204
C. F. GAUSS ON THE GENERAL THEORY OF
From this equation, combined with the remark in the preceding article, we obtain the general form of . If we represent by the following function of ,
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then has the form of an aggregate of parts,
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where , , , , &c. are determinate numerical co-efficients.
If the magnetic force at the point be resolved into three forces perpendicular to each other, , , and , of which is directed towards the centre of the earth, and and are tangential to a spherical surface concentric with the earth, passing through , directed northwards in a plane passing through and the axis of the earth, and directed westwards in a plane parallel to the equator of the earth, then
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consequently,
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On the surface of the earth and are the same horizontal components which we have designated above by those letters; is the vertical component, which is positive when directed downwards.
The expressions for these forces on the surface of the earth are, then,
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