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Geomagnetic Variations for Axial Dipole Hypothesis and Dynamo Parameters

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Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism

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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.

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Acknowledgements

The author is grateful to Valeriy Prohorovich Shcherbakov and Dmitry Dmitrievich Sokoloff for their reasonable criticism resulting in sufficient improving of this paper. The work on it was partly (estimations of magnetic geodynamo parameters) supported by the Russian Foundation for Basic Research with project No 16-05-00507a.

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Correspondence to S. V. Starchenko .

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Starchenko, S.V. (2019). Geomagnetic Variations for Axial Dipole Hypothesis and Dynamo Parameters. In: Nurgaliev, D., Shcherbakov, V., Kosterov, A., Spassov, S. (eds) Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism. Springer Geophysics. Springer, Cham. https://doi.org/10.1007/978-3-319-90437-5_33

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