Magnetic to magnetic and kinetic to magnetic energy transfers at the top of the Earth's core

被引:4
作者
Huguet, Ludovic [1 ,2 ]
Amit, Hagay [3 ]
Alboussiere, Thierry [2 ]
机构
[1] Case Western Reserve Univ, Dept Earth Environm & Planetary Sci, Cleveland, OH 44106 USA
[2] Univ Lyon 1, CNRS UMR 5276, ENS Lyon, Lab Geol Lyon,Terre,Planetes,Environm, 2 Rue Raphael Dubois, F-69622 Villeurbanne, France
[3] Univ Nantes, CNRS UMR 6112, Lab Planetol & Geodynam, 2 Rue Houssiniere, F-44000 Nantes, France
关键词
Dynamo: theories and simulations; Geomagnetic induction; Magnetic field; Rapid time variations; Core; outer core and inner core; GEOMAGNETIC SECULAR VARIATION; STRATIFIED LAYER; SHELL TRANSFERS; OUTER-CORE; FIELD; FLOW; TIME; DYNAMO; LENGTH; IRON;
D O I
10.1093/gji/ggw317
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
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. The magnetic to magnetic energy transfer shows a complex behaviour with local and non-local transfers. The spectra of magnetic to magnetic energy transfers show clear maxima and minima, suggesting an energy cascade. The kinetic to magnetic energy transfers, which are much weaker due to the weak poloidal flow, are either local or non-local between degree one and higher degrees. The patterns observed in the matrices resemble energy transfer patterns that are typically found in 3-D MHD numerical simulations.
引用
收藏
页码:934 / 948
页数:15
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