Schmucker, 1970 (Scripps) - MTNet

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<strong>Schmucker</strong>: Geomagnetic Variations 91 semicircular elevation is that of a 2 -dimensional dipole, superimposed upon a uniform horizontal field, when the field distribution in the z-plane is uniform and horizontal. Thus, 2 hH(u, v) = (R/r) cos 28 2 . zH(u,v) =(R/r) sm 28 (6.28) with cos 8 = ulr and l == u2 + }. The anomalous field of model "b" in figure 3S has been derived from these formulae. Similar profiles above elevations of semi elliptic and triangular cross section can be found in Rikitake and Witham's article (1964, pp. 40, 41).
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ANOMALIES OF GEOMAGNETIC VARIATIONS
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vi 4. 5. 6. CONTENTS Description of
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NOTATION All quantities are measure
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1. INTRODUOTION 1.1 Induction Anoma
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Schmucker: Geomagnetic Variations 1
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Schmucker, 1970 (Scripps) - MTNet

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