SM24A-03
Dione’s Magnetospheric Interaction

Tuesday, 15 December 2015: 16:30
2009 (Moscone West)
William S Kurth1, George B Hospodarsky1, Patricia Schippers2, Michel Moncuquet2, Alain Lecacheux2, Frank J Crary3, Krishan K Khurana4 and Donald G Mitchell5, (1)University of Iowa, Iowa City, IA, United States, (2)Paris Observatory Meudon, Meudon, France, (3)University of Colorado at Boulder, Boulder, CO, United States, (4)University of California Los Angeles, Los Angeles, CA, United States, (5)JHU/APL, Laurel, MD, United States
Abstract:
Cassini has executed four close flybys of Dione during its mission at Saturn with one additional flyby planned as of this writing. The Radio and Plasma Wave Science (RPWS) instrument observed the plasma wave spectrum during each of the four encounters and plans to make additional observations during the 17 August 2015 flyby. These observations are joined by those from the Cassini Plasma Spectrometer (CAPS), Magnetospheric Imaging Instrument (MIMI), and the Magnetometer instrument (MAG), although neither CAPS nor MAG data were available for the fourth flyby. The first and fourth flybys were near polar passes while the second and third were near wake passes. The second flyby occurred during a time of hot plasma injections which are not thought to be specifically related to Dione. The Dione plasma wave environment is characterized by an intensification of the upper hybrid band and whistler mode chorus. The upper hybrid band shows frequency fluctuations with a period of order 1 minute that suggest density variations of up to 10%. These density variations are anti-correlated with the magnetic field magnitude, suggesting a mirror mode wave. Other than these periodic density fluctuations there appears to be no local plasma source which would be observed as a local enhancement in the density although variations in the electron distribution are apparent. Wake passages show a deep density depletion consistent with a plasma cavity downstream of the moon. Energetic particles show portions of the distribution apparently absorbed by the moon leading to anisotropies that likely drive both the intensification of the upper hybrid band as well as the whistler mode emissions. We investigate the role of electron anisotropies and enhanced hot electron fluxes in the intensification of the upper hybrid band and whistler mode emissions.