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- W2885355593 abstract "A coarse observational/paleomagnetic confirmation is presented for the central hypothesis of paleomagnetism stating the predominance of axial dipole under averaging. The confirmation is based on the averaging time smaller than the full periods for axial dipole and larger than for equatorial one. The dipole-related average geodynamo scales are re-estimated as 18 km from the IGRF’s dipole 1905–2020 variations. That leads to too small convection and geodynamo power estimations based on the known geodynamo-like scaling laws, while obtained here smallest magnetic and average hydrodynamic 7 km scale gives realistic convection power 0.4 TW." @default.
- W2885355593 created "2018-08-22" @default.
- W2885355593 creator A5040382441 @default.
- W2885355593 date "2018-08-15" @default.
- W2885355593 modified "2023-09-26" @default.
- W2885355593 title "Geomagnetic Variations for Axial Dipole Hypothesis and Dynamo Parameters" @default.
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- W2885355593 doi "https://doi.org/10.1007/978-3-319-90437-5_33" @default.
- W2885355593 hasPublicationYear "2018" @default.
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