Contribution of tidal dissipation to lunar thermal history

Computer Science

Scientific paper

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Earth-Moon System, Energy Dissipation, Lunar Evolution, Lunar Temperature, Lunar Tides, Compressibility, Eccentric Orbits, Lunar Core, Lunar Crust, Lunar Mantle, Lunar Orbits, Lunar Rotation, Orbital Resonances (Celestial Mechanics), Tides, Heat Sources, Moon, Thermal History, Orbits, Evolution, Radius, Energy, Models, Incompressibility, Thermal Properties, Core, Mantle, Temperatures, Earth, Distance, Eccentricity, Librations

Scientific paper

Possible contributions of tidal heating to the thermal history of the moon are investigated, and conditions under which such heating would have been an important factor in the evolution of the moon are defined as precisely as possible within the bounds of the uncertainties. The tidal dissipation is defined as a function of position in the moon and of the earth-moon separation for a homogeneous incompressible moon. Results for the dissipation are given for eccentricities of zero and 0.055 as well as for the lunar obliquity as determined by the equilibrium Cassini states. Possible orbital resonances which interrupt the assumed simplified expansion of the lunar orbit are considered, along with radial variations in rigidity. The dissipation in a two-layer model moon with a molten inner core and an outer mantle with the moon's present rigidity is determined, and implications of the results for the role of tidal heating in the history of the moon are discussed.

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