Physics
Scientific paper
Dec 2006
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006agufm.p41a1250b&link_type=abstract
American Geophysical Union, Fall Meeting 2006, abstract #P41A-1250
Physics
2756 Planetary Magnetospheres (5443, 5737, 6033), 6055 Surfaces, 6280 Saturnian Satellites
Scientific paper
Cassini made 3 close flybys of Enceladus and one each of Tethys, Dione Rhea and Hyperion in 2005. Field and plasma observations obtained during these flybys provide a unique opportunity to understand the interactions of unmagnetized moons with a subsonic, sub-Alfvenic plasma. We examine the magnetic signatures of each of these moons to infer whether the moon is a net contributor to the plasma (draped magnetic field consistent with the slowing down of plasma) or an absorber like the Earth's moon (enhanced field strength in the wake). Field and plasma observations from these moons confirm that Enceladus is the main source of plasma in Saturn's magnetosphere. Surprisingly, Dione also displays the characteristics of a plasma loading moon, even though its net contribution to the plasma in the Saturnian magnetosphere is expected to be small. Tethys and Rhea clearly belong to the class of mass-absorbing moons. The wakes of these moons were observed to have enhanced field strengths and the magnetic field appeared to be drawn into the wakes from the flanks. However, it must be pointed out that the most sensitive measurement of mass-loading is provided by those passes which occur just upstream of the moons. Until, we obtain such passes, some mass-loading at these moons cannot be ruled out. Finally, no field signature was observed to be associated with Hyperion. This may be due to the large distance of the wake flyby such that that the wake had dissipated at the location of Cassini. Alternatively, the plasma flow may have had a large deviation from the corotation flow direction making the spacecraft miss the wake crossing.
Burton Marcia
Dougherty K. M. K. M.
Khurana Krishan K.
Russell Christopher T.
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