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Detailed Reference Information |
Johnson, T.V., Matson, D.L. and Carlson, R.W. (1976). Io’s atmosphere and ionosphere: New limits on surface pressure from plasma models. Geophysical Research Letters 3: doi: 10.1029/GL003i006p00293. issn: 0094-8276. |
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We have studied charge particle impact as a mechanism for the production of Io's ionosphere. Pioneer 10 thermal plasma measurements and magnetospheric plasma models which explain the observed spatial distribution of neutral hydrogen and sodium atoms in the vicinity of Jupiter's satellite Io imply electron fluxes of ~1010 cm-2 sec-1. The fluxes and the temperature (~100 eV) of this plasma suggest that electron impact ionization is the dominant process in forming the ionosphere of Io. It is found that the surface number density of the neutral species required to match the observed electron density profiles is ~109 cm-3 or less. This value is two orders of magnitude lower than previous estimates. |
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American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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