http://arxiv.org/abs/1908.05720
Mass-spring model simulations are used to investigate past spin states of Phobos and Deimos. From an initially tidally locked state, we find crossing of a spin-orbit resonance with Mars or a mean motion resonance with each other does not excite tumbling in Phobos or Deimos. However, once tumbling these moons can remain so for an extended period and during this time their orbital eccentricity can be substantially reduced. We attribute the tendency for simulations of an initially tumbling body to drop into spin-synchronous state at very low eccentricity to the insensitivity of the tumbling chaotic zone width to eccentricity. After a tumbling body enters the spin synchronous resonance, it can exhibit long lived non-principal axis rotation and this too can prolong the period of time with enhanced tidally generated energy dissipation. We propose that the low orbital eccentricities of Phobos and Deimos could in part be due to spin excitation by impacts rather than tidal evolution following orbital resonance excitation.
A. Quillen, M. Lane, M. Nakajima, et. al.
Mon, 19 Aug 19
12/46
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