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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| Vydáno v: | Proc Natl Acad Sci U S A |
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| Hlavní autor: | |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
National Academy of Sciences
1971
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC389130/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/16591922/ https://ncbi.nlm.nih.govhttps://doi.org/10.1073/pnas.68.6.1111 |
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