Published March 1997
| Version public
Journal Article
A Search for a Sodium Atmosphere around Ganymede
Abstract
Long-slit high-resolution spectra have revealed that Ganymede has an atmospheric sodium column density, between a distance of 7800 and 15600 km from the satellite surface, of less than 1 × 10^8 atoms cm^(−2), a factor of 13 times smaller than the sodium density in the atmosphere of Europa at the same distance. Assuming similar processes creating sodium on both Europa and Ganymede, we estimate that the source rate for sodium production on Ganymede should be within a factor of 2 of that on Europa. Two possibilities for the lack of detectable sodium around Ganymede are that Ganymede's surface is depleted in native sodium compared to Europa's or that Ganymede has a magnetic field capable of standing off impacting energetic particles.
Additional Information
© 1997 Academic Press. Received August 26, 1996; revised November 25, 1996. We are indebted to Roger Wiens for discussions about the sputtering and potential surface characteristics of the Galilean satellites, to Richard Hill for help with the observations, to John Spencer and Elisabeth Moyer for valuable comments, and to Don Hunten for supplying the spectrograph. This research is supported by NASA through Grant HF-01056.02.94A from the Space Telescope Science Institute, which is operated by the Association of Universities for Research in Astronomy, Inc., under NASA Contract NAS5-26555.Additional details
Identifiers
- Eprint ID
- 34509
- DOI
- 10.1006/icar.1996.5675
- Resolver ID
- CaltechAUTHORS:20120927-120624917
Related works
- Describes
- 10.1006/icar.1996.5675 (DOI)
Funding
- NASA
- HF-01056.02.94A
- NASA
- NAS5-26555
- Space Telescope Science Institute
Dates
- Created
-
2012-09-28Created from EPrint's datestamp field
- Updated
-
2021-11-09Created from EPrint's last_modified field
Caltech Custom Metadata
- Caltech groups
- Division of Geological and Planetary Sciences (GPS)