S. Parhi et Gs. Lakhina, CRITERIA FOR SHEAR-FLOW INSTABILITY IN THE MAGNETOPAUSE BOUNDARY-LAYER REGION, Earth, moon, and planets, 62(3), 1993, pp. 245-258
Shear flow instability is studied in the planar magnetopause boundary
layer region by treating the plasma as compressible. A necessary crite
rion for instability near the Alfven resonance is obtained. Sufficient
criterion for instability is derived from the solution of a six degre
e polynomial for the cases of constant and antisymmetric velocity prof
iles when there is no Alfven resonance. Both the criteria are obtained
analytically for the first time. The necessary criterion generalises
the well-known inflexion point theorem and Rayleigh's criterion in the
hydrodynamic case to magnetohydrodynamic case for incompressible plas
ma provided both the Alfven surfaces lie in the boundary layer. The Al
fven resonant surfaces are similar to the boundary walls in hydrodynam
ics. A semi-hyperbola theorem for the unstable situation is derived wh
ich represents the domain of Doppler shifted real frequency and imagin
ary frequency. From the sufficient criterion for instability it is obs
erved that plasma shear should be more for a compressible plasma in or
der to make the plasma unstable. The growth rate for instability is ob
tained. A thin layer around Alfven resonance effectively determines ho
w fast the flow could attain instability.