Radial vorticity constraint in core flow modeling

We present a new method for estimating core surface flows by relaxing the tangentially geostrophic (TG) constraint. Ageostrophic flows are allowed if they are consistent with the radial component of the vorticity equation under assumptions of the magnetostrophic force balance and an insulating mantl...

Ausführliche Beschreibung

Bibliographische Detailangaben

Veröffentlicht in:	Journal of Geophysical Research: Solid Earth 2011-11, Vol.116 (B11), p.n/a
Hauptverfasser:	Asari, S., Lesur, V.
Format:	Artikel
Sprache:	eng
Schlagworte:	core flow core-mantle boundary Flow Geodetics Geophysics High performance computing Magnetism magnetostrophic balance Meteorology satellite magnetic field model Satellites
Online-Zugang:	Volltext
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