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• W3099145280 abstract "Current Earth-like numerical dynamo simulations are able to reproduce many characteristics of the observed geomagnetic field. One notable exception is the geomagnetic octupolar component. Here we investigate whether a stably stratified layer at the top of the core, a missing ingredient in standard dynamo simulations, can explain the observed geomagnetic octupole. Through numerical simulations, we find that the existence of a stable layer has significant influence on the octupolar-to-dipolar ratio of the magnetic field. Particularly, we find that a 60-km stable layer with relatively strong stability or a 130-km layer with relatively weak stability are compatible with the observations, but a 350-km stable layer, as suggested by recent seismological evidence, is not compatible with Earth's octupole field over the past 10,000 years." @default.
• W3099145280 created "2020-11-23" @default.
• W3099145280 creator A5020904077 @default.
• W3099145280 creator A5063640595 @default.
• W3099145280 date "2018-10-16" @default.
• W3099145280 modified "2023-10-10" @default.
• W3099145280 title "Sensitivity of the Geomagnetic Octupole to a Stably Stratified Layer in the Earth's Core" @default.
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• W3099145280 doi "https://doi.org/10.1029/2018gl078975" @default.
• W3099145280 hasPublicationYear "2018" @default.
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