arXiv · 1709.02666
Magnetic Shear Damped Polar Convective Fluid Instabilities
Abstract
The influence of the magnetic field shear is studied on the $E\times B$ (and/or Gravitational) and the Current Convective Instabilities (CCI) occuring in the High latitude F-layer ionosphere. It is shown that magnetic shear reduces the growth rate of these instabilties. The magnetic shear induced stabilization is more effective at the larger scale sizes ($\geq$ tens of kilometers) while at the scintillation causing intermediate scale sizes ($\sim$ a few kms), the growth rate is largely unaffected. The eigen mode structure is localised about a rational surface due to finite magnetic shear and has broken reflectional symmetry due to centroid shift of the mode by equilibrium parallel flow or current.
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Jyoti K Atul, Rameswar Singh, Sanjib Sarkar, Oleg V Kravchenko, Sushil K Singh, Prabal K Chattopadhyaya, Predhiman K Kaw. 2017-09-08. Magnetic Shear Damped Polar Convective Fluid Instabilities. https://doi.org/10.1002/2017ja024778
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