On the Cassini spacecraft observations of Iapetus

Physics

Scientific paper

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Dusty Or Complex Plasmas, Plasma Crystals, Plasma-Material Interactions, Boundary Layer Effects, Plasma Production And Heating, Astronomical And Space-Research Instrumentation, Astronomical Observations

Scientific paper

It has been reported that the recent observations of the Saturnian satellite, Iapetus, by the Cassini spacecraft support the theory proposed by us, over three decades ago, to explain the large brightness asymmetry between the leading and trailing faces of this synchronous satellite. Here we will revisit the question of the observed brightness variations, with orbital phase, not only of the outermost, large, Saturnian satellite Iapetus, but also of the large inner ones (Tethys, Dione, Rhea, and Titan). While Titan (which has a significant atmosphere) shows no brightness variation with orbital phase, the remaining inner satellites show, small but definite, brightness variations with orbital phase, which, curiously, are in the sense opposite to that of Iapetus. In other words, while the leading face of Iapetus is much darker than its trailing face, the leading faces of the large inner satellites (with the exception of Titan) are slightly brighter. Here we provide an explanation of the latter effect too by invoking the impact on the trailing faces of these inner satellites, by a class of negatively charged dust grains in the E-ring, moving in near-circular orbits, with super Kepler speeds.

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