
doi: 10.1007/bf00649006
Residual instabilities (associated with disturbances of small wavelengths in the vertical direction) present in a vertically-oscillating system comprised of a stratified fluid with density increasing exponentially in a vertically upward direction and subjected to a gravitational field acting vertically downward are shown to be removable by a magnetic applied along the vertical direction.
disturbances of small wavelengths in vertical direction, Reaction effects in flows, density increasing exponentially, gravitational field, Stability and instability of geophysical and astrophysical flows, vertically-oscillating system, dynamic stabilisation, Rayleigh-Taylor instability, Stability and instability of magnetohydrodynamic and electrohydrodynamic flows, residual instabilities
disturbances of small wavelengths in vertical direction, Reaction effects in flows, density increasing exponentially, gravitational field, Stability and instability of geophysical and astrophysical flows, vertically-oscillating system, dynamic stabilisation, Rayleigh-Taylor instability, Stability and instability of magnetohydrodynamic and electrohydrodynamic flows, residual instabilities
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