A domino model for geomagnetic field reversals

We solve the equations of motion of a one-dimensional planar Heisenberg (or Vaks-Larkin) model consisting of a system of interacting macro-spins aligned along a ring. Each spin has unit length and is described by its angle with respect to the rotational axis. The orientation of the spins can vary in...

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Main Authors: Mori, N., Schmitt, D., Ferriz-Mas, A., Wicht, J., Mouri, H., Nakamichi, A., Morikawa, M.
Format: Report
Language:unknown
Published: arXiv 2011
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.1110.5062
https://arxiv.org/abs/1110.5062
id ftdatacite:10.48550/arxiv.1110.5062
record_format openpolar
spelling ftdatacite:10.48550/arxiv.1110.5062 2023-05-15T16:19:40+02:00 A domino model for geomagnetic field reversals Mori, N. Schmitt, D. Ferriz-Mas, A. Wicht, J. Mouri, H. Nakamichi, A. Morikawa, M. 2011 https://dx.doi.org/10.48550/arxiv.1110.5062 https://arxiv.org/abs/1110.5062 unknown arXiv arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Earth and Planetary Astrophysics astro-ph.EP FOS Physical sciences Preprint Article article CreativeWork 2011 ftdatacite https://doi.org/10.48550/arxiv.1110.5062 2022-04-01T14:04:26Z We solve the equations of motion of a one-dimensional planar Heisenberg (or Vaks-Larkin) model consisting of a system of interacting macro-spins aligned along a ring. Each spin has unit length and is described by its angle with respect to the rotational axis. The orientation of the spins can vary in time due to random forcing and spin-spin interaction. We statistically describe the behaviour of the sum of all spins for different parameters. The term "domino model" in the title refers to the interaction among the spins. We compare the model results with geomagnetic field reversals and find strikingly similar behaviour. The aggregate of all spins keeps the same direction for a long time and, once in a while, begins flipping to change the orientation by almost 180 degrees (mimicking a geomagnetic reversal) or to move back to the original direction (mimicking an excursion). Most of the time the spins are aligned or anti-aligned and deviate only slightly with respect to the rotational axis (mimicking the secular variation of the geomagnetic pole with respect to the geographic pole). Reversals are fast compared to the times in between and they occur at random times, both in the model and in the case of the Earth's magnetic field. : accepted for Physical Review E, 18 December 2012 Report Geomagnetic Pole DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Earth and Planetary Astrophysics astro-ph.EP
FOS Physical sciences
spellingShingle Earth and Planetary Astrophysics astro-ph.EP
FOS Physical sciences
Mori, N.
Schmitt, D.
Ferriz-Mas, A.
Wicht, J.
Mouri, H.
Nakamichi, A.
Morikawa, M.
A domino model for geomagnetic field reversals
topic_facet Earth and Planetary Astrophysics astro-ph.EP
FOS Physical sciences
description We solve the equations of motion of a one-dimensional planar Heisenberg (or Vaks-Larkin) model consisting of a system of interacting macro-spins aligned along a ring. Each spin has unit length and is described by its angle with respect to the rotational axis. The orientation of the spins can vary in time due to random forcing and spin-spin interaction. We statistically describe the behaviour of the sum of all spins for different parameters. The term "domino model" in the title refers to the interaction among the spins. We compare the model results with geomagnetic field reversals and find strikingly similar behaviour. The aggregate of all spins keeps the same direction for a long time and, once in a while, begins flipping to change the orientation by almost 180 degrees (mimicking a geomagnetic reversal) or to move back to the original direction (mimicking an excursion). Most of the time the spins are aligned or anti-aligned and deviate only slightly with respect to the rotational axis (mimicking the secular variation of the geomagnetic pole with respect to the geographic pole). Reversals are fast compared to the times in between and they occur at random times, both in the model and in the case of the Earth's magnetic field. : accepted for Physical Review E, 18 December 2012
format Report
author Mori, N.
Schmitt, D.
Ferriz-Mas, A.
Wicht, J.
Mouri, H.
Nakamichi, A.
Morikawa, M.
author_facet Mori, N.
Schmitt, D.
Ferriz-Mas, A.
Wicht, J.
Mouri, H.
Nakamichi, A.
Morikawa, M.
author_sort Mori, N.
title A domino model for geomagnetic field reversals
title_short A domino model for geomagnetic field reversals
title_full A domino model for geomagnetic field reversals
title_fullStr A domino model for geomagnetic field reversals
title_full_unstemmed A domino model for geomagnetic field reversals
title_sort domino model for geomagnetic field reversals
publisher arXiv
publishDate 2011
url https://dx.doi.org/10.48550/arxiv.1110.5062
https://arxiv.org/abs/1110.5062
genre Geomagnetic Pole
genre_facet Geomagnetic Pole
op_rights arXiv.org perpetual, non-exclusive license
http://arxiv.org/licenses/nonexclusive-distrib/1.0/
op_doi https://doi.org/10.48550/arxiv.1110.5062
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