Auroral X-ray Emission at Jupiter

Physics

Scientific paper

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6009 Aurorae, Airglow, And X-Ray Emission, 6220 Jupiter

Scientific paper

Auroral emissions from Jupiter have been observed across the electromagnetic spectrum including ultraviolet and X-ray emissions. X-ray emissions with a total power of about 1GW were observed by the Einstein Observatory, the Roentgen satellite (ROSAT), Chandra X-ray Observatory (CXO), and XMM-Newton. Previous studies (Cravens et al. 1995, Kharchenko et al. 1998, 2006, and Liu and Schultz 1999) have shown that precipitating energetic sulfur and oxygen ions can produce the observed X-rays. Sulfur and oxygen ions in the outer magnetosphere are presumably accelerated by field-aligned potentials before they precipitate into the atmosphere (Cravens et al. 2003). Collisions with atmospheric neutrals remove most of the incident ions' orbital electrons and subsequent charge transfer collisions produce X-rays. This study theoretically models the ion precipitation using cross sections for these charge exchange processes and an empirical stopping power. X-ray luminosities are determined for several monoenergetic beams. Our model also shows the altitude dependence of the X-ray photons produced and accounts for the change in observed X-ray power due to opacity effects.

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