Abstract
Monthly means of three geomagnetic components (X-northern, Y-eastern and Z-vertical downward) from 54 observatories over the interval 1960-2002 have been analysed to determine the annual and semi-annual variations. The method applied is a multi-taper analysis, which gives a robust estimate of the power spectral density of the temporal variation of the field components. The main objective is to investigate the geographic dependence of the annual and semi-annual variations. Surprisingly, these variations in the vertical downward component are not homogeneously distributed all over the globe, having mainly a longitudinal dependency. The results of the analysis are briefly discussed with regard to possible mechanisms responsible for these variations and to mantle conductivity. Copyright © The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences; TERRAPUB.
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Wardinski, I., & Mandea, M. (2006). Annual and semi-annual variations of the geomagnetic field components analysed by the multi-taper method. Earth, Planets and Space, 58(6), 785–791. https://doi.org/10.1186/BF03351982
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