HR: 17:10h
AN: GP34B-01 INVITED [Abstracts]
TI: On the Trail of Bullard's Dynamo
AU: * Olson, P
EM: olson@jhu.edu
AF: Department of Earth and Planetary Sciences, Johns Hopkins University
3400 North Charles St, Baltimore, MD 21218, United States
AB:
E. C. Bullard proposed the first deterministic models of the geodynamo more than five decades ago, combining
low order spherical harmonic degree poloidal flows in the outer core suggested by the geomagnetic field
structure on the core-mantle boundary with an axisymmetric zonal toroidal flow implied by the geomagnetic
westward drift. Although most of the original Bullard dynamo models were kinematic failures, their modern
dynamical counterparts have proven notably successful in accounting for many characteristics of the
geomagnetic and paleomagnetic fields, including their dipole dominance, the time average axial state,
preference for westward drift, low frequency secular variation, and the existence of polarity reversals and
excursions. However, theoretical considerations supported by some recent numerical and laboratory dynamos
indicate that small scale convection and turbulence may be more important than large scale flow in the dynamo
generation process because the outer core is in a high Rayleigh number, low Ekman number dynamical regime.
In this talk the properties of large scale laminar versus small scale turbulent numerical dynamos are compared.
Evidence is presented that large scale flows similar to those envisioned by Bullard are an important part the
geodynamo in spite of the turbulent state of the core, because of the non-uniform heat flow from the core into the
heterogeneous lower mantle. Dynamo models and laboratory experiments show that non-uniform thermal
coupling with the lower mantle generates large scale flows in the outer core that affect the symmetry of the
geomagnetic field and may cause non-uniform growth of the inner core. Dynamo models also indicate that time
dependence of core-mantle thermal coupling influences the frequency of polarity reversals and the timing of
superchrons.
DE: 1507 Core processes (1213, 8115)
DE: 1510 Dynamo: theories and simulations
DE: 1521 Paleointensity
DE: 1522 Paleomagnetic secular variation
DE: 1530 Rapid time variations
SC: Geomagnetism and Paleomagnetism [GP]
MN: 2007 Fall Meeting