Effects of depth-dependent thermal expansivity on mantle circulations and lateral thermal anomalies

Physics

Scientific paper

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Boussinesq Approximation, Earth Mantle, Free Convection, Seismology, Thermal Expansion, Prandtl Number, Rayleigh Number, Rheology, Stream Functions (Fluids), Thermal Boundary Layer

Scientific paper

The influences of depth-dependent thermal expansivity on the structure of Newtonian thermal convection and lateral thermal anomalies are studied. In an aspect-ratio ten box the effects of the depth-dependent expansivity are to produce large aspect-ratio cells with a few relatively stationary upwellings. The lateral thermal anomalies in the lower mantle are greatly diminished by depth-dependent expansivity. This together with a decrease in the temperature derivative of seismic velocities in the lower mantle would support the low level of lateral heterogeneities found in recent tomographic studies.

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