The simplest, unsteady surface flow of a frozen‐flux core that exactly fits a geomagnetic field model
- 1 April 1991
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 18 (4) , 577-580
- https://doi.org/10.1029/91gl00825
Abstract
No abstract availableThis publication has 11 references indexed in Scilit:
- Simultaneous stochastic inversion for geomagnetic main field and secular variation: 2. 1820–1980Journal of Geophysical Research, 1989
- Comparing the jerk with other global models of the geomagnetic field from 1960 to 1978Journal of Geophysical Research, 1987
- Steady flows at the top of Earth's core derived from geomagnetic field modelsJournal of Geophysical Research, 1986
- The region on the core--mantle boundary where a geostrophic velocity field can be determined from frozen-flux magnetic dataGeophysical Journal International, 1986
- Motions at core surface in the geostrophic approximationPhysics of the Earth and Planetary Interiors, 1985
- On the coupling of fluid dynamics and electromagnetism at the top of the earth's coreGeophysical & Astrophysical Fluid Dynamics, 1985
- Steady flows at the top of the core from geomagnetic field models:The steady motions theoremGeophysical & Astrophysical Fluid Dynamics, 1985
- Finding Core Motions from Magnetic Observations [and Discussion]Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 1982
- The electric field produced in the mantle by the dynamo in the corePhysics of the Earth and Planetary Interiors, 1982
- On Analysis of the Secular VariationJournal of geomagnetism and geoelectricity, 1965