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

dc.contributor.authorAlberto P.
dc.contributor.authorOliveira O.
dc.contributor.authorPais M.A.
dc.date.accessioned2022-10-10T04:25:13Z
dc.date.available2022-10-10T04:25:13Z
dc.date.issued2004
dc.description.abstractWe 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.identifierhttps://elibrary.ru/item.asp?id=14244279
dc.identifier.citationGeophysical Journal International, 2004, 159, 2, 548-554
dc.identifier.issn0956-540X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/38949
dc.subjectBackus effect
dc.subjectBackus problem
dc.subjectgeomagnetism
dc.subjectmain field models
dc.subjectnonuniqueness
dc.titleON THE NON-UNIQUENESS OF MAIN GEOMAGNETIC FIELD DETERMINED BY SURFACE INTENSITY MEASUREMENTS: THE BACKUS PROBLEM
dc.typeСтатья

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