Allowance for the influence of the world ocean on the variable geomagnetic field by means of a spherical shell of finite thickness

Details Allowance for the influence of the world ocean on the variable geomagnetic field by means of a spherical shell of finite thickness Allowance for the influence of the world ocean on the variable geomagnetic field by means of a spherical shell of finite thickness

Jun 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980ge%26ae..20..523z&link_type=abstract

Geomagnetizm i Aeronomiia, vol. 20, May-June 1980, p. 523-529. In Russian.

Physics

1

Geomagnetism, Magnetic Variations, Oceanographic Parameters, Shell Theory, Differential Equations, Spherical Shells, Surface Layers, Thin Films

Scientific paper

In the present paper, Dmitriev's (1969) boundary conditions (which take the finite thickness of the surface layer into consideration) are adapted to a thin nonuniform spherical layer. These conditions are then used as a basis to develop a method of accounting for the distorting influence of nonuniform surface layer on the probing of magnetic variations.

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