HYDRODYNAMIC SPIRALITY IN GEODYNAMO MODELS

dc.contributor.author	Reshetnyak M.Yu.
dc.contributor.author	Steffen B.
dc.date.accessioned	2024-10-19T07:54:53Z
dc.date.available	2024-10-19T07:54:53Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13507224
dc.identifier.citation	Doklady Earth Sciences, 2006, 409, 5, 739-743
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46093
dc.description.abstract	Generation of geomagnetic field is related to dynamo processes in the earth’s liquid core. It is one of the basic problems of geophysics. The geomagnetic field can be generated by both large-scale and small-scale flows. The latter possibility is closely related to the α-effect concept of the theory of intermediate fields. The nature of the α-effect consists in the reflection symmetry distortion in a convective rotating body, as a result of which the number of rightward rotating whirls in the Northern Hemisphere, for example, is systematically greater than the number of left-ward rotating whirls.
dc.title	HYDRODYNAMIC SPIRALITY IN GEODYNAMO MODELS
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06050138

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