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nich, found a decennial period in the daily
                                         range of magnetic declination. In 1852 Sir
                                         Edward Sabine announced a similar period
                                         in the number of ”magnetic storms” affect-
                                         ing all of the three magnetic elements–declination,
                                         dip, and intensity. Australian and Cana-
                                         dian observations both showed the decen-
                                         nial period in all three elements. Wolf, of
                                         Zurich, and Gauthier, of Geneva, each inde-
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