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A model for the geomagnetic field reversal rate and constraints on the heat flux variations at the core-mantle boundary
A striking feature of many natural magnetic fields generated by dynamo action is the occurrence of polarity reversals. Paleomagnetic measurements revealed that the Earth’s magnetic field has been characterised by few hundred stochastic polarity switches during its history. The rate of reversals chan...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2020
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7398921/ https://www.ncbi.nlm.nih.gov/pubmed/32747651 http://dx.doi.org/10.1038/s41598-020-69916-w |