Orbital Influence on Earth's Magnetic Field: 100,000-Year Periodicity in Inclination

  • Toshitsugu Yamazaki
    Institute for Marine Resources and Environment, Geological Survey of Japan, AIST, Tsukuba 305-8567, Japan.
  • Hirokuni Oda
    Institute for Marine Resources and Environment, Geological Survey of Japan, AIST, Tsukuba 305-8567, Japan.

書誌事項

公開日
2002-03-29
DOI
  • 10.1126/science.1068541
公開者
American Association for the Advancement of Science (AAAS)

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説明

<jats:p>A continuous record of the inclination and intensity of Earth's magnetic field, during the past 2.25 million years, was obtained from a marine sediment core of 42 meters in length. This record reveals the presence of 100,000-year periodicity in inclination and intensity, which suggests that the magnetic field is modulated by orbital eccentricity. The correlation between inclination and intensity shifted from antiphase to in-phase, corresponding to a magnetic polarity change from reversed to normal. To explain the observation, we propose a model in which the strength of the geocentric axial dipole field varies with 100,000-year periodicity, whereas persistent nondipole components do not.</jats:p>

収録刊行物

  • Science

    Science 295 (5564), 2435-2438, 2002-03-29

    American Association for the Advancement of Science (AAAS)

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