The simplest, unsteady surface flow of a frozen-flux core that exactly fits a geomagnetic field model
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/v018/i004/91GL00825/91GL00825.pdf
Reference13 articles.
1. Kinematics of geomagnetic secular varia;Backus;Soc. Land.,1968
2. The electric field produced in the mantle by the dynamo in the core;Backus;Phys. Earth Planet. Int.,1982
3. Comparing the jerk with other global models of the geomagnetic field from 1960 to 1978;Backus;J. Geophys. Res.,1987
4. The region of the coremantle boundary where a geo-strophic velocity field can be determined from frozen-flux magnetic data;Backus;Geophys. J.R. Astron. Soc.,1986
5. On the coupling of fluid dynamics and electromagnetism at the top of earth's core;Benton;Geophys. Astrophys. Fluid Dyn.,1985
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1. Topographic Core-Mantle Coupling and Fluctuations in the Earth's Rotation;Relating Geophysical Structures and Processes: The Jeffreys Volume;2013-03-18
2. Geomagnetic secular variation violating the frozen-flux condition at the core surface;Earth, Planets and Space;2010-09
3. Time dependency of fluid flow near the top of the core;Earth, Planets and Space;1998-10
4. Aliasing and noise in core-surface flow inversions;Geophysical Journal International;1996-08
5. An estimate of the radial gradient of the toroidal magnetic field at the top of the Earth's core;Physics of the Earth and Planetary Interiors;1995-07
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