Understanding the Role of Saturn's Magnetosphere in Determining the Thermal Structure of Titan's Upper Atmosphere

Physics

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[0343] Atmospheric Composition And Structure / Planetary Atmospheres, [2732] Magnetospheric Physics / Magnetosphere Interactions With Satellites And Rings, [5405] Planetary Sciences: Solid Surface Planets / Atmospheres, [6281] Planetary Sciences: Solar System Objects / Titan

Scientific paper

An updated analysis of the Cassini Ion-Neutral Mass Spectrometer data by Westlake et al. [2011] revealed that the temperatures and neutral densities in Titan's upper atmosphere were strongly correlated with the intensity of its plasma environment, as determined by CAPS-ELS and Magnetometer data (Rymer et al. [2009] and Simon et al. [2010]). In this study, we present three-dimensional (3-D) global simulations from the Titan Global Ionosphere-Thermosphere Model (T-GITM) in order to reproduce the INMS data. We investigate to what extent magnetospheric heating is required by the 3-D model in order to accurately reproduce the Cassini INMS data between TA and T40 using T-GITM. Moreover, we examine the simulated thermal structures during different magnetospheric environments: Plasma Sheet, Lobe, and Intermediate. In particular, we examine the impacts of magnetospheric heating on the escape of the major atmospheric species (N2, CH4, and H2).

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