration and plasma scale height for the Saturn polar cap and monochromatic attenuation of the Saturn rings are also considered, along with radio tracking figures for the masses of two moons, Rhea and Titan.
Document ID
19810043826
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Tyler, G. L.
(Stanford Univ. CA, United States)
Eshleman, V. R.
(Stanford University Stanford, Calif., United States)
Anderson, J. D.
(Stanford Univ. CA, United States)
Levy, G. S.
(Stanford Univ. CA, United States)
Lindal, G. F.
(Stanford Univ. CA, United States)
Wood, G. E.
(California Institute of Technology, Jet Propulsion Laboratory, Pasadena Calif., United States)
Croft, T. A.
(SRI International Menlo Park, Calif., United States)
Date Acquired
August 11, 2013
Publication Date
April 10, 1981
Publication Information
Publication: Science
Volume: 212
Subject Category
Lunar And Planetary Exploration
Accession Number
81A28230
Distribution Limits
Public
Copyright
Other

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