Abstract

On September 21, 1998, the outer jovian satellites Himalia (J6), Elara (J7), Carme (J11), Pasiphae (J8), and Sinope (J9) were detected in the J, H, and K s bandpasses in the course of the Two-Micron All Sky Survey. Similarities in near-infrared colors are consistent with the hypothesis that the outer satellites in prograde orbits are fragments of a captured C-type asteroid. The retrograde satellites in general exhibit considerable diversity. The nondetection of retrograde Ananke is significant in that it requires visible to near-infrared reddening close to that of prograde Himalia and very different from the other retrograde satellites. It is suggested that the retrograde jovian satellites are fragments of a captured parent body more heterogeneous than the prograde parent. Alternatively, it is suggested that the retrograde satellites arose from more than one retrograde capture event and possible subsequent fragmentation.

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