Time dependency of fluid flow near the top of the core
Author:
Publisher
Springer Science and Business Media LLC
Subject
Space and Planetary Science,Geology
Link
http://link.springer.com/content/pdf/10.1186/BF03352174
Reference30 articles.
1. Backus, G. E., Kinematics of the geomagnetic secular variation in a perfectly conducting core, Phil. Trans. Roy. Soc. Lond. A, 263, 239–266, 1968.
2. Backus, G. E. and J. L. Le Mouël, The region on the core-mantle boundary where a geostrophic velocity field can be determined from frozen flux magnetic data, Geophys. J. R. Astron. Soc., 85, 617–628, 1986.
3. Benton, E. R. and M. A. Celaya, The simplest, unsteady surface flow of a frozen-flux core that exactly fits a geomagnetic field model, Geophys. Res. Lett., 18, 577–580, 1991.
4. Bhattacharyya, A., An estimate of the radial gradient of the toroidal magnetic field at the top of the Earth’s core, Phys. Earth Planet. Inter., 90, 81–90, 1995.
5. Bloxham, J., On the consequences of strong stable stratification at the top of Earth’s outer core, Geophys. Res. Lett., 17, 2081–2084, 1990.
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