Viscous Relaxation Times of the Core and Mantle of Mars from Observations of Tidal Decay of the Orbit of Phobos
The orbit of Phobos exhibits an along-track acceleration, which suggests energy dissipation in the Mars-Phobos system. We hypothesize that the inferred dissipation occurs within Mars. We explore the response of a layered, incompressible Maxwell viscoelastic Mars to tidal forcing by Phobos using norm...
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| Language: | en_ca |
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2011
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| Online Access: | http://hdl.handle.net/1807/31386 |