Titlebook: Geomagnetism and Palaeomagnetism; F. J. Lowes,D. W. Collinson,A. Soward Book 1989 Kluwer Academic Publishers 1989 Catalog Service for the

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Deterministic Chaos, Geomagnetic Reversals, and the Spherical Pendulumne. The chaotic motion of a forced spherical pendulum is used to exemplify these ideas. Reasons are given why geomagnetic reversals might be interpreted as chaotic and the implications discussed. Some statistical data on the pendulum motion are presented in a form that may allow comparison with geomagnetic data.

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,Mikrobetrachtung inklusive Anwendungsfälle,l means of the vector magnetic field components measured at nearly one hundred magnetic observatories widely distributed about the Earth. The data that have been analyzed are for the time interval 1961–1977..Spherical harmonic models for each year within the indicated time interval have been compute

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Studien zur Kommunikationswissenschaftonding core motions. It is shown, however, that changes of duration from El Niño events to 50–150 years are primarily balanced by, or rather driven by, hydrospheric motions, i.e. oceanic circulation changes. Two (or three) of the major LOD changes during the last 350 years are linked to geomagnetic

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conception

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,Hochspannungs-Gleichstrom-Übertragung,00 years. The first set, derived from six 9 m Mackereth cores covers the interval back to 38000 years BP. The second and third sets extend back to about 50000 years BP. They are derived respectively from six 12 m Mackereth cores and from five Livingston cores. Holocene data have been removed from th