Physics
Scientific paper
Dec 2011
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011agufmsm14a..05s&link_type=abstract
American Geophysical Union, Fall Meeting 2011, abstract #SM14A-05
Physics
[2732] Magnetospheric Physics / Magnetosphere Interactions With Satellites And Rings, [5719] Planetary Sciences: Fluid Planets / Interactions With Particles And Fields, [5780] Planetary Sciences: Fluid Planets / Tori And Exospheres, [6281] Planetary Sciences: Solar System Objects / Titan
Scientific paper
Prior to Cassini's arrival at Saturn, nitrogen ions were thought to dominate heavy plasma in Saturn's magnetosphere and that Titan's atmosphere was the source of this nitrogen. Therefore, the presence of a Titan nitrogen torus was anticipated. However, it is now known water-group ions dominate Saturn's heavy ion plasma. While nitrogen ions have been detected beyond the orbit of Rhea, they appear to be originating from the Enceladus plumes with little nitrogen plasma detected in the magnetosphere near Titan's orbit. These results appear inconsistent with the expectation that Titan's dense relatively unprotected atmosphere should provide a significant source of heavy particles to Saturn's magnetosphere. This inconsistency suggests that the plasma environment at Titan's orbit is much more complex than originally anticipated. In this talk, we expand on our previous research that categorizes the plasma environments near Titan to include all locations along Titan's orbit. Using these categories, we develop characteristic plasma spectra of each type of environment and use these results in a 3D Monte Carlo model to more accurately examine fate of nitrogen and methane escaping Titan's atmosphere. These results are compared to Cassini observations to determine if Titan is capable of generating tori.
Johnson Robert E.
Mitchell Donald G.
Rymer Abigail M.
Smith Howard T.
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