Evolution of calculations of the virtual dipole moment of the Earth for reconstructing the oceanic inversion magnetic layer’s parameters
- 作者: Schreider A.A.1, Ignatova A.A.1, Schreider A.A.2, Sajneva A.E.1, Varga P.3, Denis C.4
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隶属关系:
- Shirshov Institute of Oceanology
- Scientific Research Institute for the Economics and Organization of Administration in the Gas Industry
- Seismological Observatory, Geodetic, and Geophysical Institute
- Institute of Astrophysics at Liege University
- 期: 卷 56, 编号 3 (2016)
- 页面: 428-434
- 栏目: Marine Geology
- URL: https://bakhtiniada.ru/0001-4370/article/view/149180
- DOI: https://doi.org/10.1134/S000143701603019X
- ID: 149180
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详细
The VDM (virtual dipole moment) is one of the most significant characteristics describing the behavior of the time evolution of the terrestrial magnetic field. However, we have revealed that the formulas with which VDM calculations are performed often do not coincide with each other in various literature sources. Hence, results are obtained from these calculations that cannot be identical. Their correctness is verified by comparing the dimension and obtained results with the known value of the VDM for our time.
作者简介
A. Schreider
Shirshov Institute of Oceanology
编辑信件的主要联系方式.
Email: aschr@ocean.ru
俄罗斯联邦, Moscow
A. Ignatova
Shirshov Institute of Oceanology
Email: aschr@ocean.ru
俄罗斯联邦, Moscow
Al. Schreider
Scientific Research Institute for the Economics and Organization of Administration in the Gas Industry
Email: aschr@ocean.ru
俄罗斯联邦, Moscow
A. Sajneva
Shirshov Institute of Oceanology
Email: aschr@ocean.ru
俄罗斯联邦, Moscow
P. Varga
Seismological Observatory, Geodetic, and Geophysical Institute
Email: aschr@ocean.ru
匈牙利, Budapest
C. Denis
Institute of Astrophysics at Liege University
Email: aschr@ocean.ru
比利时, Liege
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