In open channel flows, the transition from a rapid to fluvial flow motion is called a hydraulic jump. A related flow motion is a compression wave in a channel, also positive surge and bore. A key feature of hydraulic jumps and breaking bores is the rapid spatial and temporal deformations of the roller free-surface, in response to the interactions between entrained air bubbles and turbulent structures. The flow structure in the roller region remains a great research challenge because of large quantities of entrained air, bubble-turbulence interactions and the coupling between turbulent properties and free-surface deformations. Breaking bores and hydraulic jumps with a marked roller present a number of similar features that are discussed herein. Recent results showed that the roller is a highly unsteady turbulent region, with both the roller toe and free-surface constantly fluctuating with time and space, although the roller shape is quasi-two-dimensional in average. Downstream of the roller toe, air bubbles and vorticity are diffused in the shear zone at different rates. The double diffusive convection process leads to a complex interplay between instantaneous freesurface deformations, velocity fluctuations, interfacial processes including breakup and coalescence.