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- W2132821307 endingPage "2002" @default.
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- W2132821307 abstract "The ф-component, ϵф, of the mean electromotive force generated by asymmetric flow of fluid just beneath the core-mantle boundary (CMB), is obtained using a geomagnetic field model. This analysis is based on the supposition that the axisymmetric part of fluid flow beneath the CMB is tangentially geostrophic and toroidal. For all the epochs studied, the computed ϵф is stronger in the southern hemisphere than that in the northern hemisphere. Assuming a linear relationship between and the azimuthally averaged magnetic field , the only non-zero off-diagonal components of the pseudotensor αijrelating to , are estimated as functions of colatitude θ and the physical implications of the results are discussed." @default.
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- W2132821307 date "1992-10-23" @default.
- W2132821307 modified "2023-09-25" @default.
- W2132821307 title "Mean electromotive force generated by asymmetric fluid flow near the surface of Earth's outer core" @default.
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- W2132821307 doi "https://doi.org/10.1029/92gl01387" @default.
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