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• W1993014819 abstract "High-resolution, low-viscosity geodynamo simulations have been carried out on the Earth Simulator, one of the fastest supercomputers, in a dynamic regime similar to that of Earth's core, that is, in a quasi–Taylor state. Our dynamo models exhibit features of the geodynamo not only in spatial and temporal characteristics but also in dynamics. Polarity reversals occurred when magnetic flux patches at high latitudes moved poleward and disappeared; patches with reversed field at low and mid-latitudes then moved poleward." @default.
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• W1993014819 date "2005-07-15" @default.
• W1993014819 modified "2023-09-25" @default.
• W1993014819 title "Simulations of a Quasi–Taylor State Geomagnetic Field Including Polarity Reversals on the Earth Simulator" @default.
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• W1993014819 doi "https://doi.org/10.1126/science.1111831" @default.
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