Some New Contributions to the Theory of the Main Geomagnetic Field

Lücke, Óscar H.

doi:10.5636/jgg.17.531

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Dynamo Thories Of Geomagnetism1

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1967

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“…The dynamo theory as proposed by Elsasser (1939Elsasser ( , 1946a and developed by Elsasser (1946bElsasser ( , 1947Elsasser ( , 1950Elsasser ( , 1955Elsasser ( , 1956aElsasser ( , 1956b, Bullard (1948, 1949a, 1949b), Bullard and Gellman (1954), and Parker (1955) ispresently considered to be the most promising explanation of the main geomagnetic field and its variations. Reviews of theories of the earth's magnetism are given by Runcorn (1954Runcorn ( , 1955aRuncorn ( , 1955b, Inglis (1955Inglis ( , 1965, Hide (1956Hide ( , 1966, Hide and Roberts (1961), Jacobs (1963), Kern and Vestine (1963), Braginskiy (1964), Lucke (1965), and DeVuyst (1966), The basic idea of the self-exciting dynamo for the earth is the regeneration of a previously existing magnetic field. This is accomplished by means of complicated induction phenomena.…”

Section: Dynamo Thories Of Geomagnetismmentioning

confidence: 99%

A review of studies made on the decade fluctuations in the earth's rate of rotation.

Davey¹

1967

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Studies of variations in the length of the day (I.o. d.) on the order of a few milliseconds over the period of a few decades are briefly reviewed. In this connection, studies of the dynamo theory of geomagnetism, the westward drift of the magnetic field, and electromagnetic core-mantle coupling preface the theory of the decade fluctuations in the 1. o.d. Keywords: core-mantle coupling, decade fluctuations, dynamo theory, earth's core, geomagnetism, rotation of the earth, westward drift. 1.

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Section: Dynamo Thories Of Geomagnetismmentioning

confidence: 99%

A review of studies made on the decade fluctuations in the earth's rate of rotation.

Davey¹

1967

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Some New Contributions to the Theory of the Main Geomagnetic Field

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Cited by 1 publication

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A review of studies made on the decade fluctuations in the earth's rate of rotation.

A review of studies made on the decade fluctuations in the earth's rate of rotation.

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