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Titel Earth's inner core fluctuating rotation
VerfasserIn Julien Aubert, Mathieu Dumberry, Gauthier Hulot
Konferenz EGU General Assembly 2010
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 12 (2010)
Datensatznummer 250045216
 
Zusammenfassung
It is uncertain whether the seismically-inferred longitudinal rotation of Earth's solid inner core with respect to the mantle is steady or fluctuating in time. We use numerical dynamo modelling to show that in the limit of vanishing fluid outer core viscosity which is appropriate for the Earth, the time-dependant part of inner core differential rotation should overcome the steady part by several orders of magnitude. For the predicted amplitude of rotation fluctuations to be compatible with the existing seismic observations and geodetic constraints, the magnitude of gravitational coupling between the mantle and inner core must be lower than previously thought. The weakness of steady inner core rotation additionally confirms the possibility of texturing mechanisms of the inner core surface by lower mantle thermal heterogeneities.