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On the Backus Effect - II

Abstract : We again consider the problem of recovering the Earth's internal magnetic field B knowing its intensity IIBII at the Earth's surface and the location of the dip equator. In the present paper we focus on estimating the difference between two solutions B obtained from imperfect data. We explicitly estimate this difference and show that it converges to zero when the errors on IIBII and on the location of the dip equator E both tend to zero.
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G Khokhlov, G Hulot, J.-L Le Mouël. On the Backus Effect - II. Geophysical Journal International, Oxford University Press (OUP), 1999, 137 (3), pp.816-820. ⟨10.1046/j.1365-246x.1999.00843.x⟩. ⟨insu-01409673⟩

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