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Voyager radio science observations of Neptune and TritonVoyager 2 undertook radio science investigations of the Neptune and Triton masses and densities, as well as of their atmospheric and ionospheric vertical structures, the atmospheric composition and low-order gravitational harmonics of Neptune, and ring material characteristics. Upon probing the atmosphere of Neptune to a pressure level of about 500,000 Pa, the effects of a methane cloud region and of ammonia absorption below the cloud have become apparent. The tenuous neutral atmosphere of Triton produced distinct signatures in the occultation data; it is inferred that the Triton atmosphere is controlled by water-pressure equilibrium with surface ices.
Document ID
19900031376
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Tyler, G. L.
(Stanford University CA, United States)
Sweetnam, D. N.
(Stanford Univ. CA, United States)
Anderson, J. D.
(Stanford Univ. CA, United States)
Borutzki, S. E.
(Stanford Univ. CA, United States)
Campbell, J. K.
(Stanford Univ. CA, United States)
Kursinski, E. R.
(Stanford Univ. CA, United States)
Levy, G. S.
(Stanford Univ. CA, United States)
Lindal, G. F.
(Stanford Univ. CA, United States)
Lyons, J. R.
(Stanford Univ. CA, United States)
Wood, G. E.
(JPL Pasadena, CA, United States)
Date Acquired
August 14, 2013
Publication Date
December 15, 1989
Publication Information
Publication: Science
Volume: 246
ISSN: 0036-8075
Subject Category
Lunar And Planetary Exploration
Accession Number
90A18431
Distribution Limits
Public
Copyright
Other

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