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Magnetic Field Variation Caused by Rotational Speed Change in a Magnetohydrodynamic Dynamo

Takehiro Miyagoshi and Yozo Hamano
Phys. Rev. Lett. 111, 124501 – Published 20 September 2013
Physics logo See Focus story: Simulations Strengthen Earth’s Magnetic-Field/Climate Connection
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Abstract

We have performed numerical magnetohydrodynamic dynamo simulations in a spherical shell with rotational speed or length-of-day (LOD) variation, which is motivated by correlations between geomagnetic field and climatic variations with ice and non-ice ages. The results show that LOD variation leads to magnetic field variation whose amplitude is considerably larger than that of LOD variation. The heat flux at the outer sphere and the zonal flow also change. The mechanism of the magnetic field variation due to LOD variation is also found. The keys are changes of dynamo activity and Joule heating.

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  • Received 4 May 2013

DOI:https://doi.org/10.1103/PhysRevLett.111.124501

© 2013 American Physical Society

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Simulations Strengthen Earth’s Magnetic-Field/Climate Connection

Published 20 September 2013

Simulations support the idea that during past ice ages, a slightly faster rotation rate for the Earth could have increased its magnetic field.

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Authors & Affiliations

Takehiro Miyagoshi1 and Yozo Hamano2

  • 1Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, 3173-25 Showa-machi, Kanazawa-ku, Yokohama, Kanagawa 236-0001, Japan
  • 2Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, 2-15 Natsushima-cho, Yokosuka, Kanagawa 237-0061, Japan

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Issue

Vol. 111, Iss. 12 — 20 September 2013

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