We develop the theory for the magnetic to magnetic and kinetic to magnetic energy transfer between different spherical harmonic degrees due to the interaction of fluid flow and radial magnetic field at the top of the Earth's core. We show that non-zero secular variation of the total magnetic energy could be significant and may provide evidence for the existence of stretching secular variation, which suggests the existence of radial motions at the top of the Earth's core-whole core convection or MAC waves. However, the uncertainties of the small scales of the geomagnetic field prevent a definite conclusion. Combining core field and flow models we calculate the detailed magnetic to magnetic and kinetic to magnetic energy transfer matrices. Th...
The core follows the precession of the mantle by virtue of coupling to it. A simple model is present...
International audienceTo understand the dynamics of the Earth’s fluid, iron-rich outer core, only in...
The Earth's internal magnetic field varies on timescales of months to billions of years. The field i...
This article commences by surveying the basic dynamics of Earth's core and their impact on various m...
The mechanism by which the Earth’s magnetic field is generated is thought to be thermal convection i...
International audienceWe test the ability of large scale velocity fields inferred from geomagnetic s...
International audienceWe present a method to characterize the spectral transfers of magnetic energy ...
As Earth's main magnetic field weakens, our magnetic shield against the onslaught of the solar wind ...
We test the ability of large scale velocity fields inferred from geomagnetic secular variation data...
We present a method to characterize the spectral transfers of magnetic energy between scales in simu...
International audienceWe use numerical dynamos to investigate the possible role of magnetic diffusio...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary S...
International audienceThe geodynamo features a broad separation between the large scale at which Ear...
We study the transfer of energy between different scales for forced three-dimensional MHD turbulent ...
We study energy transfers during magnetic energy growth in small-scale and large-scale dynamos. We p...
The core follows the precession of the mantle by virtue of coupling to it. A simple model is present...
International audienceTo understand the dynamics of the Earth’s fluid, iron-rich outer core, only in...
The Earth's internal magnetic field varies on timescales of months to billions of years. The field i...
This article commences by surveying the basic dynamics of Earth's core and their impact on various m...
The mechanism by which the Earth’s magnetic field is generated is thought to be thermal convection i...
International audienceWe test the ability of large scale velocity fields inferred from geomagnetic s...
International audienceWe present a method to characterize the spectral transfers of magnetic energy ...
As Earth's main magnetic field weakens, our magnetic shield against the onslaught of the solar wind ...
We test the ability of large scale velocity fields inferred from geomagnetic secular variation data...
We present a method to characterize the spectral transfers of magnetic energy between scales in simu...
International audienceWe use numerical dynamos to investigate the possible role of magnetic diffusio...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary S...
International audienceThe geodynamo features a broad separation between the large scale at which Ear...
We study the transfer of energy between different scales for forced three-dimensional MHD turbulent ...
We study energy transfers during magnetic energy growth in small-scale and large-scale dynamos. We p...
The core follows the precession of the mantle by virtue of coupling to it. A simple model is present...
International audienceTo understand the dynamics of the Earth’s fluid, iron-rich outer core, only in...
The Earth's internal magnetic field varies on timescales of months to billions of years. The field i...