Inviscid, frozen-flux velocity components at the top of earth's core from magnetic observations at earth's surface: Part 1. A new methodology

DOI10.1080/03091928108208778zbMath0476.76107OpenAlexW2067046351WikidataQ114640765 ScholiaQ114640765MaRDI QIDQ3932524

Edward R. Benton

Publication date: 1981

Published in: Geophysical & Astrophysical Fluid Dynamics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1080/03091928108208778

zbMATH Keywords

Earth's liquid corecontinuous, bounded horizontal components of inviscid, frozen flux motionfrozen-flux induction equation

Mathematics Subject Classification ID

Magnetohydrodynamics and electrohydrodynamics (76W05) Hydrodynamic and hydromagnetic problems in astronomy and astrophysics (85A30) Geo-electricity and geomagnetism (86A25)

Related Items (1)

Steady flows at the top of the core from geomagnetic field models:The steady motions theorem

Cites Work

• Influence of an Axial Magnetic Field on the Steady Linear Ekman Boundary Layer

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