HR: 0830h
AN: U51B-0012 [PDF]
TI: Simulated geomagnetic reversals and preferred VGP paths
AU: Kutzner, C
EM: kutzner@linmpi.mpg.de
AF: Max-Planck Institute for Aeronomy, Max-Planck Strasse 2, Katlenburg-Lindau, 37191
Germany
AU: * Christensen, U R
EM: christensen@linmpi.mpg.de
AF: Max-Planck Institute for Aeronomy, Max-Planck Strasse 2, Katlenburg-Lindau, 37191
Germany
AB:
The question if virtual geomagnetic poles (VGPs) recorded during
reversals and excursions show a longitudinal preference is discussed
controversially in the palaeomagnetic community. One possible mechanism
for such VGP clustering is the heterogeneity of heat flux at the core-mantle
boundary (CMB). We use three-dimensional convection-driven numerical dynamo models
with imposed non-uniform CMB heat flow that show stochastic reversals of the dipole field.
We calculate transitional VGPs for a large number of token sites at the Earth's surface.
In a model with a simple heat flux variation given by a $Y_{22}$ harmonic, the
VGP density maps for individual reversals differ substantially from each other but
the VGPs have a tendency to fall around a longitude of high heat flow.
The mean VGP density for many reversals and
excursions shows a statistically significant correlation with the heat flow.
In a model with an imposed heat flux pattern derived from seismic
tomography we find maxima of the mean VGP density at American and
East Asian longitudes, roughly consistent with the VGP paths seen in
several palaeomagnetic studies. We find that low-latitude regions of high heat flow are
centres of magnetic activity where intense magnetic flux bundles are generated. They
contribute to the equatorial dipole component and bias its orientation in longitude.
During reversals the equatorial dipole part is not necessarily dominant at the Earth's surface,
but is strong enough to explain the longitudinal preference of VGPs as seen from different
sites.
DE: 1510 Dynamo theories
DE: 1535 Reversals (process, timescale, magnetostratigraphy)
DE: 8180 Tomography
SC: U
MN: 2003 Fall Meeting