An examination of simulated geomagnetic reversals from a palaeomagnetic perspective
By R. Coe, L. Hongre, Gary A. Glatzmaier. Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences, 2000
117 citations recorded by the source corpus.
Subfields: Atmospheric Science, Geophysics, Molecular Biology
View Paper: https://www.semanticscholar.org/paper/0caadd73d94be2b045d4ec7d27ec7cd7b72516c0
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In Atmospheric Science
- G. Hulot
- U. Christensen
- Nils Olsen
- Mioara Mandea
- P. Olson
- Christopher C. Finlay
- Catherine Constable
- M. Kono
In Geophysics
- U. Christensen
- Mioara Mandea
- G. Hulot
- Christopher C. Finlay
- Nils Olsen
- Catherine Constable
- P. Olson
- M. Kono
In Molecular Biology
- U. Christensen
- G. Hulot
- Mioara Mandea
- P. Olson
- Nils Olsen
- Christopher C. Finlay
- Julien Aubert
- Catherine Constable
Citations in the corpus
- The time-averaged magnetic field in numerical dynamos with non-uniform boundary heat flow (2002, methodology): “Coe et al. (2000) analysed the timeaveraged structure of some time-dependent dynamos with polarity reversals calculated by Glatzmaier et al. (1999).”
- The Magnetic Field of Planet Earth (2010, background): “One particularly important lesson learned from such investigations is that reversals do not always occur in the same way, even within a single dynamo run with fixed parameters and boundary conditions (Coe et al. 2000).”
- RECENT GEODYNAMO SIMULATIONS AND OBSERVATIONS OF THE GEOMAGNETIC FIELD (2002, result): “Some of their models gave reversals which are, in many ways, surprisingly similar to the paleomagnetically observed ones [see Coe et al., 2000].”