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Please use this identifier to cite or link to this item: https://libeldoc.bsuir.by/handle/123456789/58523
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dc.contributor.authorAronov, G. A.-
dc.contributor.authorAronov, A. G.-
dc.contributor.authorSaladukhin, I. A.-
dc.contributor.authorKadymau, A. A.-
dc.contributor.authorLaziuk, V. M.-
dc.coverage.spatialSwitzerlanden_US
dc.date.accessioned2024-12-19T07:11:03Z-
dc.date.available2024-12-19T07:11:03Z-
dc.date.issued2024-
dc.identifier.citationGeomagnetic Measurements at the Pleshchenitsy Geophysical Observatory / G. A. Aronov, A. G. Aronov, I. A. Saladukhin [et al.] // Solar-Terrestrial Relations and Physics of Earthquake Precursors : Proceedings of the XIII International Conference / Eds.: A. Dmitriev [et al.]. – Switzerland : Springer Nature Switzerland AG, 2024. – P. 1–11.en_US
dc.identifier.urihttps://libeldoc.bsuir.by/handle/123456789/58523-
dc.description.abstractA significant long-term increase of some geomagnetic field components was revealed suggesting a continuous movement of the Earth’s magnetic pole. In addition, the periodic change of the degree of the geomagnetic field disturbance was determined, which may be due to the solar activity variations within the 11-year cycles.en_US
dc.language.isoenen_US
dc.publisherSpringer Nature Switzerland AGen_US
dc.subjectпубликации ученыхen_US
dc.subjectgeomagnetic field componentsen_US
dc.subjectgeomagnetic field disturbanceen_US
dc.subjectsolar activity cycleen_US
dc.titleGeomagnetic Measurements at the Pleshchenitsy Geophysical Observatoryen_US
dc.typeArticleen_US
dc.identifier.DOIhttps://doi.org/10.1007/978-3-031-50248-4_10-
Appears in Collections:Публикации в зарубежных изданиях

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