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A kinematic model of vertical geomagnetic field variation resulting from a steady convective flow
Authors:Alexandra Marsenić
Affiliation:1. Institute of Geophysics, Academy of Sciences of Czech Republic, Bo?ní II/1401, 141 31 Prague 4, Czech Republic.;2. Geophysical Institute, Slovak Academy of Sciences, Dúbravská cesta 9, 845 28 Bratislava, Slovak Republic.geofalma@ig.cas.czgeofalma@savba.sk
Abstract:
Keywords:Magnetohydrodynamics  Induction equation  Geomagnetic variation  Reversed flux patches
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