La. Davalosorozco, RAYLEIGH-TAYLOR STABILITY OF A 2-FLUID SYSTEM UNDER A GENERAL ROTATION FIELD, Dynamics of atmospheres and oceans, 23(1-4), 1996, pp. 247-255
In this paper we investigate the Rayleigh-Taylor instability of a two-
fluid layer system under a general rotation field. Gravity is always p
erpendicular to the two horizontal layers and rotation has an arbitrar
y angle with respect to the vertical. It is found that, in an unstable
situation, an increase in the non-dimensional density-difference incr
eases the stable angular area of wave propagation, measured with respe
ct to the horizontal component of rotation. However, it is found that
the vertical component of rotation reduces not only this stable angula
r area but also the range in which the horizontal component stabilizes
the system according to a previous study by Davalos-Orozco (Fluid Dyn
. Res., 12:243, 1993). This decrease in stable area occurs along with
a decrease in the growth rate in the unstable region. Numerical analys
is of the eigenvalue equation shows that the stable angular area disap
pears after the non-dimensional vertical component of rotation attains
the value 0.33. Exact and approximate analytical expressions for the
critical values are calculated to help to understand the physics of th
e numerical analysis.