Physical representations of the geomagnetic field

作者: A. G. McNish

DOI: 10.1029/TR021I002P00287

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摘要: The familiar Gaussian analysis of the geomagnetic field by method spherical harmonics clearly indicates that predominant portion so-called permanent magnetism Earth is due to internal causes. One striking results this dominance first degree. These first-degree may be physically represented a dipole at center with its south-seeking end directed toward point in latitude 78°5 north, longitude 291°2 east. An improved representation which partially takes into account above degree furnished shifting 342 km 6°5 161°8 east [see 1 under “References” paper].

参考文章(1)
A. G. McNish, E. A. Johnson, Magnetization of unmetamorphosed varves and marine sediments Journal of Geophysical Research. ,vol. 43, pp. 401- 407 ,(1938) , 10.1029/TE043I004P00401