Substitute the stated scales and divide the momentum equation by . The ratio of inertial to Coriolis acceleration is the Rossby numberwhile the dimensionless buoyancy coefficient isThusThe dimensionless is the Burgers number for this rotating stratified flow.
Forboth material derivatives vanish because the fields are independent of . Since , steady momentum balance requiresThese derivatives are compatible and integrate toThe cross-stream temperature gradient and vertical stratification are in thermal-wind balance with the vertical shear.
Let . Retaining terms linear in the primed fields givesThe 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 vorticityone obtainsTherefore
At leading order as , horizontal geostrophic balance and vertical hydrostatic balance giveThe temperature equation givesMeanwhile . 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 vorticityNo normal flow at means . At , , so
InsertThe side-wall condition is automatic, and the potential-vorticity equation givesDefineThenThe top and bottom conditions becomeSetting the determinant of these two homogeneous equations for to zero and simplifying gives
For every , , soThe 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
Articles by others on the same topic
There are currently no matching articles.