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Extremely good agreement is demonstrated for the low-resolution internal fields computed by the two codes.
Should all large scale internal fields, including fields induced by the external field in the Earth's mantle, be included?
It allows to calculate scattered fields outside the sphere, internal fields, phase relations, and various cross sections.
To further simplify the illustration, consider the internal fields induced in the spherical particle on the x and y-axes only.
This model also attempts to separate the core and the internal fields induced in the Earth's mantle by the external fields (Sabaka et al. 2015).
This, combined with the fact that the external magnetic field perturbations were small due to a very long period of low solar activity, serve studies of internal fields.
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But the leaked US internal field reports record no civilian casualties at all.
The internal field, however, makes the susceptibility larger than that given by the Curie law.
The dominant component of the internal field is that of a centred dipole.
The resulting magnetization M equals χp(H + λM), in which χp is the susceptibility that the substance would have in the absence of the internal field.
Internal field coefficients for degrees n = 21 60 are static.
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