“…Non-uniform systems can also be the result of instabilities, due to underlying non-monotonic flow curves, leading to banding (147), or dynamic instabilities (20,96,99,136,148,149,150). Shear-induced migration is also important in non-uniform conditions (7,151,152,153). Remarkably, there is a growing body of evidence that these instabilities are coupled to macroscopic deformation of the free surface, when present (98,149,154,155).…”