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http://hdl.handle.net/2122/1347
Authors: | Gregori, G. P.* Dong, W. J.* Gao, X. Q.* Gizzi, F. T.* |
Title: | The separation of the geomagnetic field originated in the core, in the asthenosphere, and in the crust | Issue Date: | Apr-1999 | Series/Report no.: | 2/42 (1999) | URI: | http://hdl.handle.net/2122/1347 | Keywords: | dynamo spatial spectrum white spectrum Lowes’law Nevanlinna’s law Hamilton’s principle geomagnetic anomalies inner core outer core asthenosphere |
Subject Classification: | 04. Solid Earth::04.05. Geomagnetism::04.05.01. Dynamo theory | Abstract: | The separation of the field produced by different internal sources can be accomplished by means of the so-called spatial spectrum of the geomagnetic field of internal origin. It is shown how such a rationale, when suitably interpreted, allows to recognize the field that is originated by electric currents that flow either on the Inner-Core Boundary (ICB), or on the Core-Mantle Boundary (CMB), or on the Asthenosphere-Lithosphere Boundary (ALB). It appears crucial, however, to rely on satellite measurements alone, because ground-based and ship- and air-borne records are severely perturbed by the crustal field. Therefore, it is shown, on the basis of a critical reconsideration of a few key-papers in the literature, that the best approach is to avoid mixing together all kinds of measurements. Satellite data are best suited for recognizing the dynamo field, while ground-based, ship- and air-borne records, which are measured much closer to crustal sources, are best suited, after subtraction of the satellite-derived dynamo field, for inferring the geomagnetic anomalies that are to be associated with crustal sources alone. |
Appears in Collections: | Annals of Geophysics |
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