Global changes in intensity of the Earth's magnetic field during the past 800 kyr
Article Abstract:
Records of relative paleointensity were integrated into a composite curve covering the past 800 kyr. The intensity of The Earth's dipole field was found to have experienced large-amplitude variations during the time span, with increased intensity minima occurring at times of known excursions in field direction. There was no stable periodicity found and the data does not support the hypothesis that the orbital parameters of the Earth have a direct impact on the geodynamo.
Publication Name: Nature
Subject: Zoology and wildlife conservation
ISSN: 0028-0836
Year: 1999
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Ancient inclinations
Article Abstract:
It has been recognized since the 19th century that the main element of the Earth's magnetic field is an axial dipole aligned with the rotation axis. However, new research shows that lower inclinations were exhibited in the Palaezoic and Precambrian ages, between 250 million and 3,500 million years ago. It is suggested that during these periods the axial dipole was joined by octupole and quadrupole components of the field.
Publication Name: Nature
Subject: Zoology and wildlife conservation
ISSN: 0028-0836
Year: 1998
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Geomagnetic dipole strength and reversal rate over the past two million years
Article Abstract:
A composite curve that shows the evolution of the geomagnetic dipole strength and reversal rate is presented. The results revealed that the time-averaged field is higher during periods without reversals but the amplitude of the short-term oscillations remained the same.
Publication Name: Nature
Subject: Zoology and wildlife conservation
ISSN: 0028-0836
Year: 2005
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