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The atmosphere of IoObservations of Io suggest that it may have an atmosphere in which sodium vapor, ammonia, and nitrogen are important constituents. Several atmospheric models consisting of these gases are tested as a function of total content against the Pioneer 10 observations and for stability against escape. The results suggest that the atmosphere is very tenuous and that the interpretation of the ionosphere detected by Pioneer 10 by a static model may be inconsistent with the sodium-cloud observations. It is postulated that ionization may also be escaping and that sodium may be comparable in content in the atmosphere with some molecular constituent such as NH3 or N2. Sodium and this molecular component then dominate the atmosphere. It is also suggested that particle precipitation contributes to heating of the atmosphere and to the production of ionization; the difference between day- and nighttime ionospheres and possible trailing and leading side effects may relate to the nature of the particle energy distributions. These distributions may result from the peculiar interaction of Io with the Jovian magnetosphere.
Document ID
19770039288
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Gross, S. H.
(Polytechnic Inst. of New York Farmingdale, NY, United States)
Ramanathan, G. V.
(New York, Polytechnic Institute, Farmingdale, N.Y., United States)
Date Acquired
August 9, 2013
Publication Date
December 1, 1976
Publication Information
Publication: Icarus
Volume: 29
Subject Category
Lunar And Planetary Exploration
Accession Number
77A22140
Funding Number(s)
CONTRACT_GRANT: NGR-33-006-068
Distribution Limits
Public
Copyright
Other

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