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- W1964555900 abstract "The presence of a backgroundmagnetic field is known to have a stabilising as well as a destabilising effect for shear flow instabilities. To explain the reason for this, we extend the Counter-propagating Rossby Waves mechanism, well known in the geophysical fluid dynamics community, to the magnetohydrodynamicsetting. It is demonstrated here that wave displacement leads to a magnetic field configuration that results in an appropriate vorticity distribution, and, via the non-local velocity field generated by the local vorticity anomalies, action-at-a-distance results in a constructive interaction between two waves and leads to shear instability. The existence of shear instability then rests upon whether the chosen basic state supports such a configuration required for constructive interference." @default.
- W1964555900 created "2016-06-24" @default.
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- W1964555900 date "2014-07-01" @default.
- W1964555900 modified "2023-10-17" @default.
- W1964555900 title "Magnetohydrodynamic shear instabilities arising from interacting vorticity waves" @default.
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- W1964555900 doi "https://doi.org/10.2495/afm140321" @default.
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