ON THE NON-UNIQUENESS OF MAIN GEOMAGNETIC FIELD DETERMINED BY SURFACE INTENSITY MEASUREMENTS: THE BACKUS PROBLEM

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dc.contributor.author Alberto P.
dc.contributor.author Oliveira O.
dc.contributor.author Pais M.A.
dc.date.accessioned 2022-10-10T04:25:13Z
dc.date.available 2022-10-10T04:25:13Z
dc.date.issued 2004
dc.identifier https://elibrary.ru/item.asp?id=14244279
dc.identifier.citation Geophysical Journal International, 2004, 159, 2, 548-554
dc.identifier.issn 0956-540X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/38949
dc.description.abstract We revisit the problem of non-uniqueness of harmonic magnetic field models in a region outside a sphere containing the field sources, when only intensity values on the sphere surface are known. Using the angular momentum algebra and the Clebsch-Gordan coefficients, we are able to treat different aspects of this non-uniqueness following a unified line of reasoning. In this new framework, we first recover two Backus results, namely the proof of uniqueness in the case of a field generated by a finite number of harmonics and the recurrence relation that defines the well-known Backus series. This formalism allows us to extend previous studies in two ways: firstly, we show how to produce an harmonic series orthogonal on the sphere to some other arbitrary harmonic series; secondly, we outline a new method for computing magnetic field models starting from scalar intensity values alone.
dc.subject Backus effect
dc.subject Backus problem
dc.subject geomagnetism
dc.subject main field models
dc.subject nonuniqueness
dc.title ON THE NON-UNIQUENESS OF MAIN GEOMAGNETIC FIELD DETERMINED BY SURFACE INTENSITY MEASUREMENTS: THE BACKUS PROBLEM
dc.type Статья


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