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The Depth Variation of the Intensity of Current Induced in a Model Earth and Ocean
Author(s) -
Ashour A. A.
Publication year - 1969
Publication title -
geophysical journal of the royal astronomical society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0016-8009
DOI - 10.1111/j.1365-246x.1969.tb00241.x
Subject(s) - intensity (physics) , geology , current (fluid) , variation (astronomy) , earth (classical element) , geophysics , plane (geometry) , ocean current , field (mathematics) , geodesy , climatology , oceanography , geometry , physics , optics , mathematics , astrophysics , pure mathematics , mathematical physics
Summary The variation with depth of the currents induced in the oceans is considered in reference to a model Earth completely covered by an ocean of uniform depth. The effect of the conductivity of the underlying earth is taken into account. The results show that for variations in the inducing field with periods up to 10 s, the ordinary plane skin effect formula can be applied, and that for variations with periods from 1–24h (including those of the Sq field) the current intensity is almost the same at all depths in the ocean.

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