Author/Authors :
Coates، نويسنده , , A.J. and Wellbrock، نويسنده , , A. and Lewis، نويسنده , , G.R. and Jones، نويسنده , , G.H. and Young، نويسنده , , D.T. and Crary، نويسنده , , F.J. and Waite Jr.، نويسنده , , J.H.، نويسنده ,
Abstract :
One of the unexpected results of the Cassini mission was the discovery of negative ions at altitudes between 950 and 1400 km in Titanʹs ionosphere with masses up to 10,000 amu/q [Coates, A.J., Crary, F.J., Lewis, G.R., Young, D.T., Waite Jr., J.H., Sittler Jr., E.C., 2007. Discovery of heavy negative ions in Titanʹs ionosphere. Geophys. Res. Lett., 34, L22103, doi:10.1029/2007GL030978; Waite Jr., J.H., Young, D. T., Coates, A. J., Crary, F. J., Magee, B. A., Mandt, K. E., Westlake, J. H., 2008. The Source of Heavy Organics and Aerosols in Titanʹs Atmosphere, submitted to Organic Matter in Space, Proceedings IAU Symposium no. 251]. These ions are detected at low altitudes during Cassiniʹs closest Titan encounters by the Cassini plasma spectrometer (CAPS) electron spectrometer. This result is important as it is indicative of complex hydrocarbon and nitrile chemical processes at work in Titanʹs high atmosphere. They may play a role in haze formation and ultimately in the formation of heavy particles (tholins), which fall through Titanʹs atmosphere and build up on the surface. During Cassiniʹs prime mission negative ions were observed on 23 Titan encounters, including 7 in addition to those reported by Coates et al. [Coates, A.J., Crary, F.J., Lewis, G.R., Young, D.T., Waite Jr., J.H., Sittler Jr., E.C., 2007. Discovery of heavy negative ions in Titanʹs ionosphere. Geophys. Res. Lett., 34, L22103, doi:10.1029/2007GL030978]. Here, we also examine the altitude and latitude dependence of the high-mass negative ions observed in Titanʹs ionosphere, and we examine the implications of these results. We find that the maximum negative ion mass is higher at low altitude and at high latitudes. We also find a weaker dependence of the maximum mass on solar zenith angle.