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Recent changes of the Earth’s core derived from satellite observations of magnetic and gravity fields
To understand the dynamics of the Earth’s fluid, iron-rich outer core, only indirect observations are available. The Earth’s magnetic field, originating mainly within the core, and its temporal variations can be used to infer the fluid motion at the top of the core, on a decadal and subdecadal time-...
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| Main Authors: | , , , , , |
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| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
National Academy of Sciences
2012
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| Fag: | |
| Online adgang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3511155/ https://ncbi.nlm.nih.gov/pubmed/23064635 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1207346109 |
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