Substitute the stated scales and divide the momentum equation by . The ratio of inertial to Coriolis acceleration is the Rossby number
while the dimensionless buoyancy coefficient is
Thus
The dimensionless is the Burgers number for this rotating stratified flow.
For
both material derivatives vanish because the fields are independent of . Since , steady momentum balance requires
These derivatives are compatible and integrate to
The cross-stream temperature gradient and vertical stratification are in thermal-wind balance with the vertical shear.
Let . Retaining terms linear in the primed fields gives
The terms and respectively arise from perturbation advection of the velocity and temperature gradients in the basic state.
Differentiate the -momentum equation with respect to , subtract the derivative of the -momentum equation, and use incompressibility. With vertical perturbation vorticity
one obtains
Therefore
At leading order as , horizontal geostrophic balance and vertical hydrostatic balance give
The temperature equation gives
Meanwhile . The leading vertical-vorticity equation is . Since derivatives in do not commute with ,
The terms therefore cancel, leaving the conserved three-dimensional quasi-geostrophic potential vorticity
No normal flow at means . At , , so
Insert
The side-wall condition is automatic, and the potential-vorticity equation gives
Define
Then
The top and bottom conditions become
Setting the determinant of these two homogeneous equations for to zero and simplifying gives
For every , , so
The radicand in part f is therefore negative precisely when its second factor is negative. The two wave speeds are then complex conjugates, one with positive imaginary part and exponential growth. Hence

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