The flow above an infinite rotating disk is an example of 3D boundary-layers where crossflow instability can develop as over swept wings. With a second rotating disk parallel to the first, the configuration schematizes the cavity between the disks holding the blades of a turbine or compressor. Centrifugal and Coriolis forces produce a secondary flow in the meridian plane composed of two thin boundary-layers along the disks separated by a non-viscous geostrophic core. That produces adjacent coupled flow regions that are radically different in terms of flow stability and thickness scales involving very challenging simulations. Identify and characterize the transition mechanism is a necessity for developing future efficient control strategies ...