Cassini radio occultations of Saturn's ionosphere:: Model comparisons using a constant water flux

Recent radio occultations of Saturn's equatorial ionosphere by the Cassini spacecraft provide important insight into this poorly constrained region. Twelve new electron density profiles identify a clear dawn/dusk asymmetry as well as two apparently separate electron density peaks. This study uses a 3D general circulation model along with 1D water diffusion calculations to examine the possibility that a topside flux of neutral water into Saturn's atmosphere may provide a loss mechanism - via charge exchange with protons - that is sufficient to reproduce the ionosphere observed by Cassini. Results indicate that a constant influx of water of (0.5 - 1.0) x 10(7) H2O cm(-2) sec(-1) is adequate for reproducing Cassini measurements, providing a good match to the main electron density peak at dawn and dusk. In addition, these calculations use a reduced rate for the reaction H+ + H-2(nu >= 4) --> H-2(+) + H, significantly diminishing its importance in Saturn's ionospheric photochemistry.