A fast-moving feature of westward drift
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Abstract
he dominant feature in the magnetic declination record at all European sites for which adequate data are available is a minimum between 1750 and 1860. The time of minimum at different sites correlates well with longitude and implies a westward drift rate of 0.61 ± 0.08° yr-1. This is greatly in excess of the widely adopted value of 0.18° yr-1 for global westward drift.
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Barraclough DR, Malin SRC. A fast-moving feature of westward drift. Ann. Geophys. [Internet]. 1999Nov.25 [cited 2021Dec.4];42(1). Available from: https://www.annalsofgeophysics.eu/index.php/annals/article/view/3696
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