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The cross-over to magnetostrophic convection in planetary dynamo systems
Global scale magnetostrophic balance, in which Lorentz and Coriolis forces comprise the leading-order force balance, has long been thought to describe the natural state of planetary dynamo systems. This argument arises from consideration of the linear theory of rotating magnetoconvection. Here we te...
Gorde:
| Argitaratua izan da: | Proc Math Phys Eng Sci |
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| Egile Nagusiak: | , |
| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
The Royal Society Publishing
2017
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| Gaiak: | |
| Sarrera elektronikoa: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5378236/ https://ncbi.nlm.nih.gov/pubmed/28413338 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rspa.2016.0731 |
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