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• W1900397706 abstract "The geological evolution of length of day (LOD) variations is mainly controlled by the frictional tidal torque responsible for the secular slowdown of the Earth′s rotation and for the receding of the Moon. Superimposed on this variation, which has existed since the early history of the planet, there are, at shorter timescales (less than 1 Myr), LOD perturbations induced by the glaciation-deglaciation cycles. In this paper, we investigate the influence of mantle dynamics on LOD at the geological timescale. We use the complete non-linear equations to compute the influence of mantle density heterogeneities on the angular velocity of the rotation, that is to say on the LOD. We discuss the degree zero coefficient of the spherical harmonic expansion of the mantle mass anomaly, which is strongly dependent on the conservation of mass of the Earth." @default.
• W1900397706 created "2016-06-24" @default.
• W1900397706 creator A5046503665 @default.
• W1900397706 date "2011-09-23" @default.
• W1900397706 modified "2023-10-11" @default.
• W1900397706 title "Length of day variations due to mantle dynamics at geological timescale" @default.
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• W1900397706 doi "https://doi.org/10.1111/j.1365-246x.2011.05169.x" @default.
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