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The Magnetic Field Induced by the Bodily Tide in the Core of the Earth
The motion in the liquid core of the earth due to the bodily tide can induce a periodic magnetic field having the frequency σ of the tide as well as multiple frequencies, including a steady term. The coupling coefficient for the steady term between the convectively inducing and induced fields is est...
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| Autor principal: | |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
1971
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC389130/ https://ncbi.nlm.nih.gov/pubmed/16591922 |
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