International audienceA magneto-hydrodynamic model of boundary layers at the core–mantle boundary (CMB) is derived and used to compute the viscous and electromagnetic torques generated by the Earth's nutation forcing. The predicted electromagnetic torque alone cannot account for the dissipation estimated from the observations of the free core nutation. The presence of a viscous boundary layer in the electromagnetic skin layer at the CMB, with its additional dissipative torques, may explain the geodetic data. An apparent Ekman number at the top of the core between 2 and 4 × 10−11 is inferred depending on the electrical conductivity of the mantle
International audienceSUMMARY The Earth’s magnetic field at the core–mantle boundary is the gradient...
International audienceWe investigate the pressure torque between the fluid core and the solid mantle...
International audienceHere, we present a synthetic validation for the inversion of transient fluid m...
International audienceA magneto-hydrodynamic model of boundary layers at the core–mantle boundary (C...
International audienceA magneto-hydrodynamic model of boundary layers at the Core-Mantle Boundary (C...
The presence of an internal magnetic field influences of the Earth's nutation through the effects of...
Astronomically-determined irregular fluctuations in the Earth's rotation vector on decadal time scal...
The estimates made by Mathews et al. [2002] for the strengths of magnetic fields at the core mantle ...
International audience[1] The parameters of the nutations are now known with a good accuracy, and th...
Magnetic induction due to a steady flow of the core past a bumpy, heterogeneous mantle is investigat...
This article commences by surveying the basic dynamics of Earth's core and their impact on various m...
The core follows the precession of the mantle by virtue of coupling to it. A simple model is present...
The φ -component, εφ , of the mean electromotive force ε → generated by as...
International audienceSUMMARY The Earth’s magnetic field at the core–mantle boundary is the gradient...
International audienceWe investigate the pressure torque between the fluid core and the solid mantle...
International audienceHere, we present a synthetic validation for the inversion of transient fluid m...
International audienceA magneto-hydrodynamic model of boundary layers at the core–mantle boundary (C...
International audienceA magneto-hydrodynamic model of boundary layers at the Core-Mantle Boundary (C...
The presence of an internal magnetic field influences of the Earth's nutation through the effects of...
Astronomically-determined irregular fluctuations in the Earth's rotation vector on decadal time scal...
The estimates made by Mathews et al. [2002] for the strengths of magnetic fields at the core mantle ...
International audience[1] The parameters of the nutations are now known with a good accuracy, and th...
Magnetic induction due to a steady flow of the core past a bumpy, heterogeneous mantle is investigat...
This article commences by surveying the basic dynamics of Earth's core and their impact on various m...
The core follows the precession of the mantle by virtue of coupling to it. A simple model is present...
The φ -component, εφ , of the mean electromotive force ε → generated by as...
International audienceSUMMARY The Earth’s magnetic field at the core–mantle boundary is the gradient...
International audienceWe investigate the pressure torque between the fluid core and the solid mantle...
International audienceHere, we present a synthetic validation for the inversion of transient fluid m...