Issue |
Europhys. Lett.
Volume 68, Number 2, October 2004
|
|
---|---|---|
Page(s) | 177 - 183 | |
Section | General | |
DOI | https://doi.org/10.1209/epl/i2004-10243-1 | |
Published online | 01 October 2004 |
Geomagnetic reversals and the stochastic exit problem
1
SRON Nationaal Instituut voor Ruimteonderzoek - Sorbonnelaan 2 3584 AW Utrecht, The Netherlands
2
Mathematisch Instituut - Boedapestlaan 6, 3508 TA Utrecht, The Netherlands
Corresponding authors: p.hoyng@sron.nl duis@math.uu.nl
Received:
18
June
2004
Accepted:
30
August
2004
We consider a dynamical system consisting of a fundamental mode
(amplitude x, nonlinearly stable) and one stable periodic
overtone, coupled by multiplicative noise. The problem emerges
from attempts to understand the variability of the geomagnetic
dipole field. We determine the mean reversal rate of with
the help of stochastic exit theory, and analyse the reversal
mechanism and the crucial role of the overtone. It is argued that
models based on the induction equation of MHD will lead to
equations of the same generic type, so that our conclusions on
the reversal scenario should also hold for the geomagnetic field.
Reversals are relatively rare, fast events, associated with a
surge in the nondipole field. The mean reversal rate is very
sensitive to the control parameters.
PACS: 05.10.Gg – Stochastic analysis methods (Fokker-Planck, Langevin, etc.) / 91.25.Cw – Origins and models of the magnetic field; dynamo theories / 91.25.Mf – Reversals
© EDP Sciences, 2004
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