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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...

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Podrobná bibliografie
Vydáno v:Proc Math Phys Eng Sci
Hlavní autoři: Aurnou, J. M., King, E. M.
Médium: Artigo
Jazyk:Inglês
Vydáno: The Royal Society Publishing 2017
Témata:
On-line přístup: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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