We report on the first successful, spatially resolved spectroscopic observations of Io's SO 2 atmosphere. Observations made with the Hubble Space Telescope Faint Object Spectrograph on 1 August 1996 using the 0.26 aperture have provided detections of SO 2 gas in absorption in three locations on the
Eclipse Spectroscopy of Io's Atmosphere
โ Scribed by Antonin H Bouchez; Michael E Brown; Nicholas M Schneider
- Publisher
- Elsevier Science
- Year
- 2000
- Tongue
- English
- Weight
- 162 KB
- Volume
- 148
- Category
- Article
- ISSN
- 0019-1035
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โฆ Synopsis
High resolution optical (4193-6619 ร ) spectra of Io in eclipse show auroral emission in five lines: [OI] 6300, 6363, 5577 ร and Na 5889, 5896 ร . We conclude that Io's diffuse red emissions imaged by the Galileo Solid State Imager (P. E. Geissler et al. 1999, Science 285, 870-874) are due to impact or dissociative excitation of oxygen, while diffuse green emissions are caused by the impact or dissociative excitation of sodium. No emission lines were detected in the blue region of the spectra, suggesting that the intense emission observed above Io's equatorial plumes is due to a molecular species such as SO 2 or SO.
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A one-dimensional Direct Simulation Monte Carlo (DSMC) model is used to examine the effects of a non-condensable species on Io's sulfur dioxide sublimation atmosphere during eclipse and just after egress. Since the vapor pressure of SO 2 is extremely sensitive to temperature, the frost-supported day
The circumplanetary flow of Io's SO 2 atmosphere is modeled using the direct simulation Monte Carlo (DSMC) method. This flow develops as gas sublimates from SO 2 frost in the warm subsolar region and flows toward the colder night-side, where it condenses. The axisymmetric model presented extends fro
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