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Geomagnetic spikes on the core-mantle boundary

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  • Christopher Davies

    (School of Earth & Environment, University of Leeds
    Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography University of California at San Diego)

  • Catherine Constable

    (Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography University of California at San Diego)

Abstract

Extreme variations of Earth’s magnetic field occurred in the Levant region around 1000 BC, when the field intensity rapidly rose and fell by a factor of 2. No coherent link currently exists between this intensity spike and the global field produced by the core geodynamo. Here we show that the Levantine spike must span >60° longitude at Earth’s surface if it originates from the core–mantle boundary (CMB). Several low intensity data are incompatible with this geometric bound, though age uncertainties suggest these data could have sampled the field before the spike emerged. Models that best satisfy energetic and geometric constraints produce CMB spikes 8–22° wide, peaking at O(100) mT. We suggest that the Levantine spike reflects an intense CMB flux patch that grew in place before migrating northwest, contributing to growth of the dipole field. Estimates of Ohmic heating suggest that diffusive processes likely govern the ultimate decay of geomagnetic spikes.

Suggested Citation

  • Christopher Davies & Catherine Constable, 2017. "Geomagnetic spikes on the core-mantle boundary," Nature Communications, Nature, vol. 8(1), pages 1-11, August.
    • Handle: RePEc:nat:natcom:v:8:y:2017:i:1:d:10.1038_ncomms15593
    DOI: 10.1038/ncomms15593
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