Evolution of calculations of the virtual dipole moment of the Earth for reconstructing the oceanic inversion magnetic layer’s parameters


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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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