An improvement for calculating the correlation between the geomagnetic and the Earth's gravitational fields |
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Affiliation: | 1. Laboratoire de Planétologie et Géosciences, CNRS UMR 6112, Nantes Université, Université d''Angers, Le Mans Université, 2 rue de la Houssinière, Nantes, France;2. Institut Terre et Environnement Strasbourg, École et Observatoire des Sciences de La Terre, CNRS UMR 7063, Université de Strasbourg, Strasbourg, France |
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Abstract: | There is a correlation between the geomagnetic and the Earth's gravitational fields to a certain degree. We should consider the zeral harmonic terms to calculate the correlation function. Correlation between the geomagnetic non-dipole field of epoch 1980, which was moved eastwards 165; and the departure part of the Earth's gravitational field from the hydrostatic equilibrium, yields a value of 0.6278. It is significant at the 0.01 level. Calculating the correlations of different epochs, we find that the westward drifting velocity of the geomagnetic non-dipole field is 0.3° year−1. It is not necessary to calculate the correlations between any individual harmonic term from either field. |
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