  We present the stability analysis of a plane Couette flow which is stably
stratified in the vertical direction orthogonally to the horizontal shear.
Interest in such a flow comes from geophysical and astrophysical applications
where background shear and vertical stable stratification commonly coexist. We
perform the linear stability analysis of the flow in a domain which is periodic
in the stream-wise and vertical directions and confined in the cross-stream
direction. The stability diagram is constructed as a function of the Reynolds
number Re and the Froude number Fr, which compares the importance of shear and
stratification. We find that the flow becomes unstable when shear and
stratification are of the same order (i.e. Fr $\sim$ 1) and above a moderate
value of the Reynolds number Re$\gtrsim$700. The instability results from a
resonance mechanism already known in the context of channel flows, for instance
the unstratified plane Couette flow in the shallow water approximation. The
result is confirmed by fully non linear direct numerical simulations and to the
best of our knowledge, constitutes the first evidence of linear instability in
a vertically stratified plane Couette flow. We also report the study of a
laboratory flow generated by a transparent belt entrained by two vertical
cylinders and immersed in a tank filled with salty water linearly stratified in
density. We observe the emergence of a robust spatio-temporal pattern close to
the threshold values of F r and Re indicated by linear analysis, and explore
the accessible part of the stability diagram. With the support of numerical
simulations we conclude that the observed pattern is a signature of the same
instability predicted by the linear theory, although slightly modified due to
streamwise confinement.
