An estimate of the radial gradient of the toroidal magnetic field at the top of the Earth's core
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics
Reference24 articles.
1. The region on the core-mantle boundary where a geostrophic velocity field can be determined from frozen-flux magnetic data;Backus;Geophys. J. R. Astron. Soc.,1986
2. Spherical harmonic models of the geomagnetic field. Geomagn;Barraclough;Bull. Inst. Geol. Sci.,1978
3. The simplest, unsteady surface flow of a frozen-flux core that exactly fits a geomagnetic field model;Benton;Geophys. Res. Lett.,1991
4. On the strength of electric currents and zonal magnetic fields at the top of the Earth's core: methodology and preliminary estimates;Benton;Phys. Earth Planet. Inter.,1979
5. Rapid diffusion of the poloidal geomagnetic field through the weakly conducting mantle: a perturbation solution;Benton;Geophys. J. R. Astron. Soc.,1983
Cited by 4 articles. 订阅此论文施引文献 订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献
1. Characteristics of the spatial distribution and the secular variation of the main geomagnetic field gradients;CHINESE J GEOPHYS-CH;2012
2. Characteristics of the Spatial Distribution and Secular Variation of Gradients of the Main Geomagnetic Field;Chinese Journal of Geophysics;2012-07
3. Determining the time-variable part of the toroidal geomagnetic field in the core-mantle boundary zone;Physics of the Earth and Planetary Interiors;2010-01
4. Time dependency of fluid flow near the top of the core;Earth, Planets and Space;1998-10
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