Bf. Farrell et Pj. Ioannou, TRANSIENT DEVELOPMENT OF PERTURBATIONS IN STRATIFIED SHEAR-FLOW, Journal of the atmospheric sciences, 50(14), 1993, pp. 2201-2214
Transient development of perturbations in inviscid stratified shear fl
ow is investigated. Use is made of closed form analytic solutions that
allow concise identification of optimally growing plane-wave solution
s for the case of an unbounded flow with constant shear and stratifica
tion. For the case of channel flow, variational techniques are employe
d to determine the optimally growing disturbances. The maximum energy
growth attained over a specific time interval decreases continuously w
ith increasing stratification, and no special significance attaches to
Ri = 0.25. Indeed, transient growth can be substantial even for Ri =
O(1). A general lower bound on the energy growth attained by an optima
l perturbation in a stratified flow over a given time interval is the
square root of the growth attained by the corresponding perturbation i
n unstratified flow. Enhanced perturbation persistence is found for me
an-flow stratification lying in the range 0.1 < Ri < 0.3. Small but fi
nite perturbations in mean flow with Ri < 0.4 produce regions with loc
ally negative total density gradient, which are expected to overturn.
Although the perturbations are of wave form, buoyancy fluxes mediate t
ransfer between perturbation kinetic and potential energy during trans
ient development, thus implying that buoyancy flux is not a determinat
ive diagnostic for distinguishing between waves and turbulence in stra
tified flows.